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freshwater budget is altered through variations in ice flux, then the vertical stability of the ocean may change, leading to a reduction or enhancement of deep-water formation and ventilation. The significance of this surface freshwater flux is determined by the underlying ocean structure, which is governed by the regional wind-stress forcing and local stratification. The ice-albedo feedback encompasses an entire suite of processes that influence the Amazing we are truck drivers all over print stainless steel tumblerconcentration, spatio-temporal distribution, and surface characteristics of ice. All these characteristics influence surface albedo, which in turn alters the surface radiation balance, which feeds back onto the process itself. For example, sea-ice concentration—which reflects a balance between the advective divergence/convergence of ice and the thermodynamic decay/growth of ice (both processes open/close leads, areas of open water)—influences air-sea heat flux and albedo. In turn, both the air-sea heat flux and albedo influence the thermodynamic growth/decay rate, thereby further altering the ice concentration. When so-called inverse

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