Evaluation of large-eddy simulations via observations of nocturnal marine stratocumulus

Data from the first research flight (RF01) of the second Dynamics and Chemistry of Marine Stratocumulus (DYCOMS-II) field study are used to evaluate the fidelity with which large-eddy simulations (LESs) can represent the turbulent structure of stratocumulus-topped boundary layers. The initial data and forcings for this case placed it in an interesting part of parameter space, near the boundary where cloud-top mixing is thought to render the cloud layer unstable on the one hand, or tending toward a decoupled structure on the other hand. The basis of this evaluation consists of sixteen 4-h simulations from 10 modeling centers over grids whose vertical spacing was 5 m at the cloud-top interface and whose horizontal spacing was 35 m. Extensive sensitivity studies of both the configuration of the case and the numerical setup also enhanced the analysis. Overall it was found that (i) if efforts are made to reduce spurious mixing at cloud top, either by refining the vertical grid or limiting the effects of the subgrid model in this region, then the observed turbulent and thermodynamic structure of the layer can be reproduced with some fidelity; (ii) the base, or native configuration of most simulations greatly overestimated mixing at cloud top, tending toward a decoupled layer in which cloud liquid water path and turbulent intensities were grossly underestimated; (iii) the sensitivity of the simulations to the representation of mixing at cloud top is, to a certain extent, amplified by particulars of this case. Overall the results suggest that the use of LESs to map out the behavior of the stratocumulus-topped boundary layer in this interesting region of parameter space requires a more compelling representation of processes at cloud top. In the absence of significant leaps in the understanding of subgrid-scale (SGS) physics, such a representation can only be achieved by a significant refinement in resolution--a refinement that, while conceivable given existing resources, is probably still beyond the reach of most centers.

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Copyright 2005 American Meteorological Society (AMS). Permission to use figures, tables, and brief excerpts from this work in scientific and educational works is hereby granted provided that the source is acknowledged. Any use of material in this work that is determined to be "fair use" under Section 107 of the U.S. Copyright Act or that satisfies the conditions specified in Section 108 of the U.S. Copyright Act (17 USC §108, as revised by P.L. 94-553) does not require the AMS's permission. Republication, systematic reproduction, posting in electronic form on servers, or other uses of this material, except as exempted by the above statement, requires written permission or a license form the AMS. Additional details are provided in the AMS Copyright Policy, available on the AMS Web site located at (http://www.ametsoc.org/AMS) or from the AMS at 617-227-2425 or copyright@ametsoc.org.


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Author Stevens, Bjorn
Moeng, Chin-Hoh
Ackerman, Andrew
Bretherton, Christopher
Chlond, Andreas
de Roode, Stephan
Edwards, James
Golaz, Jean-Christophe
Jiang, Hongli
Khairoutdinov, Marat
Kirkpatrick, Michael
Lewellen, David
Lock, Adrian
Müller, Frank
Stevens, David
Whelan, Eoin
Zhu, Ping
Publisher UCAR/NCAR - Library
Publication Date 2005-06-01T00:00:00
Digital Object Identifier (DOI) Not Assigned
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Topic Category geoscientificInformation
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Metadata Date 2023-08-18T18:21:10.939886
Metadata Record Identifier edu.ucar.opensky::articles:17611
Metadata Language eng; USA
Suggested Citation Stevens, Bjorn, Moeng, Chin-Hoh, Ackerman, Andrew, Bretherton, Christopher, Chlond, Andreas, de Roode, Stephan, Edwards, James, Golaz, Jean-Christophe, Jiang, Hongli, Khairoutdinov, Marat, Kirkpatrick, Michael, Lewellen, David, Lock, Adrian, Müller, Frank, Stevens, David, Whelan, Eoin, Zhu, Ping. (2005). Evaluation of large-eddy simulations via observations of nocturnal marine stratocumulus. UCAR/NCAR - Library. http://n2t.net/ark:/85065/d7wm1fqk. Accessed 13 May 2025.

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