摘要
本文在用数值模拟方法模拟的非纬圈对称的夏季平均环流的基础上,在亚洲南部和澳大利亚地区引人热源扰动和冷源扰动,讨论这些冷热源扰动所引起的夏季风环流的改变以及流场扰动的结构和影响。
Based on a zonally non-uniform mean circulation in summer simulated by numerical modelling, perturbation heatings over South Asia and a perturbation cooling over Northwest Australia were incorporated in a numerical model to discuss their effects on summer monsoon over Asia and the structure of flow disturbance in this paper. It is shown that the perturbation heatings over the Southern Asia may make the upper easterlies to the south of the Tibetan High and the lower southwest flows strengthen, whereas the perturbation cooling over Australia can force a baroclinic disturbance and make the southeasterlies in the lower levels increase on its north side. However, so far as the scope of the anomalous heating/cooling introduced in the model and the time scale of model integration are concerned, the flow changes due to these perturbations may be mainly local and in the hemisphere where the perturbation heating/cooling is located. These changes are not strong enough to change the major features of the summer monsoon which is maintained by the global mean heating forcings and to explain the apparent strengthening of the cross-equatorial flows. The changes in divergence and vertical velocity fields are consistent with the distribution of the perturbation heating, indicating the direct contribution of anomalous heating to these changes. But the flow disturbances deviate from the perturbation heating, suggesting that the flow changes are related not only to the perturbation heating, but to the mean monsoonal circulation.
出处
《气象学报》
CSCD
北大核心
1990年第2期139-149,共11页
Acta Meteorologica Sinica
基金
国家自然科学基金
项目编号为 4870261
