Titlebook: Land Surface — Atmosphere Interactions for Climate Modeling; Observations, Models Eric F. Wood Book 1991 Kluwer Academic Publishers 1991 Pr

dictator

BRIDE

Insight from Large-Scale Observational Studies of Land/Atmosphere Interactionsive results, either particular to individual studies or common to several, are interpreted to provide insight on the value and reliability of experimental data and field systems. This is used to provide guidance for future experiments. Progress in addressing the need to provide area-average, aggrega

Valves

flutter

Passive Microwave Remote Sensing Contribution to Hydrological Variables-based, air-borne and space-borne microwave radiometers operating at different frequencies. Specific hydrological variables addressed in this paper are soil moisture, seasonal inundation of rivers and swamps, vegetation, snow, and rainfall. Passive remote sensing provides measurements of electromagn

enflame

發(fā)生

Land Surface Hydrology in a General Circulation Model N-Global and Regional Fields Needed for Validae radiation. We explore this thesis by examination of some of the climatological fields of a 6-year model simulation, using the Community Climate Model version 1 of the National Center for Atmospheric Research with addition of a diurnal cycle and coupled to a detailed treatment of land surface proce

Temporal-Lobe

Simulation of Daily Precipitation in the Pacific Northwest Using a Weather Classification Schemeuge and classes representing regional atmospheric circulation patterns, as identified from National Meteorological Center gridded observations for a large area of the North Pacific. Weather classes were identified from daily observations of surface pressure and 850 mb pressure height at five selecte

合并

canvass

FLIT

Evapotranspiration and Runoff from Large Land Areas: Land Surface Hydrology for Atmospheric General ography, soils, soil moisture and precipitation. The framework of the model is the statistical distribution of a topography-soils index, which controls the local water balance fluxes, and is therefore taken to represent the large land area. Spatially variable water balance fluxes are integrated with