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Metro-hydrological, biophysical data integration for water circulation and water resource simulation from watershed to basin scales in a distributed schemes

机译:在分布式方案中,从流域到流域尺度的水循环和水资源模拟的地铁 - 水文,生物物理数据集成

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摘要

Integration of spatial metero_hydrological, biophysical data to drive terrestrial water circulation models requires not only that the data layers themselves be spatially compatible, but also that they adequately resolve landscape attributes that the models require. Two study sites, one located at the semi_arid region of Heihe River Basin in northwestern China and another in humid area of Yangtze River Basin in Hanjiang plain, have been selected to simulate water dynamics and soil erosion process at watershed (several hundreds km2)to basin (4,0002km) scales by integrating soils, topographic, vegetation, and meteorological data with varying data resolutions and levels of topographic aggregation. Preliminary simulations indicate that spatial correlation of input variables with synoptic weather patterns is critical in determining dynamic processes such as hydrologic outflow and evapotranspiration, yet is not always possible across large regions or heterogeneous terrain. Simulation of hydrological processes at watershed to basin scales typically requires both intensive and extensive biophysical and meteorological parameterization of the earthu27s surface and atmosphere. Unfortunately, critical processes governing the interaction between terrain surface-vegetation-atmosphere at spatial scales from local to regional, and at temporal scales that range from instantaneous to seasonal, are not easily incorporated into such models that require multiple data of fixed spatial or temporal resolution as input at present. In order for the distributed models to adequately describe or predict physical processes such as streamflow dynamics, input data resolution must be compatible not only with the scale of actual hydrological functioning, but also with the resolution at which interpretation of results is critical. In this paper, the general objectives of the research undertaken in Nanjing University within a large multidisciplinary project named simply as “973”, founded by Ministry of Science & Technology, China were reviewed, the current progress and the problems existed for further efforts were discussed.
机译:集成空间水文,生物物理数据以驱动陆地水循环模型不仅需要数据层本身在空间上兼容,而且还需要它们充分解析模型所需的景观属性。选择了两个研究地点,一个位于中国西北黑河流域的半干旱地区,另一个位于汉江平原的长江流域的湿润地区,以模拟流域(数百平方公里)流域的水动力学和土壤侵蚀过程。 (4,0002 km)通过将土壤,地形,植被和气象数据与不同的数据分辨率和地形聚合级别进行集成来进行缩放。初步模拟表明,输入变量与天气天气模式的空间相关性对于确定动态过程(例如水文流量和蒸散量)至关重要,但是在大区域或异质地形上并非总是可能的。从流域到流域尺度的水文过程模拟通常需要对地球表面和大气层进行密集和广泛的生物物理和气象参数设置。不幸的是,控制从本地到区域的空间尺度以及从瞬时到季节性的时间尺度的地形地表-植被-大气之间的相互作用的关键过程不容易被整合到这样的模型中,这些模型需要具有固定的空间或时间分辨率的多个数据作为目前的输入。为了使分布式模型能够充分描述或预测诸如水流动力学之类的物理过程,输入数据分辨率不仅必须与实际水文功能的规模兼容,而且还必须与对结果的解释至关重要的分辨率兼容。本文回顾了中国科学技术部在一个名为“ 973”的大型多学科项目中在南京大学开展的研究的总体目标,讨论了目前的进展和存在的问题,需要进一步努力。

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