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dc.creatorHu, Xiao-Ming
dc.creatorNielsen-Gammon, John
dc.creatorZhang, Fuqing
dc.date.accessioned2016-10-28T20:31:07Z
dc.date.available2016-10-28T20:31:07Z
dc.date.issued2010-09-01
dc.identifier.citationHu, X.-M., J. W. Nielsen-Gammon, and F. Zhang, 2010: Evaluation of three planetary boundary layer schemes in the WRF model. J. Appl. Meteor. Clim., 49, 1831-1844, doi: 10.1175/2010JAMC2432.1.en
dc.identifier.urihttps://hdl.handle.net/1969.1/158241
dc.description© Copyright 2010 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 September 2010 Page 2 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, such as on a web site or in a searchable database, or other uses of this material, except as exempted by the above statement, requires written permission or a license from the AMS. Additional details are provided in the AMS Copyright Policy, available on the AMS Web site located at (https://www.ametsoc.org/) or from the AMS at 617-227-2425 or copyrights@ametsoc.org.en
dc.description.abstractAccurate depiction of meteorological conditions, especially within the planetary boundary layer (PBL), is important for air pollution modeling, and PBL parameterization schemes play a critical role in simulating the boundary layer. This study examines the sensitivity of the performance of the Weather Research and Forecast (WRF) model to the use of three different PBL schemes [Mellor–Yamada–Janjic (MYJ), Yonsei University (YSU), and the asymmetric convective model, version 2 (ACM2)]. Comparison of surface and boundary layer observations with 92 sets of daily, 36-h high-resolution WRF simulations with different schemes over Texas in July–September 2005 shows that the simulations with the YSU and ACM2 schemes give much less bias than with the MYJ scheme. Simulations with the MYJ scheme, the only local closure scheme of the three, produced the coldest and moistest biases in the PBL. The differences among the schemes are found to be due predominantly to differences in vertical mixing strength and entrainment of air from above the PBL. A sensitivity experiment with the ACM2 scheme confirms this diagnosis.en
dc.description.sponsorshipTexas Environmental Research Consortium Texas Commission on Environmental Qualityen
dc.language.isoen_US
dc.publisherAmerican Meteorological Society
dc.titleEvaluation of Three Planetary Boundary Layer Schemes in the WRF Modelen
dc.typeArticleen
local.departmentAtmospheric Sciencesen
dc.identifier.doi10.1175/2010JAMC2432.1


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