Convective water exchanges during differential cooling and heating: implications for dissolved constituent transport

Abstract

Convective water exchange patterns, determined from water temperature variations, were examined in the Minky Creek embayment of Guntersville Reservoir, Alabama (USA), during the month of September, 1990. During periods of differential cooling, cooler water originating from shallow stations moved as an underflow current toward the center of the embayment, while warmer water moved as an overflow current toward the shore. During periods of differential heating, convective exchange was much more shallow, occurring in the upper 3 m of the water column. As warmer water from shallow regions moved out as an overrflow current, this water was replaced by a return flow of cooler water originating from the pelagic epilimnion. Wind speed appeared to influence convective exchange patterns during differential heating phases by affecting the depth of the surface mixed layer. The potential for convective exchanges during periods of differential cooling and heating occurred on 54% and 74% of the days, respectively, in September. This high potential for horizontal water exchanges in Guntersville Reservoir has strong implications for the lateral transport of dissolved constituents.