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- W2094367037 abstract "When warm air flows from land over a cooler sea, the air is modified. It is shown that h = cX ½ , where h is the height (in meters) of this modified layer over the water, X is the distance downwind from the coast (i.e., the fetch), and c is the proportionality constant. This equation is simplified from a theoretical equation and two independent dimensional analyses. Applying the simplified equation to data from four field studies, particularly the 1979 Monsoon Experiments, in which data sets were obtained under 100‐ to 1000‐km‐long fetch conditions, c is found to be approximately 18. Commonly observed values for the pertinent parameters are used. Variation in h is less than 20% as compared with results obtained by using theoretical equations and dimensional analyses individually. Note that this variation is comparable to the contribution of entrainment, which was not taken into account in the other formulas." @default.
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- W2094367037 date "1983-01-20" @default.
- W2094367037 modified "2023-09-27" @default.
- W2094367037 title "On the growth of a thermally modified boundary layer by advection of warm air over a cooler sea" @default.
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- W2094367037 doi "https://doi.org/10.1029/jc088ic01p00771" @default.
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