According to Khromov (1957): ITCZ is bad weather strip, formed by the convergence of Xinfeng 2 hemispheres, of Xinfeng 1 hemisphere with the other hemisphere Xinfeng crossed the Equator and redirect and Xinfeng each hemisphere with temperate Maple Equatorial wind Credits extended. There are 3 models Strip comprising the tropical convergence:Type 1: near the equator. Occur in the Atlantic Ocean when a Xinfeng 2 hemispheres meet near the equator. Types of convergent band wind has a high frequency, just above the global average wind maps in the equatorial Atlantic domain. in this tropical convergence, strip strip of Cumulus clouds and cumulonimbus form irregular density range. The width of the strip of cloud approximately 200-300 m, great length, have the case almost surrounded the Earth.
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