A simple two-system-parameter model for surface-effected warming of the planetary boundary layer
The transabsorptivity concept which specifies the heat input into the PBL resulting from surface-atmosphere interactions is discussed. This concept is examined in terms of governing equations, and transabsorptivity is defined as the product of the surface absorptivity and the transfer efficiency. It...
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Veröffentlicht in: | Boundary-layer meteorology 1990-05, Vol.51 (3, Ma), p.213-227 |
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description | The transabsorptivity concept which specifies the heat input into the PBL resulting from surface-atmosphere interactions is discussed. This concept is examined in terms of governing equations, and transabsorptivity is defined as the product of the surface absorptivity and the transfer efficiency. It is proposed that the climatic effects of surface changes be formulated in terms of changes in the transabsorptivity. A diagram of the surface-atmosphere interactions is provided. |
doi_str_mv | 10.1007/BF00122138 |
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This concept is examined in terms of governing equations, and transabsorptivity is defined as the product of the surface absorptivity and the transfer efficiency. It is proposed that the climatic effects of surface changes be formulated in terms of changes in the transabsorptivity. A diagram of the surface-atmosphere interactions is provided.</description><subject>Convection, turbulence, diffusion. 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Boundary layer structure and dynamics</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>External geophysics</topic><topic>Meteorology</topic><topic>Meteorology And Climatology</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Otterman, J.</creatorcontrib><collection>NASA Scientific and Technical Information</collection><collection>NASA Technical Reports Server</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><jtitle>Boundary-layer meteorology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Otterman, J.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>A simple two-system-parameter model for surface-effected warming of the planetary boundary layer</atitle><jtitle>Boundary-layer meteorology</jtitle><date>1990-05</date><risdate>1990</risdate><volume>51</volume><issue>3, Ma</issue><spage>213</spage><epage>227</epage><pages>213-227</pages><issn>0006-8314</issn><eissn>1573-1472</eissn><coden>BLMEBR</coden><abstract>The transabsorptivity concept which specifies the heat input into the PBL resulting from surface-atmosphere interactions is discussed. This concept is examined in terms of governing equations, and transabsorptivity is defined as the product of the surface absorptivity and the transfer efficiency. It is proposed that the climatic effects of surface changes be formulated in terms of changes in the transabsorptivity. A diagram of the surface-atmosphere interactions is provided.</abstract><cop>Legacy CDMS</cop><pub>Springer</pub><doi>10.1007/BF00122138</doi><tpages>15</tpages></addata></record> |
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source | Springer Nature - Complete Springer Journals; NASA Technical Reports Server |
subjects | Convection, turbulence, diffusion. Boundary layer structure and dynamics Earth, ocean, space Exact sciences and technology External geophysics Meteorology Meteorology And Climatology |
title | A simple two-system-parameter model for surface-effected warming of the planetary boundary layer |
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