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Options for developing modernized geodetic datum for Nepal following the April 25, 2015 Mw7.8 Gorkha earthquake

  • Chris Pearson EMAIL logo , Niraj Manandhar and Paul Denys ORCID logo
Published/Copyright: June 5, 2017
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Abstract

Along with the damage to buildings and infrastructure, the April 25, 2015 Mw7.8 Gorkha earthquake caused significant deformation over a large area of eastern Nepal with displacements of over 2 m recorded in the vicinity of Kathmandu.

Nepal currently uses a classical datum developed in 1984 by the Royal (UK) Engineers in collaboration with the Nepal Survey Department. It has served Nepal well; however, the recent earthquakes have provided an impetus for developing a semi-dynamic datum that will be based on ITRF2014 and have the capacity to correct for tectonic deformation.

In the scenario we present here, the datum would be based on ITRF2014 with a reference epoch set some time after the end of the current sequence of earthquakes. The deformation model contains a grid of the secular velocity field combined with models of the Gorkha Earthquake and the May 12 Mw7.3 aftershock. We have developed a preliminary velocity field by collating GPS derived crustal velocities from four previous studies for Nepal and adjacent parts of China and India and aligning them to the ITRF. Patches for the co-seismic part of the deformation for the Gorkha earthquake and the May 12, 2015 Mw 7.2 aftershock are based on published dislocation models.

High order control would be a CORS network based around the existing Nepal GPS Array. Coordinates for existing lower order control would be determined by readjusting existing survey measurements and these would be combined with a series of new control stations spread throughout Nepal.

Funding statement: Much of the work described in this paper was conducted during a 5 week visit to the Survey Department of Nepal by Chris Pearson, which was funded by the Ministry of Foreign Affairs and Trade, New Zealand on two HOMF grants in 2015 and 2016.

Acknowledgment

We acknowledge Diego Melgar for making the dislocation model of the Gorkha earthquake and its major aftershock available to us prior to publication. We also thank the University of Otago for waiving normal overheads for this project. This manuscript benefited from a review by Richard Stanaway.

References

[1] Manandhar N. Study of Geodetic datum of Nepal, China and Pakistan and its transformation to World Geodetic System. Nepalese Journal on Geoinformatics, 2011. 10, 30–35.10.3126/njg.v10i0.23190Search in Google Scholar

[2] Spence FS. Himalayan Survey. The Geographical Journal, 1987. 153(2), 223–230.10.2307/634874Search in Google Scholar

[3] Crook C, Donnelly N, Beavan J, Pearson C. From geophysics to geodetic datum: Updating the NZGD2000 deformation Model. New Zeal J Geol Geop, 2016. 59, 22–32. doi: 10.1080/00288306.2015.1100641.Search in Google Scholar

[4] Pearson C, Snay R. Introducing HTDP 3.1 to transform coordinates across time and spatial reference frames. GPS Solutions, 2013. 17(1), 1–15. doi: 10.1007/s10291-012-0255-y.Search in Google Scholar

[5] Stanaway R, Roberts C, Blick G, Crook C. Four Dimensional Deformation Modelling, the link between International, Regional and Local Reference Frames. Online Proceedings of the FIG Working Week 2012, Rome, Italy, 6–10 May 2012. www.fig.net/pub/fig2012/papers/ts02b/TS02B_stanaway_roberts_et_al_5906.pdf. Accessed 16 Dec 2015.Search in Google Scholar

[6] Bettinelli P, Avouac JP, Flouzat M, Jouanne F, Bollinger L, Willis P, Chitrakar G. Plate motion of India and Interseismic strain in the Nepal Himalaya from GPS and DORIS measurements. J Geod, 2006. 80, 567–589.10.1007/s00190-006-0030-3Search in Google Scholar

[7] Ader T, et al. Convergence rate across the Nepal Himalaya and interseismic coupling on the Main Himalayan Thrust: Implications for seismic hazard. J Geophys Res-Earth, 2012. 117, B04403. doi: 10.1029/2011JB009071.Search in Google Scholar

[8] Banerjee P, Burgmann R, Nagarajan B, Apel E. Intraplate deformation of the Indian subcontinent. Geophys Res Lett, 2008. 35, L18301. doi: 10.1029/2008GL035468.Search in Google Scholar

[9] Jade S, Mukul M, Gaur VK, Kumar K, Shrungeshwar TS, Satyal GS, Dumka RK, Jagannathan S, Ananda MB, Kumar PD, Banerjee S. Contemporary deformation in the Kashmir–Himachal, Garhwaland Kumaon Himalaya: significant insights from 1995–2008 GPS time series. J Geod, 2014. 88, 539–557.10.1007/s00190-014-0702-3Search in Google Scholar

[10] IERS ITRF solutions, ITRF2014. International Terrestrial Reference Frame (ITRF) web site. http://itrf.ign.fr/ITRF_solutions/2014/ITRF2014_files.php. Accessed 20 April 2016.Search in Google Scholar

[11] Snay RA, Freymueller JT, Craymer MR, Pearson C, Saleh J. Modelling 3D Crustal Velocities in the United States and Canada. J Geophys Res-Earth, 2015. doi: 10.1002/2016JB012884.Search in Google Scholar

[12] Galetzka J, et al. Slip pulse and resonance of Kathmandu basin during the 2015 Mw 7.8 Gorkha earthquake, Nepal imaged with geodesy. Science, 2015. 349, 1091–1095. doi: 10.1126/science.aac6383.Search in Google Scholar PubMed

[13] Pearson C, Freymueller J, Snay R. Software to help surveying engineers deal with the coordinate changes due to crustal motion in Alaska. In: Zufelt JE, ed. Proceedings of the 10th International Symposium on Cold Regions Development (ISCORD): Planning for Sustainable Cold Regions. Reston, VA, USA, American Society of Civil Engineers, 2013. doi: 10.1061/9780784412978.031.Search in Google Scholar

[14] Caltech Tectonics Observatory Nepal GPS Array station map (Accessed March 24, 2017 at http://www.tectonics.caltech.edu/resources/kmlnepal.html).Search in Google Scholar

Received: 2016-7-19
Accepted: 2017-4-7
Published Online: 2017-6-5
Published in Print: 2017-9-26

© 2017 Walter de Gruyter GmbH, Berlin/Boston

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