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

Pessimistic

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neologism

Partial Analysis Applied to Scale Problems in Surface Moisture Fluxese widely different scales of the soil particle, a soil pedon, a field, a basin and a biome. It is suggested that simplified models can be used at these different scales to provide bounding solutions to the integrated behaviour of land surface fluxes of interest in linking hydrologic models and general circulation climate models.

CHOIR

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Consensus

https://doi.org/10.1007/978-94-009-2155-9Precipitation; Scale; Weather; hydrology; moisture; hydrogeology

規(guī)范就好

Passive Microwave Remote Sensing Contribution to Hydrological Variables the relationship between microwave observations to a particular hydrological variable leads to uncertainties in the estimation of the variable. Notwithstanding this limitation, the principles and the examples given in this paper illustrate the value of passive microwave observations to regional and

喃喃而言

Land Surface Hydrology in a General Circulation Model N-Global and Regional Fields Needed for Validaonsider the annual cycle of model hydrological fields (soil moisture, runoff, precipitation, evapotranspiration, net radiation) averaged over a box covering the central part of the United States (roughly the Mississippi basin). The seasonal cycle of evapotranspiration over this box appears to be dom

輕彈

Simulation of Daily Precipitation in the Pacific Northwest Using a Weather Classification Schemeassumed to be geometric, and the precipitation amounts for each class and season were fitted with a mixed exponential distribution. Parameters of the length of stay distributions, transition probabilities, and precipitation amounts were estimated from the period of record 1975–84..The fitted model w

Biomarker

A Refinement of the Combination Equations for Evaporationions leads to a simple approximate expression for the error associated with the linear case. Equations based on the conventional linear approximation consistently underestimate evaporation, sometimes by a substantial amount.

ATRIA

解脫

Distributed Parameterization of Complex Terraino incorporate the effects of landscape variability and horizontal divergence of energy and water. The strategy is then to trade off the detail and rigor of point exchange calculations for the ability to repeat those calculations over extensive, complex terrain. It is clear the parameterization proce