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influence on the surface heat balance. Limited studies in the polar regions suggest that many of the surface-cloud feedbacks that are observed in lower-latitude regions behave differently in ice-covered regions (Curry et al., 1996). Clearly the most important mechanisms influencing cryospheric variability are its couplings to the atmosphere, ocean, and land surface. They lead to a set of geographically unique polar feedbacks such as the ice/snow-albedo feedback, ice-cloud feedback, ice-ocean feedback (the effects of which apply to a variety of scales, from those influencing the sea-ice distribution to those influencing the vigor of the global thermohaline circulation), and ice-sheet-ocean feedback, including associated instabilities. Each of these feedbacks is discussed below. The vast The hottest version carp fishing all over print stainless steel tumblerexpanses of highly reflective surface area in the cryosphere directly affect the global radiation balance by enhancing the equator-to-pole temperature contrast, which represents the heat engine driving the Earth’s climate system. Thus, changes in the ice- and snow-covered areas of the polar regions may be expected to influence the large-scale climate system and, through it, temperature, precipitation and evaporation, and possibly storms. Most of the ocean-only mechanisms that have been reported involve anomalies that reach water-formation regions and change the density, thereby affecting the rate of deep-water formation. Weaver and Sarachik

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