海陆热力差异

PDO和伴随的亚非大陆和印度洋地区之间海陆热力差异的年代际变化对印度洋海温和东亚季风降水年际联系具有明显的调节作用。

The interannual relationship between Indian Ocean SST and East Asia monsoon rainfall is regulated by the PDO associated with interdecadal variations of land-sea thermodynamic defference between Asia-Africa continent and Indian Ocean .

中纬度海陆热力差异与东亚夏季降水关系密切。

The LSI has close connection to the East Asian summer precipitation .

海陆热力差异对威海冬季暴雪的贡献

Contribution of Thermal Contrast between Land and Sea to Snowstorm of Winter in Weihai

东亚冬季风异常的空间结构及与海陆热力差异的联系

Spatial Structure of East Asian Winter Monsoon and Its Relationship with Sea-Land Thermal Contrast

渤海湾海陆热力差异对局地天气系统的影响

The Effect of Thermal Contrast between Land and Sea over Bohai Bay on Local Synoptic System

本文认为亚洲南部的季风，主要是由行星风带的季节移动而引起的，但也有海陆热力差异的影响的观点是不合理的。

It is unrational that the Southern Asia Monsoon is mainly caused by seasonal movement of planetary Wind system .

行星风带的季节移动对南亚地区的影响强度受到海陆热力差异的制约，其固有的季节移动作用，对南亚季风形成只起加强的作用。

The seasonal movement of planetary wind system only enhances the formation of the Southern Asia Monsoon , and its effective strenth is conditioned by thermal difference between sea and Land .

热带海洋温度具有显著的年际异常，热带海温的变异不仅可以通过改变海陆热力差异，而且也通过热带地区强烈的海气相互作用，对季风系统产生重要影响，造成季风区天气和气候的异常。

The prominent interannual variability of sea temperature in tropical oceans can affect the monsoon both through altering the thermal contrast between land and sea and through strong air-sea interaction in the tropics .

着眼于东亚海陆热力强迫差异的影响，探讨了东亚初夏环流与江淮梅雨成因。

In this paper , with a view to the effect of sea-land thermal forcing contrast in East Asian , the early summer circulation in East Asia and Meiyu cause of formation in Jianghuai valley are studied .

数值试验表明，东亚海陆热力强迫的差异与夏季风、梅雨阻塞系统的形成密切相关。

The numerical experiments indicate that sea-land thermal forcing contrast in East Asia is closely related to summer monsoon and the formation of Meiyu blocking system .

亚洲南部的季风（下称南亚季风）和亚洲东部的季风（下称东亚季风）一样，都属于海陆季风，主要是由海陆之间的热力差异引起的。

Like the East Asia Monsoon , the Southern Asia Monsoon is also also caused by Thermal difference between sea and land .