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Numerical modelling of physical characteristics in the neighbourhood of an isolated hydrological section in the Barents Sea
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A. S. SARKISYAN
Veröffentlicht/Copyright:
22. Oktober 2009
Published Online: 2009-10-22
Published in Print: 1998
Walter de Gruyter
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- ON THE OCCASION OF VALENTIN P. DYMNIKOV 60th ANNIVERSARY
- Mesoscale modelling of wet convection and gas-aerosol interaction
- Stability of attractors in semidynamic systems
- Numerical model of the general circulation of the Arctic Ocean. A new version and preliminary calculation results
- Simulation of CO2 exchange processes in the atmosphere-surface biomes system by the climatic model ECSib
- Non-local turbulence closure for convective boundary layers
- On the statement and solution of inverse problems in satellite meteorology
- Circulation of the World ocean: the effect of physical factors on the formation and the long-term variability of hydrophysical fields
- Numerical modelling of physical characteristics in the neighbourhood of an isolated hydrological section in the Barents Sea
- Atmospheric circulation and weather prediction models using a semi-Lagrangian approach and high-order compact finite differences
Artikel in diesem Heft
- ON THE OCCASION OF VALENTIN P. DYMNIKOV 60th ANNIVERSARY
- Mesoscale modelling of wet convection and gas-aerosol interaction
- Stability of attractors in semidynamic systems
- Numerical model of the general circulation of the Arctic Ocean. A new version and preliminary calculation results
- Simulation of CO2 exchange processes in the atmosphere-surface biomes system by the climatic model ECSib
- Non-local turbulence closure for convective boundary layers
- On the statement and solution of inverse problems in satellite meteorology
- Circulation of the World ocean: the effect of physical factors on the formation and the long-term variability of hydrophysical fields
- Numerical modelling of physical characteristics in the neighbourhood of an isolated hydrological section in the Barents Sea
- Atmospheric circulation and weather prediction models using a semi-Lagrangian approach and high-order compact finite differences