Lethargic 发表于 2025-3-30 09:16:19
A Two-Dimensional Model of the Hydrological Response of a Hillslope, heavy rain, infiltration excess reaches the stream first as overland flow. Part of the infiltrated water may then flow rapidly below the surface to reemerge downslope or enter the stream. This is usually referred to as saturated subsurface flow. The rest reaches the unsaturated zone. The flow there薄荷醇 发表于 2025-3-30 13:00:53
http://reply.papertrans.cn/59/5806/580566/580566_52.pngDENT 发表于 2025-3-30 19:22:44
Fluxes in the Surface Layer Under Advective Conditions,applications it is (tacitly) assumed that the Earth’s surface is, on the scale of interest, horizontally homogeneous. An example is the way in which the surface fluxes are parameterized in models for the prediction of weather and climate. Also, most measuring techniques used for the determination of伦理学 发表于 2025-3-31 00:28:19
http://reply.papertrans.cn/59/5806/580566/580566_54.pnglobster 发表于 2025-3-31 03:19:10
Using One- or Two-Layer Models for Evaporation Estimation with Remotely Sensed Data,. Theoretical work on the precise structure of these models and the mathematical formulations of the various submodels is continuing. In many cases the models have been tested by comparisons with data, but rarely have the tests included data from many days over the same site, or data from different大吃大喝 发表于 2025-3-31 05:58:40
Water Vapor Flux Measurements from Aircraft,s of evaporation. These are necessary inputs into general circulation models that are used for weather forecasting (Mintz, 1984). They are also important for assessing and controlling water resources. Most of the techniques that have been developed over the years to estimate regional evaporation do忍耐 发表于 2025-3-31 09:34:28
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Use of Soil Moisture Measurements in Hydrologic Balance Studies,iques for land surface processes such as evapotranspiration (André et al., 1986). For fluxes from the surface layer to be useful as lower boundary conditions in general circulation models (GCM), the net radiation, sensible heat, latent heat, and soil heat fluxes must be accurately determined. Througallude 发表于 2025-3-31 22:19:30
Indirect Measurements of Fluxes Using Doppler Sodar,dary layer. The effort was initiated with a research point of view; however, rapidly considering the potential of the results, commercial systems have been built. Remote sensing with Sodar is now recognized as the most simple remote sensing technique to estimate wind and turbulence in the lower part