Home Geology and Mineralogy Applications of local climate zone classification in European cities: A review of in situ and mobile monitoring methods in urban climate studies
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Applications of local climate zone classification in European cities: A review of in situ and mobile monitoring methods in urban climate studies

  • Vasić Milica EMAIL logo , Dunjić Jelena , Savić Stevan and Dočkal Ondřej
Published/Copyright: September 9, 2025
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Abstract

This review explores the application of local climate zones (LCZs) through various measurement methods, with a focus on mobile and in situ data collection in European urban environments. The selection of articles for review was guided by specific keywords and a structured literature search process. In total, 61 studies were included for analysis. These studies primarily used in situ and mobile measurement techniques (car, bicycle, wearable device), while some also incorporated remote sensing technologies and machine learning. The reviewed papers addressed a range of urban climate topics, including urban heat island effects, outdoor thermal comfort, air temperature variations, and others, while using various approaches to distinguish between LCZs within cities. While in situ measurements offer consistent and reliable data, their spatial limitations often fail to capture detailed microclimatic differences in dense urban settings. On the contrary, mobile measurements provide improved spatial resolution and adaptability. Integrating multiple data sources is crucial to enhance our understanding of urban microclimates and thermal behavior across different LCZ classifications.

1 Introduction

Witnessing the more frequent and noticeable negative effects of climate change in urban environments has become more common during the twenty-first century [1,2,3]. The negative impact has been visible during various hazardous events such as frequent and prolonged heat waves, severe droughts, devastating floods and unprecedented storms [4]. The impact of climate change is felt worldwide, but the most rapid and intense changes are observed in urban areas [5]. Human impact on the environment is becoming more pronounced [6] and the negative aspects are most evident in urbanized environments, where population density is higher, the area is more paved, and vegetation is sparse [7], especially in the most urbanized parts of the cities.

Considering this, in cities, differences arise in structure, surface cover, human activity, and vegetation, which lead to thermal variations at different levels. As a result, Stewart and Oke [8] proposed a classification system for various urban areas called local climate zones (LCZs). Moreover, this framework has been accepted worldwide, and various methods have been developed to improve the localization of these zones within cities. The LCZ scheme consists of 17 different zones, where the zones represented by numbers 1–10 are built types, while the zones denoted by letters A–E include land cover areas of the city [8]. The increasing need to utilize climate zones for various research purposes has led to the necessity of mapping LCZs in cities worldwide [9]. A significant number of European cities already have a map of LCZs, such as Szeged (Hungary) [10,11,12,13,14], Novi Sad (Serbia) [15,16,17,18], Nancy and Dijon (France) [19,20,21], Madrid (Spain) [22], Augsburg (Germany) [23,24], Geneva (Switzerland) [25], Brno (Czech Republic) [26,27,28,29], Oslo (Norway) [30], etc. In all of the these cities various methodologies for LCZs delineation were used, such as remote sensing imagery-based, geographic information systems (GIS)-based, expert knowledge-based, or by using some sort of combined methods [9,31].

LCZ generator, an online platform, was developed to aid in mapping LCZs in cities worldwide [32]. This newly updated system uses training area files and valid metadata to generate accurate LCZs for the required city. The LCZ generator has great potential for the wide collection of data in urban environments, providing automated evaluation of precision. The applicability of LCZs is becoming increasingly diverse; however, the scheme is still primarily used for thermal assessments in European cities as well as in cities around the world. Temperature research conducted in European cities widely used land surface temperature (LST) measurements based on remote sensing [33], datasets from in situ measurements [34], mobile measurements [27], and other methods.

Using the different methods and models to gather data about weather conditions [35] can also help us predict situations that are inevitable [36]. The available data are being analyzed, compared, and monitored [37] to track changes that can be predicted, prevent side effects, and adapt to circumstances as needed [38]. Data can be collected from state meteorological stations, observatories, urban weather stations [17], crowdsourced weather stations [39], various types of mobile instruments (such as cars and bicycles) [21], remote sensing, radar systems, LiDAR and SoDAR [40], and more. In many European cities, urban meteorological stations have been implemented, with a developed network that ensures data are consistent and almost regularly updated. However, gathering all-encompassing data remains a challenge, particularly in obtaining data from urban meteorological stations [41] and state observatories.

Therefore, the aim of this review is to present applications of the LCZ classification concept in European cities, focusing on air temperature differences both inter- and intra-urban. Furthermore, publications utilized in situ or mobile monitoring campaigns to provide air temperature datasets that can demonstrate the suitability of the chosen LCZs in the studied cities.

This study is structured around the following objectives: (a) to present the methodology used in selecting relevant literature on LCZ studies conducted in European cities (2012–2024); (b) to provide, in the results, thorough analysis of the selected literature, including bibliometric analysis and an overview of data collection methods, whether based on in situ or mobile measurements, or combined with other types of methods. This includes a comparative analysis of LCZs across selected European cities, with particular attention to the urban heat island (UHI) phenomenon, outdoor thermal comfort (OTC), nocturnal air temperatures, and other related factors, as well as the application of the LCZs framework; (c) to discuss the main objectives of the collected articles and present the advantages and disadvantages of the most commonly used methods; and (d) to conclude with a summary of the key findings and an outline of potential future directions and improvements related to urban resilience.

2 Methodology

The search methodology action includes gathering, appraising, and examining scientific articles and it involves three phases, which are literature search using specific keywords within Scopus database, literature selection by applying inclusion criteria, and literature classification according to the reported results.

2.1 Literature search and selection

A comprehensive screening process initially involved determining the keywords used to identify and include relevant articles that best aligned with the review’s research topic. Filters applied during the literature selection process within Scopus database (https://www.scopus.com; assessed on 3rd April 2024) included document types (e.g., articles and review papers). The exclusive use of the Scopus database for the literature search was justified by the findings of Lehnert et al. [9], which showed that Web of Science (WoS) and Scopus produced comparable results. Therefore, for the purposes of this research, Scopus was considered sufficient.

This review primarily focuses on articles that pivot on researching “local climate zones.” After the introduction of the LCZ framework in 2012 by Stewart and Oke [8], research within this scientific field expanded significantly over the following years. Therefore, the term was selected as the primary keyword for the literature search through the Scopus database. Additionally, articles that implemented in situ and mobile meteorological stations were included in this review. The data collected from in situ and mobile weather stations across cities in Europe are used to determine the accuracy of the abovementioned LCZs. Moreover, the second keyword established for literature selection through Scopus was decided to be the “measurement,” which allows us to select papers that are related to data collection through field measurements (e.g., in situ and mobile measurements). Given the inter- and multidisciplinary nature of LCZ with diverse methodologies applied, the keywords were chosen to eliminate articles that were not suitable to answer the objective of the review.

The time range that is used for the literature selection obtained articles from 1st January 2012 to 3rd April 2024. The year 2012 is marked as the starting point for the search because the framework of “local climate zone” was established and introduced during that year [8].

Database literature search was conducted in April 2024, consisting of several steps.

The first step in the selection process involved searching for articles containing previously identified keywords (LCZs and measurements) through Scopus by applying the “search within all fields” function, which provided 75 articles.

In the second step, filters were applied to narrow down the search within the specified time range mentioned above. The document types selected for the search included articles and review papers, while conference papers, editorials, etc., were excluded. Considering that this review focuses on cities in Europe, only this geographical area was included, while the cities in countries from other continents were excluded. Additionally, only articles in the English language were considered in this literature selection, while articles in other languages were eliminated. These non-English publications constitute a small portion of the total and often reflect content similar to studies already published in English by the same authors. Applying these filters resulted in a significantly reduced number of papers, specifically totaling 45 articles.

The third step in evaluating relevant articles involved reviewing the titles, keywords, and subsequently the abstracts of the articles. Through this examination process, it can be determined whether, among the 45 articles in the database, there might be articles that do not pertain to the European continent, focus on remote sensing or GIS, do not apply LCZs as the main subject of research, or the articles do not fulfill the criteria. Occasionally, during the search process, the system may make errors and inadvertently contain articles that do not align with the keywords specified in the filters. After a more detailed examination, it was found that one study only mentions the term “local climate zones” without encompassing measurements and data obtained in those areas, while the other articles completely correspond to the relevant publications. At the end of the third step, there were 44 studies that were assessed for eligibility.

Nevertheless, the fourth and final step involved the “snowballing method” [42], which gave good results as well. Through the review and analysis of the selected studies for this article, additional relevant studies were identified by examining the references cited by the authors. By employing this method, 17 additional articles were identified from reviewed articles that aligned with the filters, but were not initially found during the Scopus search. At the end of the selection, the database used for this review contained 61 articles. The entire process of selecting articles described above, and their illustration is made by following the PRISMA concept (Figure 1). PRISMA stands for Preferred Reporting Items for Systematic Reviews and Meta-Analyses. It was developed to improve the reporting of systematic reviews and meta-analyses by helping authors present their work in a complete, transparent, and clear way [43].

