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be closed. Finally, both field and satellite studies are needed to refine the mass budgets of the Greenland and Antarctic ice sheets. On-site studies focused on changes in ice flow, melting, and calving should be continued and extended. Observations of water-vapor net flux will help to pin down the source of the ice sheets’ mass. A laser altimeter on a polar-orbiting satellite is needed to augment the Cool version vintage sunflower full printing low top shoesexisting radar altimetry. These instruments will provide accurate estimates of ice-sheet volume and give early warning of possible ice-sheet collapse. Other aspects of the surface energy balance need to be better understood to improve long-term cryosphere and climate predictions. These include the details controlling the spatial heterogeneity of ice surface conditions and their net influence on surface fluxes, and the extent to which seawater flooding of thin, seasonal ice cover affects their melting and albedo, particularly in the Antarctic polar oceans. Seawater flooding not only may alter the thermodynamics of the system, but may be corrupting interpretations of satellite images of ice concentration, confounding our ability to monitor the ice and evaluate the models. Internal mechanisms of cryospheric variability are usually

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