Intercomparison of parameterizations of radiative fluxes used in thermodynamic sea ice modeling for the Bohai Sea and the Baltic Sea

ZHANG Zhan-hai; CHENG Bin; LAUNIAINEN Jouko; WU Hui-ding; LIU Yu

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ZHANG Zhan-hai, CHENG Bin, LAUNIAINEN Jouko, WU Hui-ding, LIU Yu. Intercomparison of parameterizations of radiative fluxes used in thermodynamic sea ice modeling for the Bohai Sea and the Baltic Sea[J]. Haiyang Xuebao, 2006, 28(4): 17-25.

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Intercomparison of parameterizations of radiative fluxes used in thermodynamic sea ice modeling for the Bohai Sea and the Baltic Sea

1.
State Ocean Administration Key Laboratory for Polar Science, Polar Research Institute of China, Shanghai 200136, China
2.
State Ocean Administration Key Laboratory for Polar Science, Polar Research Institute of China, Shanghai 200136, China;Finnish Institute of Marine Research, Fin-00931, Helsinki, Finland
3.
Finnish Institute of Marine Research, Fin-00931, Helsinki, Finland
4.
State Ocean Administration Key Laboratory for Polar Science, Polar Research Institute of China, Shanghai 200136, China;National Marine Environment Forecast Center, Beijing 100081, China
5.
National Marine Environment Forecast Center, Beijing 100081, China

Received Date: 2005-07-25
Rev Recd Date: 2006-05-21

Abstract

Abstract

The radiative fluxes are of primary importance in the energy and mass balance of the sea ice cover.The various parameterizations of radiative fluxes in the thermo dynamic sea ice model are studied in this paper.Model outputs of the surface radiative and heat fluxes and mass balance are compared with observations.The contribution of short wave radiation is limited in large part of the winter.Therefore, simple schemes are often sufficient.Errors in estimations of the short wave radiation are mainly due to cloud effects and occasionally due to multi reflection between surface and ice crystals in the air.The long wave radiation plays an important role in heat and mass balance of ice surface during large part of winter.The effect of clouds on the accuracy of simple radiative schemes is critical, which needs further attention.In general, accuracy of the ice model results is in consistent with the accuracy of estimation of the radiative fluxes.
- parameterizations of radiative fluxes,
- energy balance at the surface of ice/snow,
- thermody namic sea ice model,
- Baltic Sea,
- Bohai Sea

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References(43)

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