Figure 1 
                  Procedure PRISMA chart of the literature selection using selected keywords in Scopus and applying snowballing method [43].
Figure 1

Procedure PRISMA chart of the literature selection using selected keywords in Scopus and applying snowballing method [43].

2.2 Inclusion criteria

The classification of the articles was achieved with the use of the two keywords “local climate zones” and “measurements,” where the keyword “local climate zone” is the primary one.

In order to visually present the analysis required for this review, we used VOSviewer (version 1.6.18.0). VOSviewer is a software that is employed to create various illustrative maps using data from multiple databases [44]. VOSviewer utilizes data from several databases, while for this purpose bibliometric data were obtained from the Scopus database. Additionally, all 61 selected articles are presented in detail through the Supplementary materials (Table S1).

The obtained outcomes are presented in the following text through annual trends in keyword application, keyword co-occurrence trends in chosen articles, journal distribution and publication trends, and article citation frequency.

2.3 Classification of applied measurements in LCZ studies

This review is based on data obtained in two ways:

(a) In situ measurements – Data obtained from in situ weather stations are an important part of understanding a thermal condition in local scale. The data obtained through these measurements include day and night oscillations of various meteorological parameters, as well as consistent data throughout the year; (b) Mobile measurements – This type of measurement includes the most diverse areas that correspond to the local- or microclimate conditions in the city. Mobile measurements can also be used in any part of the day, and can even refer to data collection in motion (bicycle, cart, etc.) to identify variations that in situ station might lack.

3 Results

3.1 Bibliometric analysis

Annual trends in keyword application were analyzed in order to observe the frequency of applied keywords, as well as the combinations in which they were used and their purposes. Considering that research needs have arisen over the years, the articles were divided in two time periods. The aim was to point out variations in keyword occurrences across these two intervals from the beginning to the end of the observed period. The first period is from 2012 to 2018 and the second from 2019 to 2024. During this time range, the occurrence and appearance of keywords progressed over the years and the most used ones are mentioned in the following sentences. The analysis was performed using VOSviewer (Figure 2).

Figure 2 
                  Analysis of authors’ keyword occurrence in selected Scopus articles (2012–2024) using VOSviewer. Circles represent the keywords used in the set of articles chosen for the review. The size of each circle indicates the frequency of the term (larger circles mean the term appears more frequently in the selected articles). The color of each circle represents the average publication year of the articles that used that keyword. Blue circles correspond to keywords used around 2014, green around 2018, and yellow indicate more recent usage. Lines connect terms that co-occur frequently in the same articles. The thickness of each line represents the strength of the co-occurrence (thicker lines indicate the terms appear together more often). The color of the lines (blue, green, and yellow) indicates the time period of co-occurrence between keywords, showing temporal relationships between frequently associated terms.
Figure 2

Analysis of authors’ keyword occurrence in selected Scopus articles (2012–2024) using VOSviewer. Circles represent the keywords used in the set of articles chosen for the review. The size of each circle indicates the frequency of the term (larger circles mean the term appears more frequently in the selected articles). The color of each circle represents the average publication year of the articles that used that keyword. Blue circles correspond to keywords used around 2014, green around 2018, and yellow indicate more recent usage. Lines connect terms that co-occur frequently in the same articles. The thickness of each line represents the strength of the co-occurrence (thicker lines indicate the terms appear together more often). The color of the lines (blue, green, and yellow) indicates the time period of co-occurrence between keywords, showing temporal relationships between frequently associated terms.

Articles that were published in the first half of the obtained period (2012–2018) used the keywords such as “local climate zones” as the most occurred keyword, as well as “urban climate” and “urban heat island.” Nonetheless, keywords that had more appearance in this time range, beside the three abovementioned keywords, are “monitoring network,” “urban meteorological network,” and “mobile measurements”. Furthermore, the keyword “air temperature” and “local climate zone” in the vast majority of cases were applied together, as well as “urban heat island.”

The first period of analyzing the keywords shows a remarkable growth in urban climate studies, where the methodology was mostly based on using monitoring networks to understand the occurrence of UHIs in LCZs and their relationships. Additionally, during this period, both in situ and mobile measurements were used, indicating a desire to present increasingly diverse data since the LCZ framework became publicly available. Furthermore, there is no noticeable use of various analytical tools such as MUKLIMO_3, regression analysis, or even LST measurements, which suggests that remote sensing and its application to LCZs was not widely adopted during the initial period of keyword analysis.

Moreover, in the second part of the following period (2019–2024) the main keywords were the same as in the first period, with the difference where “urban heat island” is more frequently used than the term “local climate zone.” In most of the studies the keywords “local climate zone” and “urban heat island” were used together in combination with “land surface temperature,” “satellite,” and “surface heat island” because the use of remote sensing data increased during the following years.

In the second period of analysis, a clear shift can be observed in the methods used to study urban climate. Unlike the first period, remote sensing has become widely used in articles focused on understanding the UHI. Moreover, in recent years, urban planning and surface measurements, as well as crowdsourcing, have contributed to the development of urban climatology and a broader understanding of this type of research, along with the adoption of alternative methods.

The most notable difference between these two periods is that in the second part of article selection, there was significantly more keywords related to citizen weather station and citizen weather network and citizen science. This reflects a broader temporal shift in research focus, as terms related to citizen science have become increasingly common, likely due to extensive EU funding in this area, where including such components is sometimes even mandatory. It can be concluded that during the last few years, the interest for the mobile measurements such as citizen stations rise which broadened many horizons and created a new spectrum of research into LCZs and urban climate. It has been noticed that in the previous years, the combination of mobile in situ measurements on one side and remote sensing and GIS on the other side increased during the second observed period.

Further, co-occurrence of keywords was analyzed. The selected articles for the review were visualized using VOSviewer (Figure 3). This concept, which is part of the bibliometric analysis used in this study, illustrates how frequently different keywords appear together. A fundamental aspect of the visualization is to highlight the application of LCZ scheme across various areas of the research field.

Figure 3 
                  The keyword co-occurrence network in selected articles from Scopus. Each circle represents an author keyword used in the selected articles. The size of each circle indicates the frequency of that term’s occurrence (larger circles mean the term appears more frequently as an author keyword). Colors (blue, green, and red) are used to group keywords into clusters based on their co-occurrence patterns. Keywords within the same color cluster are more closely related to each other, forming thematic groups or research subfields within the dataset. The lines between circles represent connections between keywords. More frequent keyword combinations across multiple studies produce thicker lines, while less frequent combinations are shown with fainter lines. The color of a line (e.g., green, blue, or red) indicates a group of words that are often associated together.
Figure 3

The keyword co-occurrence network in selected articles from Scopus. Each circle represents an author keyword used in the selected articles. The size of each circle indicates the frequency of that term’s occurrence (larger circles mean the term appears more frequently as an author keyword). Colors (blue, green, and red) are used to group keywords into clusters based on their co-occurrence patterns. Keywords within the same color cluster are more closely related to each other, forming thematic groups or research subfields within the dataset. The lines between circles represent connections between keywords. More frequent keyword combinations across multiple studies produce thicker lines, while less frequent combinations are shown with fainter lines. The color of a line (e.g., green, blue, or red) indicates a group of words that are often associated together.

The keyword visualization in VOSviewer (Figure 3) illustrates how often keywords co-occur within the selected articles. For example, keywords highlighted in blue, such as “heat island,” are mostly associated with terms like “crowdsourcing,” “measurement method,” “microclimate,” and others.

Therefore, the visualization of the literature selection reveals that the keywords local climate zones, urban climate, urban heat island, and air temperature stand out, exhibiting numerous links to various frequently used keywords represented as smaller nodes (circles). This connection shows the strong association with terminology from urban climate, linking the different urban networks conducting in situ and mobile monitoring.

The keyword “urban heat island” has a total link strength of 86 connections, while “local climate zones” has 67 links to several keywords presented in Figure 3. “Urban climate” and “air temperature” also show significant associations with the same keywords with the total link strength of approximately 50, while the others have less than 20 or do not have a notable linkage.

In Figure 3, three different clusters can be seen in red, blue, and green. Red cluster is focused on terms such as LCZs, UHI, LST, climate change, atmospheric temperature, and urbanization. This suggests a focus on the physical aspects of urban climate change and measuring the temperature effects of urbanization, while the green cluster is dominated by keywords like urban climate, air temperature, environmental monitoring, relative humidity (RH), and climate modeling. It appears to be more oriented toward quantitative methods, modeling, and the measurement of microclimatic characteristics in urban areas. Moreover, the blue cluster is connected to topics such as heat island, urban planning, crowdsourcing, dataset, and measurement method. This cluster places more emphasis on methodology, data management, and urban planning aspects.

There is a clear inter-cluster connection, particularly between the red and green clusters, through nodes such as air temperature, climate conditions, and LCZ. This indicates an interdisciplinary nature of the research, where physical measurements are closely linked with modeling and urban planning contexts. The blue cluster is slightly more peripheral, although it is connected to others through methodological terms, which implies that methodological innovations are only partially integrated into the broader thematic areas. The size of the nodes indicates the frequency of keyword usage where UHI, urban climate, and air temperature are dominant, suggesting their central role in the chosen literature.

