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  DNS of a radiatively driven cloud-top mixing layer as a model for stratocumulus clouds

de Lózar, A., & Mellado, J.-P. (2015). DNS of a radiatively driven cloud-top mixing layer as a model for stratocumulus clouds. In J. Fröhlich (Ed.), Direct and Large-Eddy Simulation IX (ERCOFTAC Series; 20) (pp. 419-422). Heidelberg: Springer. doi:10.1007/978-3-319-14448-1_53.

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Item Permalink: https://hdl.handle.net/11858/00-001M-0000-002A-5F2C-9 Version Permalink: https://hdl.handle.net/21.11116/0000-000B-B3AC-9
Genre: Book Chapter

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978-3-319-14448-1.pdf (Publisher version), 567KB
 
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 Creators:
de Lózar, Alberto1, Author           
Mellado, Juan-Pedro1, Author           
Affiliations:
1Max Planck Research Group Turbulent Mixing Processes in the Earth System, The Atmosphere in the Earth System, MPI for Meteorology, Max Planck Society, ou_913573              

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 Abstract: The marine planetary boundary layer topped by stratocumulus clouds (STBL) is key for the planetary radiation balance. In its simplest configuration the STBL consists of a lower moist boundary layer which is topped by a dry and warm free atmosphere. The top of the STBL is populated by stratocumulus clouds that emit long wave radiation, cooling the moist boundary layer. Radiative cooling is thought to be the main source of turbulent energy for the STBL.

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Language(s): eng - English
 Dates: 20152015
 Publication Status: Issued
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 Rev. Type: Peer
 Identifiers: DOI: 10.1007/978-3-319-14448-1_53
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Title: Direct and Large-Eddy Simulation IX (ERCOFTAC Series; 20)
Source Genre: Book
 Creator(s):
Fröhlich, Jochen, Editor
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Publ. Info: Heidelberg : Springer
Pages: - Volume / Issue: - Sequence Number: - Start / End Page: 419 - 422 Identifier: ISBN: 978-3-319-14447-4