付超, 李维亮. 1996: 大尺度瞬变涡旋经向热量和水沟通量在纬向平均气流形成中的效应. 气象学报, (3): 373-378. DOI: 10.11676/qxxb1996.038
引用本文: 付超, 李维亮. 1996: 大尺度瞬变涡旋经向热量和水沟通量在纬向平均气流形成中的效应. 气象学报, (3): 373-378. DOI: 10.11676/qxxb1996.038
Fu Chao, Li Weiliang. 1996: PARAMETERIZATIONS OF LARGE-SCALE EDDY HEAT AND MOISTURE IN A ZONALLY AVERAGED DYNAMIC MODEL. Acta Meteorologica Sinica, (3): 373-378. DOI: 10.11676/qxxb1996.038
Citation: Fu Chao, Li Weiliang. 1996: PARAMETERIZATIONS OF LARGE-SCALE EDDY HEAT AND MOISTURE IN A ZONALLY AVERAGED DYNAMIC MODEL. Acta Meteorologica Sinica, (3): 373-378. DOI: 10.11676/qxxb1996.038

大尺度瞬变涡旋经向热量和水沟通量在纬向平均气流形成中的效应

PARAMETERIZATIONS OF LARGE-SCALE EDDY HEAT AND MOISTURE IN A ZONALLY AVERAGED DYNAMIC MODEL

  • 摘要: 在一个纬向平均模式中加入大尺度瞬变涡旋经向热量和水汽通量参数化方案。模拟出涡动通量的空间分布和时间变化。实验表明,涡动通量在中高、纬地区大气能量输送过程中起重要作用。应用上述参数化方案提高了模式的模拟能力。

     

    Abstract: In this paper,the transport of large-scale eddy heat and moisture are parameterized in a two-dimensional tonally averaged model. The parameterized eddy fluxes simulated the seasonal and latitudinal variations reasonably well. Compared with noninteractive test,some very effective strong feedbacks effect between the modeled tonal-mean climate and parameterized meridional eddy transport is identified.

     

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