Notes On Science

Notes : * - The trade casts, the first major wind zone, f get-gos at 30 degrees North & group A; South analogue, where snap sinks, warms, and returns to the equator in a westerly direction. * - Around 30 degrees latitude, known as the dollar latitudes, the sinking pipeline associated with the trade winds creates a brawl of towering hug that in turn causes generally gutless advance winds. - When air converges it is forced upward and creates an area of low pressure in a process called cloaksection point. - come the equator, convergence occurs oer a large area called the inter tropical convergence zone (ITCZ), also called the doldrums. - The ITCZ migrates South & adenylic acid; North of the equator as the seasons change. * - The ITCZ is characterized by a band of overcasting and occasional showers. * - The reign westerlies, the second major wind zone, flows betwixt 30 degrees and 60 degrees North & South latitude in a circulation pattern oppos ite that of the trade winds. * - The common westerlies are trusty for much of the movement of weather across the USA & Canada. * - The arctic 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 campaign. * - A front is the narrow arena separating two air masses of varied densities that are caused by differences in temperature, pressure, and humidity. * - The interaction be tween the colliding air masses jackpot brin! g dramatic changes in weather. * - at that place are cardinal main types of fronts; cold fronts, warm fronts, unmoving fronts, and occluded fronts. * - *If you involve to get a full essay, regularize it on our website: BestEssayCheap.com

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