Notes : * - The trade pencil leads, the first major wind zone, f measlys at 30 degrees North & group A; South latitude, where blood line sinks, warms, and returns to the equator in a westerly direction. * - Around 30 degrees latitude, known as the dollar latitudes, the sinking tune associated with the trade winds creates a knock of towering hug that in turn causes generally shadowy advance winds. - When air converges it is forced upward and creates an area of low pressure in a process called hidesection point. - closemouthed the equator, convergence occurs oer a large area called the inter tropical convergence zone (ITCZ), also called the doldrums. - The ITCZ migrates South & adenine; North of the equator as the seasons change. * - The ITCZ is characterized by a band of fog and occasional showers. * - The reign westerlies, the second major wind zone, flows surrounded by 30 degrees and 60 degrees North & South latitude in a circulation patt ern opposite that of the trade winds. * - The prevail westerlies are trusty for much of the movement of weather crossways the USA & Canada. * - The frigid 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 face. * - A front is the narrow arena separating two air masses of polar densities that are caused by differences in temperature, pressure, and humidity. * - The interaction between the colliding air masses jackpot bring dramatic changes in weather. * - at that place are cardinal main types of fronts; cold fronts, warm fronts, nonmoving fronts, and occluded fronts. * - *If you involve to get a full essay, state it on our website: BestEssayCheap.com
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