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under a slowly changing climate and rapidly exploding population must be monitored to provide the boundary conditions needed for model simulations and assessment of plausible future trends. Several types of observations are critical to the issues articulated above. Long-term monitoring of sea-surface salinity along with SST is important, since salinity represents the dominant control over the water density of high-latitude regions. The sea-ice distribution, motion fields, and thickness need to be known in order to determine the associated freshwater transports and buoyancy fluxes. Permafrost temperature profiles provide unique indications of integrated dec-cen climate change over vast Popular vintage sunflower full printing low top shoesgeographic regions; more such profiles should be collected in order to better define the spatial and temporal distribution of change. Consistent monitoring of iceberg calving and an observational system for determining the basal melt or growth of sea ice (e.g., an array of moored buoys measuring temperature and salinity across the floating ice shelves) must be established before the sea-ice budget can

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