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000903176 1001_ $$0P:(DE-Juel1)165588$$aPoll, S.$$b0$$eCorresponding author
000903176 245__ $$aGrid resolution dependency of land surface heterogeneity effects on boundary‐layer structure
000903176 260__ $$aWeinheim [u.a.]$$bWiley$$c2022
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000903176 520__ $$aLand surface heterogeneity exerts a strong control on atmospheric boundary-layer (ABL) evolution by spatially varying the distribution and partitioning of surface energy fluxes and triggering secondary circulations. The representation of this physical process in numerical weather prediction (NWP) models is especially affected in the terra incognita as the model grid resolution approaches the length-scale of the largest eddies in the boundary layer. We explore these effects for a mesoscale strip-like land surface inhomogeneity in land cover, soil moisture or a superposition of both embedded in an elsewhere homogeneous landscape. The study is conducted with the numerical weather prediction model ICON (ICOsahedral Nonhydrostatic), using the default operational level 2.5 Mellor–Yamada turbulence closure (MY) and a large-eddy simulation (LES) configuration as a benchmark. While simulations with the default ABL scheme approach the LES reference when refining the spatial grid towards finer resolution, the model generates artificial circulations leading to ABL height oscillations when the horizontal grid resolution (∆
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000903176 7001_ $$0P:(DE-HGF)0$$aShrestha, P.$$b1
000903176 7001_ $$0P:(DE-HGF)0$$aSimmer, C.$$b2
000903176 773__ $$0PERI:(DE-600)2089168-4$$a10.1002/qj.4196$$gp. qj.4196$$n Part A$$p141-158$$tQuarterly journal of the Royal Meteorological Society$$v148$$x0035-9009$$y2022
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000903176 9141_ $$y2022
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