In July and August, the ITCZ lies well to <u>the</u><u> north of the equator </u><u>over Africa, Asia and Central America before going to south</u> into South America, central Africa and Australia by January and February.
<u>In January the </u><u>ITCZ</u><u> lies about at 15°S over</u><u> South America and Africa.</u><u> The</u><u> ITCZ</u><u> is less mobile over the oceans,</u> where it binds a stationary position just north of the equator.
<h3>What is the ITCZ ?</h3>
The Intertropical Convergence Zone, or ITCZ, is defined as a band of low pressure around the Earth which commonly lies near to the equator. The trade winds of the northern and southern hemispheres meet here, which takes them to the development of frequent thunderstorms and heavy rain.
<h3>What is the characteristics of ITCZ?</h3>
The ITCZ is characterized by low atmospheric pressures, as a result of the upward movement induced by the trade winds convergence. It forms a high atmospheric pressure in the upper troposphere.
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The volume of the rectangular prism is 72
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The Hawaiian islands were formed by hot spots that were occurring in the middle of the Pacific Plate. The combined process of magma formation, eruption, and the continuous movement of the Pacific Plate helped form the islands of Hawaii.
