Calculation of surface temperature and surface fluxes in the GLAS GOM
Because the GLAS model's surface fluxes of sensible and latent heat exhibit strong 2 delta t oscillations at the individual grid points as well as in the zonal hemispheric averages and because a basic weakness of the GLAS model lower evaporation over oceans and higher evaporation over land in a...
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creator | Sud, Y. C. Abeles, J. A. |
description | Because the GLAS model's surface fluxes of sensible and latent heat exhibit strong 2 delta t oscillations at the individual grid points as well as in the zonal hemispheric averages and because a basic weakness of the GLAS model lower evaporation over oceans and higher evaporation over land in a typical monthly simulation, the GLAS model PBL parameterization was changed to calculate the mixed layer temperature gradient by solution of a quadratic equation for a stable PBL and by a curve fit relation for an unstable PBL. The new fluxes without any 2 delta t oscillation. Also, the geographical distributions of the surface fluxes are improved. The parameterization presented is incorporated into the new GLAS climate model. Some results which compare the evaporation over land and ocean between old and new calculations are appended. |
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A.</creatorcontrib><description>Because the GLAS model's surface fluxes of sensible and latent heat exhibit strong 2 delta t oscillations at the individual grid points as well as in the zonal hemispheric averages and because a basic weakness of the GLAS model lower evaporation over oceans and higher evaporation over land in a typical monthly simulation, the GLAS model PBL parameterization was changed to calculate the mixed layer temperature gradient by solution of a quadratic equation for a stable PBL and by a curve fit relation for an unstable PBL. The new fluxes without any 2 delta t oscillation. Also, the geographical distributions of the surface fluxes are improved. The parameterization presented is incorporated into the new GLAS climate model. Some results which compare the evaporation over land and ocean between old and new calculations are appended.</description><language>eng</language><publisher>Legacy CDMS</publisher><subject>Geophysics</subject><creationdate>1981</creationdate><rights>Copyright Determination: GOV_PUBLIC_USE_PERMITTED</rights><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>781,801</link.rule.ids><linktorsrc>$$Uhttps://ntrs.nasa.gov/citations/19810021159$$EView_record_in_NASA$$FView_record_in_$$GNASA$$Hfree_for_read</linktorsrc></links><search><creatorcontrib>Sud, Y. C.</creatorcontrib><creatorcontrib>Abeles, J. A.</creatorcontrib><title>Calculation of surface temperature and surface fluxes in the GLAS GOM</title><description>Because the GLAS model's surface fluxes of sensible and latent heat exhibit strong 2 delta t oscillations at the individual grid points as well as in the zonal hemispheric averages and because a basic weakness of the GLAS model lower evaporation over oceans and higher evaporation over land in a typical monthly simulation, the GLAS model PBL parameterization was changed to calculate the mixed layer temperature gradient by solution of a quadratic equation for a stable PBL and by a curve fit relation for an unstable PBL. The new fluxes without any 2 delta t oscillation. Also, the geographical distributions of the surface fluxes are improved. The parameterization presented is incorporated into the new GLAS climate model. Some results which compare the evaporation over land and ocean between old and new calculations are appended.</description><subject>Geophysics</subject><fulltext>true</fulltext><rsrctype>report</rsrctype><creationdate>1981</creationdate><recordtype>report</recordtype><sourceid>CYI</sourceid><recordid>eNrjZHB1TsxJLs1JLMnMz1PIT1MoLi1KS0xOVShJzS1ILUosKS1KVUjMS4GLp-WUVqQWK2TmKZRkpCq4-zgGK7j7-_IwsKYl5hSn8kJpbgYZN9cQZw_dvMTixPi8kqLieENLC0MDAyNDQ1NLYwLSAIbrLhQ</recordid><startdate>19810701</startdate><enddate>19810701</enddate><creator>Sud, Y. C.</creator><creator>Abeles, J. A.</creator><scope>CYE</scope><scope>CYI</scope></search><sort><creationdate>19810701</creationdate><title>Calculation of surface temperature and surface fluxes in the GLAS GOM</title><author>Sud, Y. C. ; Abeles, J. A.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-nasa_ntrs_198100211593</frbrgroupid><rsrctype>reports</rsrctype><prefilter>reports</prefilter><language>eng</language><creationdate>1981</creationdate><topic>Geophysics</topic><toplevel>online_resources</toplevel><creatorcontrib>Sud, Y. C.</creatorcontrib><creatorcontrib>Abeles, J. A.</creatorcontrib><collection>NASA Scientific and Technical Information</collection><collection>NASA Technical Reports Server</collection></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext_linktorsrc</fulltext></delivery><addata><au>Sud, Y. C.</au><au>Abeles, J. A.</au><format>book</format><genre>unknown</genre><ristype>RPRT</ristype><btitle>Calculation of surface temperature and surface fluxes in the GLAS GOM</btitle><date>1981-07-01</date><risdate>1981</risdate><abstract>Because the GLAS model's surface fluxes of sensible and latent heat exhibit strong 2 delta t oscillations at the individual grid points as well as in the zonal hemispheric averages and because a basic weakness of the GLAS model lower evaporation over oceans and higher evaporation over land in a typical monthly simulation, the GLAS model PBL parameterization was changed to calculate the mixed layer temperature gradient by solution of a quadratic equation for a stable PBL and by a curve fit relation for an unstable PBL. The new fluxes without any 2 delta t oscillation. Also, the geographical distributions of the surface fluxes are improved. The parameterization presented is incorporated into the new GLAS climate model. Some results which compare the evaporation over land and ocean between old and new calculations are appended.</abstract><cop>Legacy CDMS</cop><oa>free_for_read</oa></addata></record> |
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title | Calculation of surface temperature and surface fluxes in the GLAS GOM |
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