There are still some limitations to this figure, such as overlapping in terms. Additionally, the red cluster is quite dense, which can make it harder to read individual terms. Applying filters based on term frequency might improve the overall readability of the map.

Journal distribution and publication trends were examined by reviewing all 61 articles selected for this study, it was found that some journals published a higher number of these articles than others. Table 1 presents a summary of these journals, organized by the quantity of articles they contributed to the review.

Table 1

Distribution of articles by journals. The first row shows the total number of journals where the selected articles appeared, the second row lists the names of these journals, and the third row indicates how many articles from each journal were included in the study

Journal Number of articles
1 Urban Climate 11
2 Hungarian Geographical Bulletin 5
3 Geographica Pannonica 4
4 Theoretical and Applied Climatology 4
5 International Journal of Climatology 3
6 Atmosphere 2
7 Building and Environment 2
8 Climate 2
9 Climate Research 2
10 Idojaras 2
11 ISPRS International Journal of Geo-Information 2
12 Meteorologische Zeitschrift 2
13 Remote Sensing 2
14 Sustainable Cities and Society 2
15 Climatic Change 1
16 Energy and Buildings 1
17 Environmental Monitoring and Assessment 1
18 Environmental Research Letters 1
19 Geography, Environment, Sustainability 1
20 Geoscientific Model Development 1
21 International Journal of Biometeorology 1
22 Natural Hazards 1
23 Quarterly Journal of the Royal Meteorological Society 1
24 Remote Sensing of Environment 1
25 Science of the Total Environment 1
26 Scottish Geographical Journal 1
27 Sustainability 1
28 Sustainable Futures 1
29 Urban Forestry and Urban Greening 1

It is observed from the database of articles used in this research that the majority of articles, in which this subject area was most recognized, were published in the journal Urban Climate, with as many as 11 articles, which is twice as many as in the second-ranked journal, the Hungarian Geographical Bulletin. Given that a larger number of articles were published in the journal Urban Climate, it is important to highlight that this journal serves as the dominant platform where the scientific community converges around the topic. This reflects a clear trend within the field. Consequently, a significant portion of the relevant literature included in this review is published in Urban Climate, which aligns closely with the central focus of this research on urban climate, covering topics such as the UHI effect, OTC, and related issues. In contrast, other journals listed in Table 1 contain noticeably fewer articles included in this review. This is primarily because their research focus tends to diverge toward different aims, such as urban design, remote sensing, energy systems, and other related fields.

Following these are the journals Geographica Pannonica, Theoretical and Applied Climatology, and International Journal of Climatology, while the other journals have fewer than three published articles in the database.

Moreover, article citation frequency highlights the most significant publications by the number of citations and it is shown in Table 2. The most cited articles [19,45,30] focus on analyzing urban air temperature variations through diverse data sources, methodologies, and climate classification systems. They focus on mapping LCZs, evaluating the influence of urban characteristics on thermal patterns, and exploring adaptation strategies to enhance thermal comfort in European cities.

Table 2

Ten most influential articles by citations. The last check of citation is 13.10.2024

Refences Title Citations Authors
[19] Using Local Climate Zone scheme for UHI assessment: Evaluation of the method using mobile measurements 206 Leconte et al.
[45] Counteracting urban climate change: Adaptation measures and their effect on thermal comfort 198 Müller et al.
[30] Hyperlocal mapping of urban air temperature using remote sensing and crowdsourced weather data 113 Venter et al.
[39] Intra and inter ‘local climate zone’ variability of air temperature as observed by crowdsourced citizen weather stations in Berlin, Germany 105 Fenner et al.
[26] Modelled spatiotemporal variability of outdoor thermal comfort in local climate zones of the city of Brno, Czech Republic 94 Geletič et al.
[23] Air temperature characteristics of local climate zones in the Augsburg urban area (Bavaria, southern Germany) under varying synoptic conditions 68 Beck et al.
[73] Using LCZ data to run an urban energy balance model 66 Alexander et al.
[17] Heat wave risk assessment and mapping in urban areas: case study for a midsized Central European city, Novi Sad (Serbia) 44 Savić et al.
[64] Micro-scale variability of air temperature within a local climate zone in Berlin, Germany, during summer 41 Quanz et al.
[9] Mapping local climate zones and their applications in European urban environments: A systematic literature review and future development trends 41 Lehnert et al.

Moreover, the prominence of certain authors is highlighted in Figure 4. Authors are marked in yellow to indicate their influence, considering both primary and co-authorization. The most cited researcher is Oke T.R., with 166 citations. Unger J. and Gal T. also have more than 100 citations each, while the remaining authors have fewer than 100 citations (citation last check 13.10.2024).

Figure 4 
                  Visualization of authors citation. Warmer colors represent areas of higher citation density, larger font size indicates authors with more citations, and the distance between names reflects the strength of their co-citation relationships.
Figure 4

Visualization of authors citation. Warmer colors represent areas of higher citation density, larger font size indicates authors with more citations, and the distance between names reflects the strength of their co-citation relationships.

The geographical scope of the study covers a large domain covering the continent of Europe, involving more than ten countries (Figure 5).

Figure 5 
                  Contribution of articles per country. The quantity of collected studies for review is represented in shades of purple. Countries shown in white indicate that no articles were found, while progressively darker shades correspond to a greater number of studies retrieved from that country.
Figure 5

Contribution of articles per country. The quantity of collected studies for review is represented in shades of purple. Countries shown in white indicate that no articles were found, while progressively darker shades correspond to a greater number of studies retrieved from that country.

Figure 5 shows that out of the 61 studies selected for this review, as many as 10 were conducted in Germany, with research primarily concentrating on cities such as Oberhausen, Berlin, Augsburg, Freiburg, etc. Thus, the majority of research was concentrated in German cities. Following Germany, Hungary contributed nine studies, with most research carried out in Szeged. Serbia had eight studies, where Novi Sad was the most frequently researched city. Additionally, seven studies from the Czech Republic were included, with the research largely focusing on Brno and Olomouc. Research conducted in cities in Italy and France was also part of the review, accounting for six and four studies, respectively. Both Ireland and Switzerland had more than one article included.

The map of publications reveals a strong concentration of research outputs within specific regional networks, primarily in Germany, with few local networks based in Hungary, Czech Republic, Serbia, etc. This uneven geographical distribution introduces a potential spatial bias in urban climate analysis, as less-studied regions may possess climatic characteristics that are underrepresented in current datasets. Such bias could limit the generalizability of findings and highlight the need for expanded research efforts across a broader range of urban environments worldwide. This limitation also affects the applicability and robustness of the LCZ classification system, as it relies on diverse urban contexts to fully capture local climate variability.

3.2 In situ measurement-based studies

The collected data from in situ stations enables the recognition of similarities and differences among LCZ. An analysis of the chosen literature shows that most research is based on data collection from in situ stations, such as urban networks, national observatories, or CWS. Additionally, Lehnert et al. [9] and Migliari et al. [46] presented similar methodological approaches for studying urban climate phenomena, including thermal analysis based on mobile and in situ measurements within the LCZ framework.

Several studies [12,15,18,22,47,48,49,50] have focused on investigating the spatiotemporal variations of UHI in cities across LCZ. Multiple studies that used in situ measurements [10,12,18,22,51] has shown that built-up areas with high building density and impervious surfaces (e.g., LCZ 2) record the highest UHI intensities, while natural (LCZ and A) or less dense zones (LCZ 6) remain cooler, especially at night. The maximum UHI intensity is typically reached a few hours after sunset. Unger et al. [10] concluded that the greatest differences between LCZs occur before dawn, with temperature differences reaching up to 5°C during early spring. The intensity of temperature differences among LCZs can vary depending on the city, duration of the measurements, instruments used, as well as local characteristics and the spatial and temporal variability of the UHI effect. For instance, while LCZs 2, 3, and 5 exhibit the strongest summer UHI, they can still be cooler than other zones during daytime. Moreover, heating rates differ significantly, illustrating the complex and dynamic nature of urban thermal patterns. The importance of multiple factors is evident, as shown in the study by Dunjić et al. [52], where it was demonstrated that air temperature dynamics correlate with air humidity, and that the urban dry island (UDI) effect is strongest during the day and evening, especially in LCZ 2, with lower values observed in the afternoon in LCZs 5, 6, 8, and 9 in Novi Sad, Serbia. This type of study highlights the necessity of analyzing and understanding not only air temperature but also humidity, in order to capture changes in other indices such as UDI, which is essential for comprehending the UHI effect, as these phenomena are directly linked. Savić et al. [17] monitored the nocturnal UHI in Novi Sad, highlighting that LCZs 2, 5, and 6 exhibited very high or high risk values, which were associated with a higher rate of mortality. The findings show that nighttime heat in densely built areas can seriously impact health, pointing to the need for more research on how UHI varies across cities and how it is connected to mortality.

