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contributor authorZhou, Bowen
contributor authorXue, Ming
contributor authorZhu, Kefeng
date accessioned2019-09-19T10:07:49Z
date available2019-09-19T10:07:49Z
date copyright2/6/2018 12:00:00 AM
date issued2018
identifier otherjas-d-17-0346.1.pdf
identifier urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4261862
description abstractAbstractA grid-refinement-based method is implemented in a community atmospheric model to improve the representation of convective boundary layer (CBL) turbulence on gray-zone [i.e., ~O(1) km] grids. At this resolution, CBL convection is partially resolved and partially subgrid scale (SGS), such that neither traditional mesoscale planetary boundary layer (PBL) schemes nor SGS closures for large-eddy simulations (LESs) are appropriate. The proposed method utilizes two-way interactive nesting to refine the horizontal resolution of the unstable surface layer of the daytime CBL. SGS turbulent mixing in the fine nest and coarse parent grids are parameterized by an LES turbulence closure and a PBL scheme, respectively. The method does not rely on predetermined empirical functions to introduce grid (scale) dependency and in theory works with any PBL scheme. Compared to the stand-alone gray-zone simulation, the proposed approach shows improvements in terms of higher-order statistics, the timing of the onset of resolved convection, and the convective structures. A deficiency of the method exists when the nest domain is limited to the surface layer; the convective structures become gradually contaminated by spurious convection on the parent gray-zone grid. A deeper nest domain alleviates the issue at increased computational costs.
publisherAmerican Meteorological Society
titleA Grid-Refinement-Based Approach for Modeling the Convective Boundary Layer in the Gray Zone: Algorithm Implementation and Testing
typeJournal Paper
journal volume75
journal issue4
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/JAS-D-17-0346.1
journal fristpage1143
journal lastpage1161
treeJournal of the Atmospheric Sciences:;2018:;volume 075:;issue 004
contenttypeFulltext


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