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the ocean that can affect the atmosphere on dec-cen time scales. Variations in density play a strong role in the surface circulation as well, since the density gradients determine the volume of water contained in the surface waters, and thus the mass of water that is moved by the surface winds. This volume determines how much temperature change will result in surface waters for a given flux of heat across the air-sea boundary. Therefore, the circulation systems and property distributions of the deep and surface waters are Cool version mandala sunflower cannabis full printing low top shoesintimately linked, and constantly interact. This link is important, since it implies that the surface properties of the ocean, which play a direct and immediate role in climate, are controlled by both surface and deep-ocean processes. The question of how regional flood potential varies in response to the dec-cen climate variation patterns is of great interest. Many hydrologic parameters, including the flood potential, reflect an interaction of slow and fast time scales of large-scale climate and regional hydrologic evolution. To advance our knowledge of how regional

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