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the planetary boundary layer are functions of wind friction at the Earth’s surface. Surface roughness is greatly influenced by both the stature and density of vegetation, in addition to the effects of topography. Models have treated the basal boundary condition of ice sheets as a function of underlying surface composition and temperature, as well as of the ocean-ice-sheet interaction along ice shelves. The observations needed to test these formulations are Amazing weed leaf mandala full printing low top shoeslacking, however. Correct model treatment of ice streams, which are small-scale features with high flow rates, will also require further study. These streams represent a major path through which ice sheets are drained, and their distribution may greatly alter estimates of average ice drainage and ice-sheet stability. Considerable uncertainties are associated with the prognostic treatment of polar clouds. Prognosis is further complicated by the possibility that polar clouds respond differently from clouds in other regions to changes in surface and forcing conditions. Better-polar cloud modeling is needed to more realistically depict the important ice-cloud feedback discussed above, and an extensive,

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