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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