A few articles used combination of in situ data with different data collection methods. Varentsov et al. [50] combined thermal satellite images and mesoscale modeling, while Feng et al. [53,54] used a combination of MODIS observations and two urban meteorological networks to explore the relationship between surface UHI intensity and canopy heat island intensity. Boccalatte et al. [25] combined sensor data with modeling approaches at various scales (local, city, street, etc.). Núñez-Peiró et al. [22] and Unger et al. [10] combined urban networks and official stations. Combination of different measurement methods, as presented previously, provides a more complete understanding of urban climate phenomena and highlights the strengths of each technique. However, even this combination can have limitations, such as inconsistencies between data sources, differences in spatial or temporal resolution, and remaining gaps in data coverage. These challenges should be improved in future research methodologies, along with finding better ways to reduce these biases.

Some articles showed the innovative method approaches such as modeling which have improved UHI assessment accuracy. Agathangelidis et al. [55] found that UHeatEx better captures urban spatial heterogeneity in Athens compared to LCZ mapping, especially when analyzing T min data from five LCZ 2 stations. This study shows the importance of innovative approaches in understanding urban microclimates, as it is one of the few that uses complex modeling methods to improve UHI assessment. The limitations of such models, such as the impact of spatial resolution and input data quality on the outcomes, must be carefully taken into consideration. Núñez-Peiró et al. [56] showed that using UHI intensity as a model input, rather than air temperature, led to much better results and improved modeling results. The results suggest a potential to make urban climate research more efficient by minimizing the time and expenses required for field measurement campaigns.

OTC has been one of the prime topics for articles that for their investigation used in situ measurements. Milošević et al. [57], Unger et al. [58], and Müller et al. [45] used a thermal comfort index PET (physiological equivalent temperature) to monitor different LCZs in cities such as Novi Sad (Serbia), Szeged (Hungary), and Oberhausen (Germany), respectively. Geletič et al. [59] assessed OTC in Brno during a heatwave using MUKLIMO_3 and urban climate data, evaluating HUMIDEX based on air temperature (Ta) and RH, and found that the most built-up LCZs (2, 3, 5, 8, 10) were the least comfortable. Šećerov et al. [60] provided thorough analyses of air temperature, RH, and OTC. Their study found that LCZ 2 recorded the highest temperatures and the lowest levels of thermal comfort during the measurement period, while natural LCZs (A and D) offered the most comfortable conditions on site. While these studies effectively illustrate that highly built-up LCZs (such as LCZ 2, 3, 5, 8, and 10) tend to be less thermally comfortable and often validate the expectations of the LCZ framework, the magnitude of discomfort can vary significantly depending on the duration of heat events, local adaptation measures, and uncertainties in OTC indices, all of which require further investigation.

Researchers often do not discuss how inconsistencies in defining or mapping LCZs, or variations within each zone, might affect their results or make it difficult to compare findings across studies. The study that does discuss is the one by Briegel et al. [61], who applied the human thermal comfort neural network machine learning model, highlighting both inter- and notably intra-LCZ variability, with distinct universal thermal comfort index distributions between old and new building districts despite similar characteristics. This demonstrates the importance of analyzing intra-LCZ differences due to specific characteristics; in this study, it is a building age. Guerri et al. [62] evaluated thermal stress in one of the warmest areas of Florence, Italy, focusing on the main agri-food market (LCZ 8) to test three tree-based mitigation scenarios. They used in situ microclimate monitoring, urban characterization, and spatial analysis with GIS tools (QGIS) and microclimate simulations (ENVI-met) to analyze thermal patterns. Their research shows that the LCZ framework can be used for more than just simple classification, it can also help plan targeted urban interventions. But, like many other studies based on LCZ, it does not fully address the uncertainty in the accuracy of LCZ mapping or the differences between zones, which could affect the effectiveness of microclimate modeling and mitigation.

One of the primary focuses in research on LCZs is air temperature in different urban settings. Therefore, studies on inter- and intra-LCZ air temperature differences have been conducted in several cities, such as Berlin (Germany) [63,64], Olomouc (Czech Republic) [65], Brno (Czech Republic) [26], Augsburg (Germany) [23], Szeged (Hungary) [14,66], and Novi Sad (Serbia) [11]. These investigations revealed a consistent difference between built-up LCZs during the day and night, with especially high differences observed at night. Most authors highlighted nighttime temperature differences as the most significant, while Fenner et al. [63], Lehnert et al. [65], Skarbit et al. [66], Beck et al. [23], and Fricke et al. [14] analyzed the nighttime temperatures and found that they were considerably higher in built-up LCZs compared to non-built-up LCZs, with LCZ 2 standing out, as expected. Geletič et al. [26], Lehnert et al. [65], Fricke et al. [14], Skarbit et al. [66], and Quanz et al. [64] showed that nighttime urban heat is most pronounced in LCZs 2, 3, 5, 6, 8, 9, 10, and E, with particularly high temperatures found in compact built areas, especially LCZ 2B with dense courtyards and minimal vegetation. It has been observed that even within the same LCZ class, urban and rural settings can behave differently. Urban canopies may dampen short-term weather fluctuations more effectively than exposed locations. This means that some LCZs, although conceptually warmer, can show milder thermal responses depending on vegetation, sky view factor (SVF), or enclosure. Wind also plays a significant role, as it can increase variability and reduce thermal stress. To avoid the influence of micro-scale characteristics, LCZs of different classes should not be directly compared through single points. Within subclasses, geometric layout should also be considered.

In this review, several relevant articles that used CWS data were identified, focusing on the analysis of temperature differences between LCZs in cities such as London (England), Berlin (Germany), Oslo (Norway), and Bern (Switzerland). Brousse et al. [67] analyzed air temperature in London using data primarily collected from CWS. Moreover, some studies highlight the importance of combining CWS with other methods, such as networks of low-cost instruments [68], urban networks [39], remote sensing techniques [30,69], and modeling approaches to more effectively analyze and interpret the data. Citizen weather stations have gained popularity in recent years due to their affordability, higher density, and placement in areas with high population density. They can be deployed across different locations within the same LCZ, capturing variations in parameters and providing temperature data year-round under all weather conditions, resulting in a broad and rich database. However, crowdsourced instruments have negative aspects as well, such as less representation of natural LCZs and inconsistencies caused by diverse setups. Despite these challenges, the dense and widespread nature of crowdsourced instruments allow for detailed investigation of temperature variability within LCZs, which is influenced by local urban structure heterogeneity and larger-scale urban influences. Addressing biases through comparison with nearby established stations can enhance the reliability of crowdsourced data for urban climate analysis.

In several cases, data from official stations served as the primary source for analysis [10,13,22,29,49,50,56,59,69,70]. Other studies combined official station data with additional sources, including urban network stations [10,22,59,70], EURO-CORDEX model simulations [13,29], and remote sensing technologies [48,49,71,72]. Alexander et al. [73,74] applied the LCZ framework in a different context, combining data from the meteorological station at Dublin Airport with urban energy flux measurements. Bokwa et al. [28] carried out a study on heat load in Central European cities using a combination of urban climate modeling and observational monitoring data. On contrary, Bechtel et al. [75] highlighted the importance of using remote sensing independently, without relying on data from in situ or mobile instruments, thereby enhancing the potential for alternative data collection methods. Nonetheless, Šečerov et al. [16] noted that long-term in situ measurements are essential for capturing thermal variations in different urban settings. These data can help compare temperature differences both within the same city and between different urban areas, providing valuable insights into the urban climate, especially in the canopy layer.

Using in situ measurements for investigating UHI and OTC, as well as for calculating various indices and indicators, can be an effective approach. When positioned at designated measurement points within or around LCZs, in situ measurements can improve our understanding and analysis of these values. They also allow us to gather data over specific time periods (daily, nightly, weekly, monthly, seasonally, or annually), which helps collect the necessary information for thorough analysis. Nonetheless, in situ measurements come with certain drawbacks. It is often the case that in situ stations are set up as part of a specific project and once the project ends, the instruments are neglected and measurements are no longer continued at those locations.

Moreover, in situ stations sometimes fail to cover all parts of an LCZ properly, especially considering that differences exist even within the same LCZ. Another issue is that these stations are often placed where they will not disturb people, sometimes at a height above human level, which means they do not fully reflect the actual thermal experience at ground level or the areas where people are constantly moving. In situ measurements also do not capture the short-term, moment-to-moment changes in human thermal perception, especially when walking through different parts of an LCZ, for example, under a tree, next to a building, or near a glass facade. Therefore, they may not be suitable for certain types of environments.

Combining in situ data with remote sensing and LST measurements helps improve temperature monitoring and enhances the calculation of bioclimatic indices. This approach is also visually easier to interpret. The introduction of CWS, supported and increasingly implemented through EU initiatives, is helping to expand measurement coverage, particularly in areas with high population density.

3.3 Mobile measurement-based studies

The use of mobile instruments allows for the monitoring of dynamic conditions, enabling the rapid collection of data at multiple points within or between different LCZs.

