Snow Cover Influence on Sea Ice in the Taganrog Bay

被引：0
作者：
D. D. Zav’yalov
T. A. Solomakha
机构：
[1] Russian Academy of Sciences,Marine Hydrophysical Institute
来源：
Russian Meteorology and Hydrology | 2019年 / 44卷
关键词：
Sea ice models; thermodynamics; ice thickness; snow parameterization; Sea of Azov;
D O I：
暂无
中图分类号：
学科分类号：
摘要：
The seasonal evolution of sea ice thickness in the eastern part of the Taganrog Bay is studied using the one-dimensional thermodynamic sea ice model. The numerical experiments are conducted to simulate the thermal evolution of sea ice thickness using various snow parameterization schemes. The results of modeling for the winters of 2007/2008 and 2008/2009 are compared with in situ observations. The quality of the forecast of seasonal variations in sea ice thickness is assessed.
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页码：45 / 52
页数：7
相关论文
共 13 条
[1]  
Bogorodskii P. V.(2011)Influence of Melt Ponds on the Formation of the Multiyear Sea Ice Cover Okeanologiya 2 51-undefined
[2]  
Pnyushkov A. V.(2015)Numerical Model of Ice Cover Evolution in Arctic Seas for Operational Forecasting Led i Sneg 3 55-undefined
[3]  
Klyachkin S. V.(2010)Freezing of the Sea of Azov and Climate at the Beginning of the 21st Century Vestnik YuNTs RAN 1 6-undefined
[4]  
Guzenko R. B.(2009)Reproduction of the Large–scale State of Water and Sea Ice in the Arctic Ocean in 1948–2002. Part I. Numerical Model Izv. Akad. Nauk, Fiz. Atmos. Okeana 3 45-undefined
[5]  
Mai R. I.(2006)Modified Snow Algorithms in the Canadian Land Surface Scheme: Model Runs and Sensitivity Analysis at Three Boreal Forest Stands Can. Meteorol. Oceanogr. Soc., Atmosphere–Ocean 3 43-undefined
[6]  
Matishov G. G.(undefined)undefined undefined undefined undefined-undefined
[7]  
Matishov D. G.(undefined)undefined undefined undefined undefined-undefined
[8]  
Gargopa Yu. M.(undefined)undefined undefined undefined undefined-undefined
[9]  
Dashkevich L. V.(undefined)undefined undefined undefined undefined-undefined
[10]  
Yakovlev N. G.(undefined)undefined undefined undefined undefined-undefined
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