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regions, and are to some degree dependent on the ice distribution at their lower surface, they might be expected to show some degree of dependence on regional ice and snow distributions as well. This dependence has not been clearly documented, and is not well understood, but it has the potential to extend polar influences to climate attributes elsewhere through their influence on The hottest product we are truck drivers all over print stainless steel tumblerteleconnection patterns. The part of the Earth’s surface that remains perennially frozen, as well as the portion that is near or below the freezing point, constitutes the cryosphere. Our working definition of the cryosphere here is all the forms of frozen water on the land or sea surface, whether admixed or pure . Thus, this section addresses not only glaciers and sea ice , but also vast areas of frozen ground and permafrost, as well as seasonal snow fields that lie beyond the limits of glaciers. At present, glacial ice covers about 3 percent of the Earth’s surface, while containing nearly 75 percent of its non-ocean water; sea ice covers another 7 percent; and perennially frozen ground covers percent of the exposed land surface. The estimates of thermal expansion and ice melt over the last century generally add up to less than the

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