Titlebook: Land Surface Evaporation; Measurement and Para Thomas J. Schmugge,Jean-Claude André (Director) Book 1991 Springer-Verlag New York Inc. 1991

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书目名称Land Surface Evaporation影响因子(影响力)




书目名称Land Surface Evaporation影响因子(影响力)学科排名




书目名称Land Surface Evaporation网络公开度




书目名称Land Surface Evaporation网络公开度学科排名




书目名称Land Surface Evaporation被引频次




书目名称Land Surface Evaporation被引频次学科排名




书目名称Land Surface Evaporation年度引用




书目名称Land Surface Evaporation年度引用学科排名




书目名称Land Surface Evaporation读者反馈




书目名称Land Surface Evaporation读者反馈学科排名

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Indirect Measurements of Fluxes Using Doppler Sodar,d Coulter, 1986) have led to a better understanding of the different parts of the boundary layer. For more information about these results and a historical point of view of acoustic sounding, see Little (1969), Weill (1981), Underwood (1984), Singal (1988), and Kallistratova (1959).

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Use of Soil Moisture Measurements in Hydrologic Balance Studies,st, cost-effective data sets that can be collected regionally on a large scale hydrologic experiment. This article discusses application of soil moisture measurement techniques for estimation and verification of the latent heat flux, which includes evaporation from soil and plant surfaces and transpiration from plants.

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In Situ Water Vapor Measurements in the Lyman-alpha and Infrared Spectrum: Theory and Components,ty-temperature conditions, and become more severe at lower and higher temperatures, especially at the lowest and highest relative humidities. Absorption by and adsorption on the components of the system leading to the transducer element can readily produce misleading results especially when the humidity rapidly decreases by an order of magnitude.

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and surface. Thus, in the context of climate modeling, it became important to develop techniques which would realistically estimate the evaporation flux on land. .Land Surface Evaporation: Measurement and . .Parameterization. discusses strategies for the use of experimental data in developing and te

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Parameterization of Land-Surface Processes in Numerical Weather Prediction,ce fluxes and with at least the background of the most widely used formulations (see, e.g., Rowntree, this volume). So this chapter concentrates on the practical problems of accounting for land-surface processes in NWPMs.

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Temporal Variation of Heat and Moisture Flux Within the Atmospheric Boundary Layer over a Grasslandis the focus, especially variability on the subdiurnal time scale. Several physical processes are presented that could account for subdiurnal time variability and an example of the effect of turbulent transport throughout the depth of the ABL is demonstrated.