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- W2029486513 abstract "Several variations of a basic energy budget model were tested under varying atmospheric stability conditions using temperature data from Lake Mendota and meteorologic data from nearby Truax Airfield, Madison, Wisconsin. The flux enhancements predicted by Model 1 (Deardorff) for prevailing over-lake lapse conditions were inconsistent with measured changes in lake heat storage. When using the Budyko formulation for sky emissivity, ε, satisfactory energy residuals were obtained by eliminating the lapse enhancement while retaining the suppressive effects of over-lake inversions (Model 2 = modified Deardorff). Here, the best estimate of the 10 m Dalton coefficient was 1.45 × 10−3 (cgs units; neutral profile). However, when the Koberg model for ε was adopted instead, satisfactory energy residuals were obtained only after eliminating all adjustments for non-neutral conditions, and increasing the 10 m Dalton coefficient to approximately 1.55 × 10−3 (Model 3). Models 2 and 3 predicted annual evaporation from Lake Mendota of 71 and 86 cm during 1977 (including approximately 6 cm of sublimation during ice cover), bracketing earlier estimates for this locality (76 cm) based on U.S. Weather Bureau Class A pan data, and consistent with intensive studies of Pretty Lake in northern Indiana. My estimates of the 10 m Dalton coefficient (1.45 × 10−3 to 1.55 × 10−3) also narrowly bracket values for Lake Hefner and Lake Mead (1.49 × 10−3), obtained in studies by the U.S. Geological Survey. Moreover, as in the case of the Will Rogers airport near Lake Hefner, meteorologic data collected at Truax Airfield, Wisconsin, proved adequate for estimating sensible and latent heat transfer over the adjacent lake." @default.
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- W2029486513 date "1991-11-01" @default.
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- W2029486513 title "Testing lake energy budget models under varying atmospheric stability conditions" @default.
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- W2029486513 doi "https://doi.org/10.1016/0022-1694(91)90134-4" @default.
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