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

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发表于 2025-3-21 19:17:00 | 显示全部楼层 |阅读模式
书目名称Land Surface — Atmosphere Interactions for Climate Modeling
副标题Observations, Models
编辑Eric F. Wood
视频video
图书封面Titlebook: Land Surface — Atmosphere Interactions for Climate Modeling; Observations, Models Eric F. Wood Book 1991 Kluwer Academic Publishers 1991 Pr
描述It is well known that the interactions between land surfaces and the atmosphere, and the resulting exchanges in water and energy have a tremendous affect on climate. The inadequate representation of land-atmosphere interactions is a major weakness in current climate models, and is providing the motivation for the HAPEX and ISLSCP experiments as well as the proposed Global Energy and Water Experiment (GEWEX) and the Earth Observing System (EOS) mission. The inadequate representation reflects the recognition that the well-known phys­ ical relationships, which are well described at small scales, result in different relationships when represented at the scales used in climate models. Understanding this transition in the mathematical relationships with increased space-time scales appears to be very difficult, and has led to different approaches; at one extreme, the famous "bucket" model where the land-surface is a simple one layer storage without vegetation; the other extreme may be Seller‘s Simple Biosphere Model (Sib) where one big leaf covers the climate model grid. Given the heterogeneous nature of landforms, soils and vegetation within a climate model grid, the development of new l
出版日期Book 1991
关键词Precipitation; Scale; Weather; hydrology; moisture; hydrogeology
版次1
doihttps://doi.org/10.1007/978-94-009-2155-9
isbn_softcover978-94-010-7470-4
isbn_ebook978-94-009-2155-9
copyrightKluwer Academic Publishers 1991
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发表于 2025-3-21 21:02:41 | 显示全部楼层
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.
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https://doi.org/10.1007/978-94-009-2155-9Precipitation; Scale; Weather; hydrology; moisture; hydrogeology
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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
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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
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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
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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.
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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
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