水的表现形式:降水、蒸发、渗流、径流,统称为水文现象。 降水:凡空气中水气以任何形式冷凝并降落在地表上都属于降水。降水的 形式有雨、雪、雾、雹等, 蒸发:地表向空中逸散水分,使水上升成为水气的主要途径有截留蒸发、 地面蒸发、叶面散发、水面散发、水面蒸发和海洋蒸发等5种
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R30 Model One of the simulations conducted as part of the GFDL-University Consortium project is a 17 year simulation in which the lower boundary conditions repeat the mean seasonal cycle. Attributes of the model simulation are given below
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Parallel Climate Model Effort (Version 1) This is a joint effort to develop a DOE-sponsored parallel climate model between Los Alamos National aboratory (LANL), the Naval Postgraduate School (NPG), the US Army Corps of Engineers' Cold
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Climate change output CSIRO Atmospheric Research Technical Paper No 37, 1998 Kevin J. Hennessy Contents Abstract Global climate models Regional climate models CsiRo climate models
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CCCma has develped a number of climate simulation models for climate prediction, study of climate change and variability, and to better understand the various processes which govern our climate system. A brief description of these models and their corresponding references can be found in this section
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CCSM(Coupled Model) releases Each release includes the complete collection of component model source code, documentation, input data Model output data is available Release date d CCSM 3. 0 June 2004 Notable
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HadCM3--Coupled atmosphere-Ocean general circulation model HadCM3 is a coupled atmosphere-ocean general circulation model(AOGCM)developed at the Hadley Centre and described by gordon et al (2000)and Pope et al (2000). Unlike earlier AOGCMs at the Hadley
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