赤道辐合带

如陆面的CWP高值中心主要位于非洲中部、东南亚地区以及南美洲的热带雨林区；而洋面CWP则集中在赤道辐合带、南太平洋辐合带以及南北半球中纬度地区。

CWP on the lands are mainly located over rain forest in Central Africa , Southeast Asia , and South America ; on the oceans , CWP are concentrated in ITCZ , SPCZ and the mid-latitudes in the northern and southern hemispheres .

全球副热带高压和赤道辐合带演变规律的分析和应用

Analysis on the varying laws of the global subtropical high and the equatorial ITCZ and its application

在1982／1983ENSO过程中暖池和赤道辐合带相互作用对大气表面风的影响

Influence of interaction between the shift of warm pool and that of equatorial convergence zones on atmospheric surface winds fields during 1982 / 1983 ENSO

赤道辐合带上热带气旋发生机制的一个数值试验

A numerical experiment about the mechanism of the initiation of tropical cyclone along the intertropical convergence zone

台风与西风槽相互作用与赤道辐合带的北跳

The Relations Between the Intertropical Convergence Zone ( ITCZ ) Skipping Northward and the Interaction Between Typhoon and Westerly Trough ( TT ) Pattern

春季和秋季赤道辐合带为主要的水汽汇，亚澳季风区无明显越赤道水汽输送。

In spring and autumn , ITCZ is the main moisture sink , there is no apparent water vapor transport between Asian monsoon region and Australian monsoon region .

通过对气候平均场的研究发现，在同一个季节，赤道辐合带在不同经度上位置有很大差别；在不同季节，赤道辐合带在不同经度上的位移也不一样。

The results show that : ( 1 ) Average climatic maps show that equatorial belt of converage is quite different along to the longitude at the same season in location , and its displacement is also different along to season .

这两年夏季亚洲西风带阻塞高压活动都十分频繁，1998年更甚。夏季赤道辐合带1998年明显弱于1954年。

At the same time , ITCZ of summer was notably weaker in 1998 than in 1954.But the action of blocking high of the westerly belt in Asia was very frequently in summer of the both years , especially in 1998 .

观测表明，高云的夏季块状分布和冬季带状分布，与低层赤道辐合带的夏季与冬季的形状十分相似；并且卷云和卷层云可以独立于深对流单独存在。

According to the observations in Part I , block pattern in summer and zonal belt pattern in winter concerning with tropical high clouds is like the corresponding patterns of Intertropical convergence zone ( hereafter , ITCZ ), and Cirrostratus and Cirrus can form locally without deep convective cloud .