Several studies [19,20,21,27,76,77,78] have used car-based measurements for different purposes. Leconte et al. [19,20,21] emphasized that when using instruments on vehicles, data collected at speeds below 15 km/h should not be used due to heat release from other vehicles, which can affect the measurements, which is why car speeds were in a range of 15–60 km/h. Moreover, Lehnert et al. [27] excluded the measurements on traffic lights where there was influence of heat release in traffic. Leconte et al. [20] found that LCZ 2 and 5 retain more heat due to low SVFs and tall buildings, whereas LCZ 8 and 6/9 exhibit better nocturnal cooling due to more favorable urban morphology. Lelovics et al. [77] confirmed that compact and mid-rise urban areas are warmer than open and low-rise zones, while sparsely built areas showed temperatures similar to rural LCZ classes, validating the link between LCZ types and air temperature.

Skarbit et al. [71] used mobile measurement techniques, incorporating a Citizen weather stations receiver for georeferencing, global positioning system/global navigation satellite system receiver for georeferencing, remote sensing via an airborne thermal camera to collect real-time temperature data, and data from the Hungarian Meteorological Service. Moreover, Herbel et al. [79] conducted a study on detecting the atmospheric urban heat island in Cluj-Napoca, Romania, using a combination of mobile measurements taken from a car and data from in situ stations to enhance the analysis and understanding of the phenomenon.

Bicycle-based measurements are one of the well accepted forms of mobile data collection, chosen for their ability to easily navigate a variety of urban environments. In a study by Lehnert et al. [80], daytime and nighttime temperature measurements were taken to identify hot and cold spots in the city center of Olomouc, Czech Republic. The study found that temperature differences between LCZs were more pronounced at night than during the day. LCZ 2 was consistently the hottest area, making it a hotspot, while LCZ D stood out as one of the coolest locations. On contrary, Emery et al. [81] focused on evening measurements and found that areas with dense vegetation and water bodies likely aid in cooling urban environments at night, potentially reducing the UHI effect.

In a similar manner to the previous research, Rathmann et al. [82] aimed to simultaneously collect data on various relevant characteristics across different urban routes to better understand people’s physiological responses in specific climate conditions. Instead of the method used in earlier studies, this work focused on capturing variations in the thermoregulatory responses of participants during transient thermophysiological states (such as walking) under diverse outdoor conditions. The measurements were taken using a wearable sensor system, with physiological data collected via Microsoft Band 2 wristbands.

Car-based measurements capture temperature and other data while moving but these measurements alone do not show pedestrian routes even though pedestrians are the people most affected by thermal conditions and their routes are largely influenced by the urban environment. Although the variations may be minimal factors like shading and SVF can still introduce bias. Furthermore, studies have shown that LCZ classification is a more important factor than distance from the city center in explaining the UHI effect and that temperature variability within LCZ classes is linked to city size and topographic diversity.

Furthermore, mobile measurements such as those conducted by bicycle or with devices like wearable sensor systems provide better results for the surrounding environment and pedestrians. Bicycle paths are often located right next to pedestrian walkways, presenting a slightly different situation during measurements and enabling more accurate results under certain climatic conditions. In addition, bicycles and certain devices do not contribute to an increase in the surrounding air temperature, as is the case with cars, although a potential factor may be the influence of stronger wind if the cycling speed is higher than walking speed, which directly affects the perception of the environment. Moreover, bicycles and wearable devices allow better access to various locations along the route, while cars are limited to roads. Therefore, it is very difficult to determine the type of mobile measurement to be used, as it depends on the specific city, its local structure, population density, and other factors.

Nonetheless, the combination of various methods is the most important aspect of such measurements in order to fill gaps and correct biases during data analysis within LCZs. Some futuristic beliefs and ideas still lead to other types of research and innovations, as studies have shown that LCZ classification offers a better understanding of intra-urban temperature variations compared to land cover classification because it better reflects the differences in urban morphology, vegetation, and different surface characteristics on site. Therefore, there was a proposal to extend LCZs into “local wellbeing zones” to integrate climatic, physiological, and personal factors, which can help to improve strategies for mitigating urban heat stress and enhancing climate resilience.

4 Discussion

Since the LCZ classification became publicly available [8], various approaches and applications have emerged for its use. Although the LCZ system was originally designed to monitor and determine the consistent presence of the UHI effect, its applications have gradually expanded. This includes the advancement of data collection methods, as well as the adaptation of LCZ mapping for a broader range of purposes [9,33].

Through bibliometric analysis, certain trends and changes have been identified over time in the ways LCZs are researched. These include shifts in methods, temporal variations, and evolving applications. The bibliometric study revealed a wide spectrum of diversity across the literature, including variations in keywords, publication journals, the most cited and most read papers, and a progression in both methodological approaches and innovations related to LCZ usage. Additionally, there has been a noticeable increase in the use of various in situ and mobile measurements, often in combination with each other or through the integration of multiple data collection methods (e.g., additional techniques) to better assess the climate characteristics of LCZs.

Throughout the analysis, which was conducted using the Scopus database along with the snowballing method, a total of 61 relevant studies were identified. These studies employed in situ and mobile instruments and often combined them with remote sensing, modeling, and other methodologies. The choice to rely solely on the Scopus database (rather than including, for instance, the WoS) was based on findings indicating that both databases tend to yield similar or even identical sets of articles when filtered by specific keywords and geographic focus (such as Europe) [9]. Furthermore, the snowballing method increased the comprehensiveness of the literature by including a wider range of sources. The review of selected studies and references ultimately contributed to a more robust dataset and increased the quality of the analysis.

The studies selected for this analysis utilized a variety of research objectives, instruments, methods, data sources, timeframes, and regions. Topics such as air temperature differences, the UHI effect, OTC, and related urban LCZ dynamics have been recurring subjects in the literature. These studies applied different tools to demonstrate the practical use of LCZ mapping, including in situ networks (urban networks, governmental instruments, local monitoring stations, etc.) and mobile platforms (vehicles, bicycles, citizen weather stations, among others).

Stationary urban networks, typically based on official meteorological stations or monitoring systems managed by research institutions or academic groups, allow for long-term observations and temporal comparisons of thermal behavior across zones with differing urban structures. These data sources are essential for identifying consistent patterns, seasonal shifts, and daily variations across LCZs. However, while these measurements are reliable, they are often spatially limited and may fail to capture microclimatic diversity within complex urban environments.

There are several limitations associated with in situ measurement stations:

  1. In situ stations are fixed at a specific location, within a single LCZ, and continuously measure parameters relevant to that immediate area;

  2. Stations are frequently placed at only one point within a zone, presenting a generalized representation without considering internal variability or micro-zones;

  3. An uneven distribution of stations across different LCZs may result in biased datasets (for example, built-up areas tend to have a higher concentration of stations, while non-built-up zones often have few or none);

  4. In situ stations are often installed at a certain height (frequently higher attached to poles for electricity access), which may not align with the level at which people experience thermal conditions, potentially reducing the accuracy of human-centered measurements;

  5. Stations are not typically positioned along pedestrian routes, even though pedestrian experiences are often central to urban thermal studies. Instead, they may be located in hidden or inaccessible places that do not reflect real conditions;

  6. When installed as part of temporary projects or grant-funded initiatives, these stations are frequently neglected once the funding ends, especially if local institutions or residents are unwilling to maintain them;

  7. National meteorological stations are generally located outside of urban zones and thus fail to capture the true thermal conditions within cities.

These limitations show why in situ measurements, while valuable, need to be supported by other methods. Proper integration is important to avoid biased results and to allow for accurate interpretation. On the positive side, in situ instruments provide both short-term and long-term data across different seasons, during heatwaves, cold spells, and throughout the day and night, which improves the overall reliability and quality of urban climate research. However, because these stations are fixed, unevenly distributed, and often vary in height and placement, the data they produce can be biased and may not fully represent the conditions of an entire LCZ or several LCZs. This limits their usefulness for accurately mapping microclimatic differences within zones and across cities, and it highlights the need to combine them with other measurement methods that can better capture spatial variability. If these issues are not addressed, the resulting data can lead to limited assessments of UHI intensity, misleading interpretations of OTC, and reduced comparability between cities. This becomes especially problematic in cities with heterogeneous LCZ structures, where microclimatic differences often remain unnoticed.

An important development in in situ monitoring is the increased use of citizen weather stations (CWS), which have improved both spatial and temporal resolution. CWS installations typically cover a greater number of micro-locations within cities. They are situated in densely populated areas, require minimal maintenance by the owners, and operate continuously, offering insight into localized conditions. However, CWS systems also have limitations. Their deployment often depends on external funding or specific projects. Moreover, they are usually installed in urban LCZs, with limited presence in land cover areas. This can introduce biases and reduce the capacity for comparisons across all LCZ types. Despite this, CWS platforms are valuable for analyzing inter-LCZ and micro-local variations, such as differences between shaded and sunlit areas, areas near vegetation, or different surfaces. These comparisons are easier to perform within built-up zones. Nonetheless, the lack of CWS coverage in rural areas limits the ability to compare urban and non-urban LCZs. Since UHI is measured based on temperature differences between urban and rural zones, this creates a bias and diminishes the utility of the data. Although CWS stations significantly improve spatial coverage and help capture micro-local variability, their concentration in built-up areas introduces analytical biases. Biases in CWS data likely result from improper siting near buildings, causing positive nighttime and negative daytime biases, while bicycle mounted mobile measurements and low-cost measurement devices could provide clearer nocturnal temperature patterns. These challenges underscore the need for strategic station placement and complementary data sources.

