By G. Dennis Cooke
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Extra resources for Lake and Reservoir Restoration
This source may be very minor, but a walk around some or all of a lake's perimeter during a rainstorm may be needed to confirm that conclusion. Some workers have assigned this component of the hydrologie equation to the residual term (along with groundwater), but this increases the potential for error in the overall budget. Others have used the Soil Conservation Service technique described by Mockus (1971), in which soil infiltration characteristics, five-day antecedent precipitation, and land use are used to calculate overland flow.
7) gave accurate predictions in 80 percent of the study lakes; the other models were accurate in 70 percent of the lakes tested. Reckhow (1979a; b) describes a method of estimating the total uncertainty or reliability of a prediction in which Vollenweider's (1976) model (eq. 7) was used. Calculation of uncertainty in the prediction is important, since this provides a measure of the value of the information contained in the prediction and thus allows the user to weigh the results in any decision-making process.
The prediction of internal phosphorus load in lakes with anoxic hypolimnia. M. 1977. Nonpoint Source-Stream Nutrient Level Relationships: A Nationwide Study. EPA 600/3-77-105. W. 1957. Species composition of limnetic Zooplankton communities. Limnol Oceanogr 2:222-232. L. 1968. Runoff characteristics in the Great Lakes Basin. Proc 11th Conf Great Lakes Res 11:326-359. G. 1975. Sediment movement from loessial watersheds. In Present and Prospective Technology for Predicting Sediment Yields and Sources, Proc.