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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<span>The main difference of
temperature in July for Canada and Alaska is of the temperature, January is
usually colder in Canada and Alaska varying from 10 degree Fahrenheit to 20
degree Fahrenheit while in July it gets warm or at times hot varying from 51
degree Fahrenheit to 69 degree Fahrenheit. </span>
The drainage area is not an important factor in determining stream discharge because it is not the main force behind stream discharge.
<h3>What is a
stream discharge?</h3>
This refers to the volume of water that flows through a stream or river per unit of time.
This discharge are usually calculated by using the measurements of the stream’s velocity, its depth and width
The factors that affect stream discharge includes:
- velocity of the water because the faster the water, the more the discharge
- the width & depth of the river
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Answer:
c
Explanation:
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