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

Stevens, B., Moeng, C. H., Ackerman, A. S., Bretherton, C. S., Chlond, A., De Roode, S., et al. (2005). Evaluation of large-Eddy simulations via observations of nocturnal marine stratocumulus. Monthly Weather Review, 133(6), 1443-1462. doi:10.1175/MWR2930.1.

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Stevens, B., Autor                 
Moeng, C. H., Autor
Ackerman, A. S., Autor
Bretherton, C. S., Autor
Chlond, A.1, Autor           
De Roode, S., Autor
Edwards, J., Autor
Golaz, J. C., Autor
Jiang, H. L., Autor
Khairoutdinov, M., Autor
Kirkpatrick, M. P., Autor
Lewellen, D. C., Autor
Lock, A., Autor
Mueller, F.2, Autor           
Stevens, D. E., Autor
Whelan, E., Autor
Zhu, P., Autor
Affiliations:
1Boundary Layer Measurements, The Land in the Earth System, MPI for Meteorology, Max Planck Society, Bundesstraße 53, 20146 Hamburg, DE, ou_913567              
2Climate Processes, ou_persistent22              

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 Zusammenfassung: 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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Sprache(n): eng - English
 Datum: 2005-06
 Publikationsstatus: Erschienen
 Seiten: -
 Ort, Verlag, Ausgabe: -
 Inhaltsverzeichnis: -
 Art der Begutachtung: Expertenbegutachtung
 Identifikatoren: eDoc: 256400
DOI: 10.1175/MWR2930.1
 Art des Abschluß: -

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Titel: Monthly Weather Review
  Alternativer Titel : Mon. Weather Rev.
Genre der Quelle: Zeitschrift
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Ort, Verlag, Ausgabe: -
Seiten: - Band / Heft: 133 (6) Artikelnummer: - Start- / Endseite: 1443 - 1462 Identifikator: ISSN: 0027-0644