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Improvement of the Noah land surface model for warm season processes: evaluation of water and energy flux simulation

机译:诺亚陆面模型在暖季过程中的改进:水和能量通量模拟的评估

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The Noah model is a land surface model of the National Centers for Environmental Prediction. It has been widely used in regional coupled weather and climate models (i.e. Weather Research and Forecasting Model, Eta Mesoscale Model) and global coupled weather and climate models (i.e. National Centers for Environmental Prediction Global Forecast System, Climate Forecast System). Therefore, its continued improvement and development are keys to enhancing our weather and climate forecast ability and water and energy flux simulation accuracy. North American Land Data Assimilation System phase 1 (NLDAS-1) experiments indicated that the Noah model exhibited substantial bias in latent heat flux, total runoff and land skin temperature during the warm season, and such bias can significantly affect coupled weather and climate models. This paper presents a study to improve the Noah model by adding model parameterization processes such as including seasonal factor on leaf area index and root distribution and selecting optimal model parameters. We compared simulated latent heat flux, mean annual runoff and land skin temperature from the Noah control and test versions with measured latent heat flux, land surface skin temperature, mean annual runoff and satellite-retrieved land surface skin temperature. The results show that the test version significantly reduces biases in latent heat, total runoff and land skin temperature simulation. The test version has been used for the NLDAS phase 2 (NLDAS-2) to produce 30-year water flux, energy flux and state variable products to support the US drought monitor of National Integrated Drought Information System. Copyright © 2012 John Wiley & Sons, Ltd.
机译:Noah模型是美国国家环境预测中心的地表模型。它已广泛用于区域耦合的天气和气候模型(即天气研究和预报模型,Eta中尺度模型)和全球耦合的天气和气候模型(即国家环境预测中心全球预报系统,气候预报系统)。因此,它的持续改进和发展是增强我们的天气预报和气候预测能力以及水和能量通量模拟精度的关键。北美土地数据同化系统第1阶段(NLDAS-1)实验表明,诺亚模型在温暖季节表现出潜热通量,总径流量和土地表皮温度的显着偏差,并且这种偏差会显着影响天气和气候耦合模型。本文提出了一项通过添加模型参数化过程(例如在叶面积指数和根系分布上包括季节性因素)并选择最佳模型参数来改进Noah模型的研究。我们将来自Noah对照和测试版本的模拟潜热通量,年平均径流量和陆地表皮温度与测得的潜热通量,陆地表面表皮温度,年平均径流量和卫星获取的地面表皮温度进行了比较。结果表明,该测试版本显着降低了潜热,总径流量和陆地皮肤温度模拟中的偏差。该测试版本已用于NLDAS第二阶段(NLDAS-2),以产生30年的水通量,能量通量和状态变量产品,以支持美国国家干旱综合信息系统的干旱监测。版权所有©2012 John Wiley&Sons,Ltd.

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