Mobile measurements also have a significant impact on urban climate and it can be used for different purposes and with different techniques. Compared to in situ measurements, mobile instruments are, as the name suggests, mobile and can collect data while in motion (using bicycles, handheld devices, cars, etc.). They are especially effective in identifying hot and cool spots, assessing intra-urban variability, and detecting short-term thermal anomalies. It can provide different data and it can be used alone, or combined with in situ stations. Studies using mobile surveys have shown their effectiveness in mapping thermal contrasts across multiple LCZs within a single city, particularly during extreme heat events.

However, several limitations affect the accuracy and quality of mobile data:

  1. Mobile measurements are typically short-term and provide data over brief periods, such as during specific times of day or during heatwaves and cold spells which can result in bias;

  2. Handheld devices may also introduce bias, particularly during hot summer days, as body heat, sweat, or humidity from the user’s hand can interfere with the sensor’s performance and influence temperature or humidity readings.

  3. In contrast, fast bicycle rides can artificially increase ventilation, which may reduce or distort heat perception during hot conditions or have little effect during cold spells;

  4. Car-based measurements may be influenced by vehicle emissions, metallic surfaces, and traffic patterns such as idling at lights or varying driving speeds where these factors can affect readings and introduce distortion;

  5. Cars are confined to roadways, away from pedestrian routes, whereas bicycles offer a closer approximation to sidewalk conditions;

  6. Differences in mobile instruments make it difficult to compare data across cities, methods, or devices;

Mobile measurements also offer both advantages and disadvantages. These measurements, conducted with instruments mounted on moving vehicles such as bicycles, cars, or handheld devices, provide high spatial resolution and flexibility for recording data across various locations throughout the city. Handheld devices provide accurate pedestrian-level measurements, as they are directly exposed to local SVFs and microclimatic conditions. During mobile measuring, the route can be diverse, conducting different LCZs, microclimatic differences, vegetation, or pavement cover, as well as the parts with more or less people. Mobile routes can be provided on maps showing the real picture of the LCZ and be useful in analysis. Although mobile measurements provide valuable insights into spatial temperature variations, their fragmented nature and methodological inconsistency require cautious interpretation. It is essential to integrate these results with long-term in situ data to avoid misinterpretations or non-comparable conclusions about urban microclimates.

As with in situ measurements, it is important to combine different measurement types, include reference stations where needed, utilize in situ data, and employ satellite imagery for broader spatial context. Comparative analysis of these two measurement approaches within the LCZ framework emphasizes the necessity of methodological integration. By combining in situ and mobile instruments, remote sensing techniques, and CWS data, researchers can achieve a more comprehensive and accurate assessment of thermal environments in urban areas. This integrated approach is especially important for urban climate adaptation strategies and for planning more resilient urban designs.

The results clearly confirm that built LCZs (such as LCZ types 2, 3, 5, 6, and 9) consistently experience the highest thermal loads, elevated nighttime temperatures, and strong UDI effects. Conversely, natural LCZs (A through D) serve as thermal refuges that help mitigate extreme heat. This spatial differentiation within cities is critical for planning targeted interventions, such as increasing green spaces, improving water infrastructure, and optimizing urban layouts to reduce thermal stress. Nevertheless, the differences between LCZs continue to raise questions. Although studies generally confirm that heavily built LCZs (such as types 2, 3, 5, 8, and 10) are less thermally comfortable and align with LCZ expectations, the extent of thermal discomfort can vary considerably depending on the duration of heat events, local adaptation measures, and uncertainties in thermal comfort indices. These variations call for further investigation and refinement in urban climate research.

Research on temperature measurements, whether in situ or using mobile methods, shows that the focus is mostly on daytime measurements. Long-term databases are most often used, with series lasting more than 3 years, and especially periods of heat waves are studied. Results indicate that daytime temperature differences between LCZs in built-up urban areas are decreasing, largely matching the existing LCZ classification, with occasional exceptions where some zones are warmer than expected.

In situ data are mostly obtained from national meteorological stations, while CWS networks are becoming increasingly common. Mobile measurements are also frequent, especially during the day, when shading, vegetation, and varying levels of solar radiation cause larger temperature differences. In this context, recent research increasingly highlights the concept of climate shelters, which present spaces adapted to climate change, designed to provide safe refuge and thermal comfort during the hottest parts of the day. These spaces use shading, green areas, water elements, and improved ventilation, and are intended for vulnerable groups as well as the general public.

At night, mobile measurements are rarer, although they can reveal important patterns. However, given the growing urbanization and heat accumulation during nighttime hours, nighttime measurements could provide valuable insights into ventilation conditions, wind influence, and human presence at specific locations, which is crucial for identifying “stress” points.

In addition to daily measurements, seasonal, annual, and decadal measurements are also conducted, most often using data from in situ stations because they provide a higher volume and longer time series of data. Mobile measurements are not carried out in this way and therefore, have certain limitations, such as lower temporal coverage, spatial inconsistency, and difficulty in capturing long-term trends. There are only a few studies that analyze mobile instrument measurements conducted over multiple days [80,81], highlighting the limited temporal scope in current mobile measurement research. A combination of these methods is often recommended.

Daily measurements have shown differences between built-up LCZs as well as between land cover ones, with the greatest focus on comparisons among built-up LCZs (1–10) and between built-up and land cover LCZs (A–E). However, shortcomings have been observed in comparing land cover LCZs, specifically within the range from LCZ A to LCZ E. This trend was also noted in nighttime measurements.

Several reviews [9,35,46,83,84,85,86,87,88] have investigated different aspects of the LCZ framework, such as bibliometric analysis [83,84], mapping methods [9,87], and its overall status and future outlook [86]. Han et al. [85] discussed progress and remaining challenges in methodology, while Xue et al. [84] noted that most research focuses on how land use and urban form affect urban climate, with a recent shift toward thermal environments and heatwaves. Fan et al. [83] pointed out that human exposure to heatwaves is still not well studied, with only one relevant article found [82]. Lehnert et al. [9] highlighted that the high spatial variability in European environments makes it hard to get representative data for local zones. This shows the need for a clear, standardized, and widely accepted LCZ classification system, supported by consistent urban data, to help improve both research and practical use.

LCZs have helped urban studies by improving data collection and standardizing study areas. Still, challenges remain with data availability and classification accuracy, though deep learning methods seem promising. Migliari et al. [46] found that cooler LCZs are not always more comfortable because OTC depends on more than just air temperature. LCZ 5 (open midrise) was the least comfortable, while LCZ 9 (sparsely built), LCZ 4 (open high-rise), and LCZ 6 (open low-rise) ranked better, with natural LCZs A (dense trees) and G (water) performing best.

Although the previously reviewed articles [83,84,85,86,87,88] provide valuable insights into the development of the LCZ framework, with a focus on bibliometric trends, mapping methods, and conceptual improvements in classification, it can be observed that most of them remain theoretical and do not address the practical challenges of applying measurement techniques in urban environments. These studies mostly concentrate on classification approaches, the use of remote sensing, or the integration of LCZs with various models, while the critical evaluation of measurement methods, such as in situ and mobile data collection, is often limited or entirely missing. Unlike these studies, this research places greater attention on the actual application of measurement tools within the LCZ framework, emphasizing their advantages and limitations in real-world conditions. In this way, it addresses an existing gap in the literature by offering a more practice-oriented perspective that links theoretical concepts with methodological challenges and the reliability of collected data.

Recent global-scale reviews show that beyond Europe, particularly in Asia, North America LCZ studies are increasingly using advanced data sources and automated mapping. Wang et al. [87] reported over 400 LCZ‑related publications covering approximately 250 cities globally, with a strong emphasis on integration of WUDAPT‑based remote sensing, machine learning classifiers, and large‑scale modeling frameworks. Nonetheless, Huang et al. [88] highlighted that deep learning and high‑resolution satellite data (e.g., Sentinel‑1/2, GF‑6) are becoming standard in LCZ mapping studies outside Europe. These developments demonstrate a growing global effort to improve the consistency and comparability of LCZ mapping practices across different regions. In this context, Middel et al. [89] proposed the concept of microclimate zones as a refinement of the LCZ framework, aiming to better capture urban thermal variability at finer spatial scales.

