澳洲夏季风热源低频变化对北半球冬季风影响的数值研究
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国家自然科学基金


NUMERICAL STUDY OF EFFECT OF LOW-FREQUENCY CHANGE OF AUSTRALIAN SUMMER MONSOON HEAT SOURCE ON NORTHERN WINTER MONSOON
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    摘要:

    采用p-σ混合坐标系的5层原始方程模式研究了与澳洲辽季风低频变化相伴随的对流性低频加热源所激发的大气强迫波和东亚冬季风的关系。结果表明澳洲夏季风低频热源可引起北半球副热带高低层环流、东西向Walker环流、经向环流、越赤道气流的低频振荡,其振荡周期、强度与热源的振荡周期、强度有关。结果还进一步表明,澳洲低频热源可激发出扰动的北传,从而引起北半球副热带环流、副热带西风急流的低频振荡,澳洲夏季风活跃后的6天左右,东亚冬季风有一次增强过程,而澳洲夏季风的中断对冬季风则没有多大影响。

    Abstract:

    By using a five-layer primitive equation model in the p-σ incorperated coodinates,astudy is made of the relationship between the East Asian winter monsoon and the forcedwaves excited by the convective heat source associated with the low-frequency change ofAustralian summer monsoon. Experimental results indicate that the low frequency changecan cause the LFO of the Northern subtropical upper and low level circtilation,east-westWalker circulation,meridional circulation and cross-equatorial flow,Its oscillation period andintensity are related to those of the heat sotirce. Besides,the low frequency heat source canexcite the northward disttirbance,resulting in the LFO of the stibtropical cicrulation and sub-tropical west wind jet in the Northern Hemisphere. Six days or so after the onset of Australian summer monsoon East Asian winter monsoon can have a strengthening process。However,the lull of the Australian monsoon has no impact on the East Asian winter monsoon.

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徐海明,何金海,1994.澳洲夏季风热源低频变化对北半球冬季风影响的数值研究[J].大气科学学报,17(1):58-63. Xu Haiming, He Jinhai,1994. NUMERICAL STUDY OF EFFECT OF LOW-FREQUENCY CHANGE OF AUSTRALIAN SUMMER MONSOON HEAT SOURCE ON NORTHERN WINTER MONSOON[J]. Trans Atmos Sci,17(1):58-63.

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  • 收稿日期:1992-11-21
  • 最后修改日期:1993-03-01
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