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ZHANG Zhanhai,CHENG Bin,LAUNIAINEN Jouko,WU Huiding,LIU Yu. 2006. Inter-comparisons of thermodynamic sea-ice modeling results using various parameterizations of radiative flux. Acta Oceanologica Sinica, (1):21-31
Inter-comparisons of thermodynamic sea-ice modeling results using various parameterizations of radiative flux
Inter-comparisons of thermodynamic sea-ice modeling results using various parameterizations of radiative flux
Received:August 02, 2005  Revised:November 03, 2005
DOI:
Key words:parameterizations of radiative fluxes  energy balance at the surface of ice/snow  thermodynamic sea-ice model  Baltic Sea  Bohai Sea
中文关键词:  parameterizations of radiative fluxes  energy balance at the surface of ice/snow  thermodynamic sea-ice model  Baltic Sea  Bohai Sea
基金项目:
Author NameAffiliationE-mail
ZHANG Zhanhai State Oceanic Administration Key Laboratory for Polar Science, Polar Research Institute of China, Shanghai 200136, China zhangzhanhai@263.net.cn 
CHENG Bin Finnish Institute of Marine Research, Helsinki Fin-00931, Finland  
LAUNIAINEN Jouko Finnish Institute of Marine Research, Helsinki Fin-00931, Finland  
WU Huiding State Oceanic Administration Key Laboratory for Polar Science, Polar Research Institute of China, Shanghai 200136, China
National Marine Environment Forecast Center, Beijing 100081, China 
 
LIU Yu National Marine Environment Forecast Center, Beijing 100081, China  
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Abstract:
      Radiative fluxes are of primary importance in the energy and mass balance of the sea-ice cover.Various parameterizations of the radiative fluxes are studied in a thermodynamic sea-ice model.Model outputs of the surface radiative and heat fluxes and mass balance are compared with observations.The contribution of short-wave radiation is limited to a long part of winter.Therefore,simple schemes are often sufficient.Errors in estimations of the short-wave radiation are due mainly to cloud effects and occasionally to multi-reflection between surface and ice crystals in the air.The long-wave radiation plays an important role in the ice surface heat and mass balance during most part of a winter.The effect of clouds on the accuracy of the simple radiative schemes is critical,which needs further attention.In general,the accuracy of an ice model depends on that of the radiative fluxes.
中文摘要:
      Radiative fluxes are of primary importance in the energy and mass balance of the sea-ice cover.Various parameterizations of the radiative fluxes are studied in a thermodynamic sea-ice model.Model outputs of the surface radiative and heat fluxes and mass balance are compared with observations.The contribution of short-wave radiation is limited to a long part of winter.Therefore,simple schemes are often sufficient.Errors in estimations of the short-wave radiation are due mainly to cloud effects and occasionally to multi-reflection between surface and ice crystals in the air.The long-wave radiation plays an important role in the ice surface heat and mass balance during most part of a winter.The effect of clouds on the accuracy of the simple radiative schemes is critical,which needs further attention.In general,the accuracy of an ice model depends on that of the radiative fluxes.
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