Based on the articles chosen for this review, it has been noticed that the LCZ scheme is not only used to investigate urban temperatures and the UHI effect, but it is also applicable to various types of studies, such as energy balance and water budget models [74], urban heat exposure [24], thermal physiology, and human well-being [82], among others. Moreover, it can be seen that the framework has begun to be useful in various aspects of urban climate, and it has not yet moved much further from that. However, with new types of models, machine learning, and different modelling techniques, it is starting to expand. These articles show different methods for observing urban climate from different aspects, whether it is UHI, OTC, bioclimatic indexes, etc. The combination of different methods and models can improve the accuracy of collected data and propose new suggestions on how urban climate can be improved, as well as science overall. Furthermore, efforts should be made to make LCZ classification more precise and take full advantage of new data sources. This way, we can better capture local climate differences in cities and create solutions that fit each unique urban context.

5 Conclusion

This review gathered 61 articles on measuring temperature variations and characteristics of specific LCZs in various European cities, using both in situ and mobile stations. The LCZ scheme proved to be a good indicator of the zones themselves and the characteristics that define each local area. As LCZ classification has become more popular in recent years, its applications keep expanding, especially in studies of UHI, OTC, and different urban climate indexes. According to the findings in the reviewed literature, the UHI effect is strongest in built-up LCZs, with temperature differences of a few degrees compared to land cover zones in cities. However, these differences are not always consistent across all cities, highlighting the need for further research that considers local context and additional influencing factors. The WUDAPT method is a promising tool for urban climate studies, as it prioritizes data sharing and ease of use in LCZ mapping. However, its accuracy still needs improvement. A major focus in LCZ research should be on developing more precise and scalable mapping techniques by combining different high-quality datasets and advanced classification methods.

Given the advanced pace of urbanization and climate change, future research should continue to explore the combination of different measurement methods, and promote the application of LCZ in various studies (such as thermal variations). Mobile measurements are shown to be promising types of data gathering, especially during hot summer days, while measurements conducted by cars, bicycles, and handheld instruments can improve data gathering in the LCZs where in situ instruments are not placed. Moreover, in situ stations are also important for data gathering, as they are located in specific locations (different urban settings), where different parameters are monitored on a daily, seasonal, or annual basis, and provide long-term data while keeping track of changes. Furthermore, in recent studies it can be noticed that the growing usage of other measurement methods, such as citizen weather stations [30,39,67,68,69], remote sensing [48,49,71,72], and numerical modeling [25,50,56,61], either alone or in combination with in situ and mobile instruments. These data collection methods have become some of the most important, especially in certain areas where better spatial coverage and temporal resolution are required, as well as in places where it is challenging to install in situ instruments or perform measurements using mobile instruments. For instance, remote sensing data can support the assessment of surface temperature and land cover, while crowdsourced weather stations provide real-time, high-resolution observations in dense urban settings. The integration of multiple data sources, such as in situ stations, crowdsourced instruments, and satellite observations, can significantly improve the representation of urban microclimates and the interpretation of thermal patterns in different LCZ. Therefore, combining these complementary methods represents a necessary approach for understanding the complex interactions between urban form, land cover, and atmospheric conditions [9].

Ultimately, the application of the LCZ framework, supported by robust thermal data, provides essential tools for urban planners, architects, and policymakers. It offers a strategic pathway for designing healthier, more sustainable, and climate-resilient cities, ensuring improved OTC and quality of life for urban residents. Additionally, these kind of local- and micro-scales climate monitoring and LCZ assessments are in line with the Agenda 2030 [90] – a United Nations initiative adopted in 2015 that outlines 17 sustainable development goals (SDGs) aimed to achieve peace, prosperity, and healthy planet for all by the year 2030. Specifically, the various LCZ analysis could contribute to reach some of the SDGs like: SDG 3 – an increased awareness of the necessity of improving public health and well-being of dwellers through the monitoring and analysis of climate conditions in different urban designs; SDG 11 – contributing to a better implementation of climate-conscious urbanization that can improve the quality of life, local and microclimate conditions, and contribute to the development of sustainable cities; and SDG 13 – work on further climate measures toward the adaptation to climate change, especially in urban areas where the local and microclimate are additionally modified due to the impact of urbanization [91].

Acknowledgments

The research was supported by the project no. 003026234 2024 09418 003 000 000 001, funded by the Autonomous Province of Vojvodina (regional government).

  1. Funding information: The research was supported by project no. 003026234 2024 09418 003 000 000 001, funded by the Autonomous Province of Vojvodina (regional government). The funder had no role in the study design, data collection, analysis, interpretation of data, writing of the manuscript, or decision to submit for publication.

  2. Author contributions: All authors have accepted responsibility for the entire content of this manuscript and consented to its submission to the journal, reviewed all the results, and approved the final version of the manuscript. M.V. was responsible for the overall conceptualization, methodology, data analysis, interpretation of results, and writing of the manuscript. D.J. contributed to the methodology and provided feedback during manuscript preparation. S.S. assisted with the discussion and offered guidance throughout the research process. D.O. supported the work by producing graphs and spatial analyses using GIS tools. The authors applied the SDC approach for the sequence of authors.

  3. Conflict of interest: The authors state no conflict of interest.

  4. Data availability statement: Not applicable.

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Received: 2025-05-20
Revised: 2025-08-01
Accepted: 2025-08-06
Published Online: 2025-09-09

© 2025 the author(s), published by De Gruyter

This work is licensed under the Creative Commons Attribution 4.0 International License.

