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• W2160716278 abstract "The article examines the flow generated by time‐periodic variations in surface temperature along an infinite slope in an initially unperturbed, stably stratified atmosphere at rest. Uniform boundary conditions at the surface are conducive to an along‐slope parallel flow, governed by a periodically reversing local imbalance between along‐slope advection and slope‐normal fluxes of momentum and heat. It is shown that solutions include both a transient part and a periodic regime and that three different flow regimes may occur. The properties of the solutions in each regime are examined and discussed, outlining novelties with respect to previously known results." @default.
• W2160716278 created "2016-06-24" @default.
• W2160716278 creator A5014932541 @default.
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• W2160716278 date "2014-12-27" @default.
• W2160716278 modified "2023-10-03" @default.
• W2160716278 title "An analytic solution for time‐periodic thermally driven slope flows" @default.
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• W2160716278 doi "https://doi.org/10.1002/qj.2485" @default.
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