Bulk parameterization
Published: March 30, 2010, 12:00 am
Updated: December 17, 2011, 4:34 pm
This article has been reviewed by the following Topic Editor:
C Michael Hogan
Bulk parameterization is a concept in physical oceanography. In studying air–sea interactions, it is difficult to obtain direct measurements of the surface fluxes, and those that are available are extremely limited in geographic scope. Therefore, extensive, global–scale estimates must be obtained via parameterizations of the surface fluxes that permit the use of more easily obtained quantities. The basic premise of the concept of bulk parameterizations is to relate the surface layer fluxes to logarithmic profiles of the mean quantities. The fluxes can then be determined from the mean wind, temperature and humidity at a single height by introducing bulk transfer coefficients of heat, moisture and momentum. This method is also used to quantify gas exchange processes.
Further Reading
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Seas of the world on the Encyclopedia of Earth
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G. L. Geernaert. Bulk parameterizations for the wind stress and heat flux. In G. L. Geernaert and W. Plant, editors, Surface Waves and Fluxes, Vol. 1, pages 91-172. Kluwer Academic, 1990.
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David P. Rogers. Air-sea interaction: connecting the ocean and atmosphere. Rev. Geophys., 33 Supp.:?, 1995
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Citation
Steve Baum (Lead Author);C Michael Hogan (Topic Editor) "Bulk parameterization". In: Encyclopedia of Earth. Eds. Cutler J. Cleveland (Washington, D.C.: Environmental Information Coalition, National Council for Science and the Environment). [First published in the Encyclopedia of Earth March 30, 2010; Last revised Date December 17, 2011; Retrieved May 23, 2013 <http://www.eoearth.org/article/Bulk_parameterizations>
The Author
Assistant Research Scientist, Physical Section
Department of Oceanography
Texas A&M University ... (Full Bio)
Bulk parameterization is a concept in physical oceanography. In studying air–sea interactions, it is difficult to obtain direct measurements of the surface fluxes, and those that are available are extremely limited in geographic scope. Therefore, extensive, global–scale estimates must be obtained via parameterizations of the surface fluxes that permit the use of more easily obtained quantities. The basic premise of the concept of bulk parameterizations is to relate the surface layer fluxes to logarithmic profiles of the mean quantities. The fluxes can then be determined from the mean wind, temperature and humidity at a single height by introducing bulk transfer coefficients of heat, moisture and momentum. This method is also used to quantify gas exchange processes.
Further Reading
-
Seas of the world on the Encyclopedia of Earth
-
G. L. Geernaert. Bulk parameterizations for the wind stress and heat flux. In G. L. Geernaert and W. Plant, editors, Surface Waves and Fluxes, Vol. 1, pages 91-172. Kluwer Academic, 1990.
-
David P. Rogers. Air-sea interaction: connecting the ocean and atmosphere. Rev. Geophys., 33 Supp.:?, 1995
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