Notes : * - The trade mites, the first major wind zone, f down(p)s at 30 degrees North & group A; South line of latitude, where line of merchandise sinks, warms, and returns to the equator in a westerly direction. * - Around 30 degrees latitude, known as the dollar latitudes, the sinking circulate associated with the trade winds creates a smash of towering hug that in turn causes generally promiscuous advance winds. - When air converges it is forced upward and creates an area of low pressure in a process called lay to restsection point. - progress the equator, convergence occurs oer a large area called the inter tropical convergence zone (ITCZ), also called the doldrums. - The ITCZ migrates South & deoxyadenosine monophosphate; North of the equator as the seasons change. * - The ITCZ is characterized by a band of cloud cover and occasional showers. * - The reign westerlies, the second major wind zone, flows amidst 30 degrees and 60 degrees Nor th & South latitude in a circulation pattern opposite that of the trade winds. * - The predominant westerlies are trusty for much of the movement of weather crosswise the USA & Canada. * - The gelid easterlies, the third major wind zone, lies between 60 degrees latitude and the poles. * - In both hemispheres, the polar easterlies are characterized by cold air. * - In the middle latitudes, air masses with unlike characteristics sometimes collide, forming a summit. * - A front is the narrow arena separating two air masses of incompatible densities that are caused by differences in temperature, pressure, and humidity. * - The interaction between the colliding air masses jackpot bring dramatic changes in weather. * - in that respect are cardinal main types of fronts; cold fronts, warm fronts, unmoving fronts, and occluded fronts. * - *If you involve to get a full essay, enounce it on our website: BestEssayCheap.com
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