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  46. Trace elements and melt inclusion in zircon within the Qunji porphyry Cu deposit: Application to the metallogenic potential of the reduced magma-hydrothermal system
  47. Pore, fracture characteristics and diagenetic evolution of medium-maturity marine shales from the Silurian Longmaxi Formation, NE Sichuan Basin, China
  48. Study of the earthquakes source parameters, site response, and path attenuation using P and S-waves spectral inversion, Aswan region, south Egypt
  49. Source of contamination and assessment of potential health risks of potentially toxic metal(loid)s in agricultural soil from Al Lith, Saudi Arabia
  50. Regional spatiotemporal evolution and influencing factors of rural construction areas in the Nanxi River Basin via GIS
  51. An efficient network for object detection in scale-imbalanced remote sensing images
  52. Effect of microscopic pore–throat structure heterogeneity on waterflooding seepage characteristics of tight sandstone reservoirs
  53. Environmental health risk assessment of Zn, Cd, Pb, Fe, and Co in coastal sediments of the southeastern Gulf of Aqaba
  54. A modified Hoek–Brown model considering softening effects and its applications
  55. Evaluation of engineering properties of soil for sustainable urban development
  56. The spatio-temporal characteristics and influencing factors of sustainable development in China’s provincial areas
  57. Application of a mixed additive and multiplicative random error model to generate DTM products from LiDAR data
  58. Gold vein mineralogy and oxygen isotopes of Wadi Abu Khusheiba, Jordan
  59. Prediction of surface deformation time series in closed mines based on LSTM and optimization algorithms
  60. 2D–3D Geological features collaborative identification of surrounding rock structural planes in hydraulic adit based on OC-AINet
  61. Spatiotemporal patterns and drivers of Chl-a in Chinese lakes between 1986 and 2023
  62. Land use classification through fusion of remote sensing images and multi-source data
  63. Nexus between renewable energy, technological innovation, and carbon dioxide emissions in Saudi Arabia
  64. Analysis of the spillover effects of green organic transformation on sustainable development in ethnic regions’ agriculture and animal husbandry
  65. Factors impacting spatial distribution of black and odorous water bodies in Hebei
  66. Large-scale shaking table tests on the liquefaction and deformation responses of an ultra-deep overburden
  67. Impacts of climate change and sea-level rise on the coastal geological environment of Quang Nam province, Vietnam
  68. Reservoir characterization and exploration potential of shale reservoir near denudation area: A case study of Ordovician–Silurian marine shale, China
  69. Seismic prediction of Permian volcanic rock reservoirs in Southwest Sichuan Basin
  70. Application of CBERS-04 IRS data to land surface temperature inversion: A case study based on Minqin arid area
  71. Geological characteristics and prospecting direction of Sanjiaoding gold mine in Saishiteng area
  72. Research on the deformation prediction model of surrounding rock based on SSA-VMD-GRU
  73. Geochronology, geochemical characteristics, and tectonic significance of the granites, Menghewula, Southern Great Xing’an range
  74. Hazard classification of active faults in Yunnan base on probabilistic seismic hazard assessment
  75. Characteristics analysis of hydrate reservoirs with different geological structures developed by vertical well depressurization
  76. Estimating the travel distance of channelized rock avalanches using genetic programming method
  77. Landscape preferences of hikers in Three Parallel Rivers Region and its adjacent regions by content analysis of user-generated photography
  78. New age constraints of the LGM onset in the Bohemian Forest – Central Europe
  79. Characteristics of geological evolution based on the multifractal singularity theory: A case study of Heyu granite and Mesozoic tectonics
  80. Soil water content and longitudinal microbiota distribution in disturbed areas of tower foundations of power transmission and transformation projects
  81. Oil accumulation process of the Kongdian reservoir in the deep subsag zone of the Cangdong Sag, Bohai Bay Basin, China
  82. Investigation of velocity profile in rock–ice avalanche by particle image velocimetry measurement
  83. Optimizing 3D seismic survey geometries using ray tracing and illumination modeling: A case study from Penobscot field
  84. Sedimentology of the Phra That and Pha Daeng Formations: A preliminary evaluation of geological CO2 storage potential in the Lampang Basin, Thailand
  85. Improved classification algorithm for hyperspectral remote sensing images based on the hybrid spectral network model
  86. Map analysis of soil erodibility rates and gully erosion sites in Anambra State, South Eastern Nigeria
  87. Identification and driving mechanism of land use conflict in China’s South-North transition zone: A case study of Huaihe River Basin
  88. Evaluation of the impact of land-use change on earthquake risk distribution in different periods: An empirical analysis from Sichuan Province
  89. A test site case study on the long-term behavior of geotextile tubes
  90. An experimental investigation into carbon dioxide flooding and rock dissolution in low-permeability reservoirs of the South China Sea
  91. Detection and semi-quantitative analysis of naphthenic acids in coal and gangue from mining areas in China
  92. Comparative effects of olivine and sand on KOH-treated clayey soil
  93. YOLO-MC: An algorithm for early forest fire recognition based on drone image
  94. Earthquake building damage classification based on full suite of Sentinel-1 features
  95. Potential landslide detection and influencing factors analysis in the upper Yellow River based on SBAS-InSAR technology
  96. Assessing green area changes in Najran City, Saudi Arabia (2013–2022) using hybrid deep learning techniques
  97. An advanced approach integrating methods to estimate hydraulic conductivity of different soil types supported by a machine learning model
  98. Hybrid methods for land use and land cover classification using remote sensing and combined spectral feature extraction: A case study of Najran City, KSA
  99. Streamlining digital elevation model construction from historical aerial photographs: The impact of reference elevation data on spatial accuracy
  100. Analysis of urban expansion patterns in the Yangtze River Delta based on the fusion impervious surfaces dataset
  101. A metaverse-based visual analysis approach for 3D reservoir models
  102. Late Quaternary record of 100 ka depositional cycles on the Larache shelf (NW Morocco)
  103. Integrated well-seismic analysis of sedimentary facies distribution: A case study from the Mesoproterozoic, Ordos Basin, China
  104. Study on the spatial equilibrium of cultural and tourism resources in Macao, China
  105. Urban road surface condition detecting and integrating based on the mobile sensing framework with multi-modal sensors
  106. Application of improved sine cosine algorithm with chaotic mapping and novel updating methods for joint inversion of resistivity and surface wave data
  107. The synergistic use of AHP and GIS to assess factors driving forest fire potential in a peat swamp forest in Thailand
  108. Dynamic response analysis and comprehensive evaluation of cement-improved aeolian sand roadbed
  109. Rock control on evolution of Khorat Cuesta, Khorat UNESCO Geopark, Northeastern Thailand
  110. Gradient response mechanism of carbon storage: Spatiotemporal analysis of economic-ecological dimensions based on hybrid machine learning
  111. Comparison of several seismic active earth pressure calculation methods for retaining structures
  112. Mantle dynamics and petrogenesis of Gomer basalts in the Northwestern Ethiopia: A geochemical perspective
  113. Study on ground deformation monitoring in Xiong’an New Area from 2021 to 2023 based on DS-InSAR
  114. Paleoenvironmental characteristics of continental shale and its significance to organic matter enrichment: Taking the fifth member of Xujiahe Formation in Tianfu area of Sichuan Basin as an example
  115. Equipping the integral approach with generalized least squares to reconstruct relict channel profile and its usage in the Shanxi Rift, northern China
  116. InSAR-driven landslide hazard assessment along highways in hilly regions: A case-based validation approach
  117. Attribution analysis of multi-temporal scale surface streamflow changes in the Ganjiang River based on a multi-temporal Budyko framework
  118. Maps analysis of Najran City, Saudi Arabia to enhance agricultural development using hybrid system of ANN and multi-CNN models
  119. Hybrid deep learning with a random forest system for sustainable agricultural land cover classification using DEM in Najran, Saudi Arabia
  120. Long-term evolution patterns of groundwater depth and lagged response to precipitation in a complex aquifer system: Insights from Huaibei Region, China
  121. Remote sensing and machine learning for lithology and mineral detection in NW, Pakistan
  122. Spatial–temporal variations of NO2 pollution in Shandong Province based on Sentinel-5P satellite data and influencing factors
  123. Numerical modeling of geothermal energy piles with sensitivity and parameter variation analysis of a case study
  124. Stability analysis of valley-type upstream tailings dams using a 3D model
  125. Variation characteristics and attribution analysis of actual evaporation at monthly time scale from 1982 to 2019 in Jialing River Basin, China
  126. Investigating machine learning and statistical approaches for landslide susceptibility mapping in Minfeng County, Xinjiang
  127. Investigating spatiotemporal patterns for comprehensive accessibility of service facilities by location-based service data in Nanjing (2016–2022)
  128. A pre-treatment method for particle size analysis of fine-grained sedimentary rocks, Bohai Bay Basin, China
  129. Study on the formation mechanism of the hard-shell layer of liquefied silty soil
  130. Comprehensive analysis of agricultural CEE: Efficiency assessment, mechanism identification, and policy response – A case study of Anhui Province
  131. Simulation study on the damage and failure mechanism of the surrounding rock in sanded dolomite tunnels
  132. Towards carbon neutrality: Spatiotemporal evolution and key influences on agricultural ecological efficiency in Northwest China
  133. High-frequency cycles drive the cyclical enrichment of oil in porous carbonate reservoirs: A case study of the Khasib Formation in E Oilfield, Mesopotamian Basin, Iraq
  134. Reconstruction of digital core models of granular rocks using mathematical morphology
  135. Spatial–temporal differentiation law of habitat quality and its driving mechanism in the typical plateau areas of the Loess Plateau in the recent 30 years
  136. Review Articles
  137. Humic substances influence on the distribution of dissolved iron in seawater: A review of electrochemical methods and other techniques
  138. Applications of physics-informed neural networks in geosciences: From basic seismology to comprehensive environmental studies
  139. Ore-controlling structures of granite-related uranium deposits in South China: A review
  140. Shallow geological structure features in Balikpapan Bay East Kalimantan Province – Indonesia
  141. A review on the tectonic affinity of microcontinents and evolution of the Proto-Tethys Ocean in Northeastern Tibet
  142. Advancements in machine learning applications for mineral prospecting and geophysical inversion: A review
  143. Special Issue: Natural Resources and Environmental Risks: Towards a Sustainable Future - Part II
  144. Depopulation in the Visok micro-region: Toward demographic and economic revitalization
  145. Special Issue: Geospatial and Environmental Dynamics - Part II
  146. Advancing urban sustainability: Applying GIS technologies to assess SDG indicators – a case study of Podgorica (Montenegro)
  147. Spatiotemporal and trend analysis of common cancers in men in Central Serbia (1999–2021)
  148. Minerals for the green agenda, implications, stalemates, and alternatives
  149. Spatiotemporal water quality analysis of Vrana Lake, Croatia
  150. Functional transformation of settlements in coal exploitation zones: A case study of the municipality of Stanari in Republic of Srpska (Bosnia and Herzegovina)
  151. Hypertension in AP Vojvodina (Northern Serbia): A spatio-temporal analysis of patients at the Institute for Cardiovascular Diseases of Vojvodina
  152. Regional patterns in cause-specific mortality in Montenegro, 1991–2019
  153. Spatio-temporal analysis of flood events using GIS and remote sensing-based approach in the Ukrina River Basin, Bosnia and Herzegovina
  154. Flash flood susceptibility mapping using LiDAR-Derived DEM and machine learning algorithms: Ljuboviđa case study, Serbia
  155. Geocultural heritage as a basis for geotourism development: Banjska Monastery, Zvečan (Serbia)
  156. Assessment of groundwater potential zones using GIS and AHP techniques – A case study of the zone of influence of Kolubara Mining Basin
  157. Impact of the agri-geographical transformation of rural settlements on the geospatial dynamics of soil erosion intensity in municipalities of Central Serbia
  158. Where faith meets geomorphology: The cultural and religious significance of geodiversity explored through geospatial technologies
  159. Applications of local climate zone classification in European cities: A review of in situ and mobile monitoring methods in urban climate studies
  160. Complex multivariate water quality impact assessment on Krivaja River
  161. Ionization hotspots near waterfalls in Eastern Serbia’s Stara Planina Mountain
  162. Shift in landscape use strategies during the transition from the Bronze age to Iron age in Northwest Serbia
  163. Assessing the geotourism potential of glacial lakes in Plav, Montenegro: A multi-criteria assessment by using the M-GAM model
  164. Flash flood potential index at national scale: Susceptibility assessment within catchments
  165. SWAT modelling and MCDM for spatial valuation in small hydropower planning
  166. Disaster risk perception and local resilience near the “Duboko” landfill: Challenges of governance, management, trust, and environmental communication in Serbia
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