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
1. Verfasser: Otterman, J.
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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.
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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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