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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Development of a hydrometeorological forcing data set for global soil moisture estimation
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Development of a hydrometeorological forcing data set for global soil moisture estimation

机译:开发用于全球土壤湿度估算的水文气象强迫数据集

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Off-line land surface modeling simulations require accurate meteorological forcing with consistent spatial and temporal resolutions. Although reanalysis products present an attractive data source for these types of applications, bias to many of the reanalysis fields limits their use for hydrological modeling. In this study, we develop a global 0.5 degrees forcing data sets for the time period 1979-1993 on a 6-hourly time step through application of a bias correction scheme to reanalysis products. We then use this forcing data to drive a land surface model for global estimation of soil moisture and other hydrological states and fluxes. The simulated soil moisture estimates are compared to in situ measurements, satellite observations and to a modeled data set of root zone soil moisture produced within a separate land surface model, using a different data set of hydrometeorological forcing. In general, there is good agreement between anomalies in modeled and observed (in situ) root zone soil moisture. Similarly, for the surface soil wetness state, modeled estimates and satellite observations are in general statistical agreement; however, correlations decline with increasing vegetation amount. Comparisons to a modeled data set of soil moisture also demonstrates that both simulations present estimates that are well correlated for the soil moisture in the anomaly time series, despite being derived from different land surface models, using different data sources for meteorological forcing, and with different specifications of the land surfaces properties. Copyright (c) 2005 Royal Meteorological Society.
机译:离线陆面建模模拟需要精确的气象强迫和一致的时空分辨率。尽管再分析产品为这些类型的应用提供了有吸引力的数据源,但对许多再分析领域的偏见限制了它们在水文建模中的使用。在这项研究中,我们通过将偏差校正方案应用于重新分析产品,在6小时的时间步长上开发了1979-1993年时间段的全球0.5度强迫数据集。然后,我们使用此强迫数据来驱动土地表面模型,以对土壤湿度以及其他水文状态和通量进行全局估计。使用不同的水文气象强迫数据集,将模拟的土壤水分估算值与原位测量,卫星观测结果以及与在单独的土地表面模型中产生的根区土壤水分的模型化数据集进行比较。通常,在模拟和观察到的(原位)根区土壤湿度之间存在良好的一致性。同样,对于表层土壤湿度状态,模型估计和卫星观测值在总体上具有统计一致性;但是,相关性随着植被数量的增加而下降。与土壤水分建模数据集的比较还表明,尽管来自不同的土地表面模型,使用不同的数据源进行气象强迫,并且使用不同的数据,但两种模拟均给出了与异常时间序列中的土壤水分良好相关的估计值陆地表面属性的规范。版权所有(c)2005皇家气象学会。

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