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  • Surface resistance  (2)
  • Latent heat flux  (1)
  • Springer  (2)
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  • Springer  (2)
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  • 1
    Electronic Resource
    Electronic Resource
    The behaviour of a mixed-layer model of the convective boundary layer coupled to a big leaf model of surface energy partitioning (1998)
    Springer
    Boundary layer meteorology 88 (1998), S. 87-101 
    Details
    ISSN: 1573-1472
    Keywords: Atmospheric boundary layer ; Diurnal variability ; Latent heat flux ; Priestley-Taylor coefficient ; Surface resistance
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract Daily mean values of the Priestley-Taylor coefficient, α¯, are derived from a simple model of the daily growth of a convective boundary layer. For a particular control set of driving environmental variables, α¯ is related to the prescribed bulk surface resistance, rS by 1/α¯ = 1/α0 + mrS for parameters α0 and m. The dependence of the parameters α0 and m on weather is explored and a potential use of this linear relation to provide information about regional values of rS is indicated.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1023/A:1001110819090
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    Paper (German National Licenses)
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  • 2
    Electronic Resource
    Electronic Resource
    The Effect of Orography on Evaporation (1998)
    Springer
    Boundary layer meteorology 86 (1998), S. 487-504 
    Details
    ISSN: 1573-1472
    Keywords: Orography ; Planetary boundary layer ; Atmospheric feedback ; Surface resistance
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract The effect of orography on the spatial variability of surface evaporation is studied numerically for two hill heights and two prescribed forms of surface resistance. A numerical model of the planetary boundary layer carrying scalars of temperature and specific humidity, and with a surface energy balance scheme, is employed. It is found that the difference in mean evaporation between model runs with hills and analogous runs for flat terrain may be explained primarily by an increase in surface area and adiabatic cooling at the hill surface.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1023/A:1000795206459
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    Paper (German National Licenses)
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