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海冰热力模式的辐射参数化方案在渤海和波罗的海应用的比较

张占海 程斌 LAUNIAINENJouko 吴辉碇 刘煜

张占海, 程斌, LAUNIAINENJouko, 吴辉碇, 刘煜. 海冰热力模式的辐射参数化方案在渤海和波罗的海应用的比较[J]. 海洋学报, 2006, 28(4): 17-25.
引用本文: 张占海, 程斌, LAUNIAINENJouko, 吴辉碇, 刘煜. 海冰热力模式的辐射参数化方案在渤海和波罗的海应用的比较[J]. 海洋学报, 2006, 28(4): 17-25.
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.
Citation: 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.

海冰热力模式的辐射参数化方案在渤海和波罗的海应用的比较

基金项目: 国家自然科学基金资助项目(40233032;40376006)

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

  • 摘要: 研究了海冰热力模式中的各种辐射参数化方案,对比了模式计算的太阳短波辐射、大气长波辐射以及海冰热力变化,并利用渤海和波罗的海观测资料进行比较和误差分析.冬季大部分时间太阳短波辐射对海冰热力过程的作用有限.简单计算方案一般满足海冰模式要求.误差主要受云和冰雪表面与大气之间的多重反射影响.长波辐射对表面热平衡和海冰质量变化起重要作用.长波辐射参数化方案的计算结果受环境因素影响.云量参数化有待进一步改进.海冰模式计算结果的精度与长波辐射计算精度有一致性.
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  • 收稿日期:  2005-07-25
  • 修回日期:  2006-05-21

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