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- W2891748660 abstract "Atmospheric convection is an essential aspect of atmospheric movement, and it is a source of errors in Climate Models. Being able to generate approximate limit formulas and compare the estimations they produce, could give a way to reduce them. In this article, it is shown that it is enough to assume that the velocity's $L^2$-norm is bounded, has locally integrable, $L^1_{loc}$, weak partial derivatives up to order two, and a negligible variation of its first velocity's coordinate in direction parallel to the surface, to obtain a Reynolds' limit formula for a Dorodnitzyn's compressible gaseous Boundary Layer in atmospheric conditions." @default.
- W2891748660 created "2018-09-27" @default.
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- W2891748660 date "2018-08-18" @default.
- W2891748660 modified "2023-09-27" @default.
- W2891748660 title "REYNOLDS' LIMIT FORMULA FOR DORODNITZYN'S ATMOSPHERIC BOUNDARY LAYER MODEL IN CONVECTIVE CONDITIONS" @default.
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- W2891748660 doi "https://doi.org/10.12732/ijam.v31i4.12" @default.
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