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Role of precipitation forcing on the uncertainty of land surface model simulated soil moisture estimates

机译:降水强迫对土地面积模型不确定性模拟土壤水分估算的作用

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Land surface processes considerably Influence the global weather and climate patterns which makes its quantification significant to scientists, hydrologists as well as policymakers alike. Considering the lack of available in-situ measurement, retrieval of the land surface fluxes mostly relies on remotely sensed satellite retrieval and through simulations from land surface models (LSMs). Hence, it is essential to quantify the uncertainties present in the output of these land surface models which are mainly due to errors in forcing data, model parameters and model structure. Precipitation is one of the key input forcing data used in LSMs. With the advancement of remote sensing techniques, multiple sources of precipitation products are made available to the user community. This study examines the effect of precipitation uncertainty in LSM simulated soil moisture. For this study, four precipitation products are used namely, Tropical Rainfall Measuring Mission (TRMM) Multi-satellite Precipitation Analysis (TMPA) 3B42RT v7, Global Data Assimilation System (GDAS), Climate Hazards Infrared Precipitation with Stations (CHIRPS) and Multi-Source Weighted-Ensemble Precipitation (MSWEP). These data products are used as meteorological forcing in Noah 3.6 LSM for the simulation of soil moisture. The uncertainty inherent in the precipitation products are examined using two approaches a) By evaluating the precipitation products against the gridded India Meteorological Department (IMD) precipitation dataset and b) By using the precipitation products for simulating soil moisture outputs. These were validated over the Indian subcontinent using validation data from the European Space Agency-Climate Change Initiative (ESA-CCI) soil moisture and Central Tibetan Plateau Soil Moisture and Temperature Monitoring Network (CTP-SMTMN) dataset for the years 2010 to 2012. The study utilizes various graphical as well as quantitative evaluation methods to determine the best performing precipitation product. Our study indicates that the simulated soil moisture forced with GDAS and MSWEP precipitation product performed consistently superior among all the other simulation outputs over India.
机译:土地面过程显着影响全球天气和气候模式,这使其对科学家,水文学家以及政策制定者相似的量化。考虑到缺乏现场测量,陆地表面通量的检索主要依赖于远程感测的卫星检索,并通过陆地表面模型(LSM)模拟。因此,必须量化这些土地表面模型输出中存在的不确定性,这主要是由于迫使数据,模型参数和模型结构中的错误。降水是LSM中使用的关键输入强制数据之一。随着遥感技术的进步,对用户社区提供了多种降水产品来源。本研究探讨了降水不确定性在LSM模拟土壤水分中的影响。对于本研究,使用四种沉淀产品即,热带降雨测量任务(TRMM)多卫星降水分析(TMPA)3B42RT V7,全球数据同化系统(GDA),气候危害红外降水与站(Chirps)和多源加权集合沉淀(MSWEP)。这些数据产品被用作诺亚3.6 LSM中的气象迫使,用于模拟土壤水分。通过使用用于模拟土壤湿度产出的降水产品来评估沉淀产品,通过评估沉淀产品来检查沉淀产品中固有的不确定性a)。这些通过欧洲空间局 - 气候变化倡议(ESA-CCI)土壤水分和中央藏高平原土壤水分和温度监测网络(CTP-SMTMN)数据集2010年至2012年的验证数据,这些验证数据经过验证。该研究利用各种图形以及定量评价方法来确定最佳的性沉淀产品。我们的研究表明,使用GDA和MSWEP沉淀产品强制模拟的土壤水分在印度的所有其他仿真输出中始终如一地进行。

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