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Titlebook: Handbook of Hydrometeorological Ensemble Forecasting; Qingyun Duan,Florian Pappenberger,John C. Schaake Reference work 2019 Springer-Verla

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發(fā)表于 2025-3-26 22:44:06 | 只看該作者
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發(fā)表于 2025-3-27 01:20:53 | 只看該作者
Distributed Hydrological Modelsteorology, computer science and engineering, and other related science and engineering disciplines, divide the terrain of a basin into fine-resolution cells and calculate the hydrological processes at both the cell and basin scales. Numerous PBDHMs have been proposed. Because PBDHMs can model hydrol
33#
發(fā)表于 2025-3-27 09:15:16 | 只看該作者
Land Surface Hydrological Models “parent” atmospheric model. Topics include atmospheric forcing to LSMs, land data sets, surface-layer turbulence, surface fluxes and energy and water budgets, land-surface physics, and the role of the land states and surface fluxes in local land-atmosphere interaction. Connections of LSMs with hydr
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發(fā)表于 2025-3-27 10:21:22 | 只看該作者
ment: ecology, economy, society, environment, and culture. This aims to reinvigorate urban waterfront spaces, restore the ecological integrity of the area, preserve the humanistic essence of the old city while enhancing residents’ sense of belonging, enhance the living environment, and uphold the city’s cultural and historical legacy.
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發(fā)表于 2025-3-27 15:13:32 | 只看該作者
Malaquias Pe?a,L. Gwen Chen,Huug van den Doolhe events better is presented; the events of 1989 brought the countries of Central Europe back to their pre-revolutionary path of development which constitutes the events the “postponed counterrevolution”.
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發(fā)表于 2025-3-27 20:10:18 | 只看該作者
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發(fā)表于 2025-3-28 00:41:58 | 只看該作者
12.2). . .). Nous développons la notion de . d’un module sur un schéma formel idyllique qui jouera un r?le important dans la suite de ce traité. Nous étudions enfin les propriétés différentielles des schémas formels idylliques.
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發(fā)表于 2025-3-28 05:56:48 | 只看該作者
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發(fā)表于 2025-3-28 09:17:26 | 只看該作者
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發(fā)表于 2025-3-28 12:04:33 | 只看該作者
Land Surface Hydrological Models budgets, land-surface physics, and the role of the land states and surface fluxes in local land-atmosphere interaction. Connections of LSMs with hydrological models (e.g., saturated zone or groundwater, and streamflow or river-routing) and land data assimilation are outside the scope of this chapter.
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