首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Characterizing the surface radiation budget over the Tibetan Plateau with ground-measured, reanalysis, and remote sensing data sets: 1. Methodology
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Characterizing the surface radiation budget over the Tibetan Plateau with ground-measured, reanalysis, and remote sensing data sets: 1. Methodology

机译:利用地面测量,重新分析和遥感数据集,表征青藏高原的地表辐射收支:1.方法论

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The surface radiation budget (SRB) over the Tibetan Plateau (TP) greatly influences local climate, climate extremes (e.g., drought, flood) in China, and the East Asian monsoon. However, current estimates of SRB from models and satellite data are subject to large errors, and ground-measured data sets within this region are rather limited over the TP. Our objective is to determine the SRB over the TP by integrating information from three sources: (1) four ground-measured data sets from AsiaFlux, ChinaFLUX, GAME/Tibet, and CAMP/Tibet; (2) four reanalysis data sets from Climate Forecast System Reanalysis, Modern-Era Retrospective Analysis for Research and Applications, ERA-Interim, and Japanese 25-year Reanalysis; and (3) two remote sensing data sets, Global Energy and Water Cycle Experiment Surface Radiation Budget and International Satellite Cloud Climatology Project FD. This study, the first of a two-paper series, presents the methodology. Individual radiation components of reanalysis and remote sensing data set were first validated using ground-measured data from 1997 to 2007; then, a linear regression method was applied to generate the fused data from July 1983 to December 2007. The cross-validation results indicate that the monthly mean root-mean-square errors (RMSEs) of fused downward shortwave irradiance and albedo are 15.1 W m~(-2) and 0.05, respectively; the RMSEs of the downward and upward longwave fluxes are 13.3 and 8.4 W m~(-2), respectively; and the RMSE of all-wave net radiation is as low as 18.9 W m~(-2). Compared to nine sites with long-term observation of downward shortwave irradiance, the fused data represent the decadal variations with higher correlation than using individual products, suggesting the potential for application of the fused data sets in climatic and environmental research. Key Points The surface radiation budget over the Tibetan Plateau is validatedA multiple linear regression method is applied to integrate multiple datasetsThe fused data insolation agreed well with that of other stations
机译:青藏高原(TP)上的地表辐射预算(SRB)极大地影响了当地的气候,中国的极端气候(例如干旱,洪水)和东亚季风。但是,根据模型和卫星数据得出的SRB的当前估算值存在较大误差,并且该区域内的地面测量数据集在TP上相当有限。我们的目标是通过整合来自三个来源的信息来确定TP上的SRB:(1)来自AsiaFlux,ChinaFLUX,GAME / Tibet和CAMP / Tibet的四个地面测量数据集; (2)来自气候预测系统再分析,研究和应用的现代时代回顾分析,ERA-Interim和日本25年再分析的四个再分析数据集; (3)两个遥感数据集,即全球能源和水循环实验表面辐射预算和国际卫星云气候学项目FD。本研究是两篇论文系列文章中的第一篇,介绍了该方法。首先使用1997年至2007年的地面测量数据对重新分析和遥感数据集的各个辐射分量进行了验证;然后,使用线性回归方法生成1983年7月至2007年12月的融合数据。交叉验证结果表明,融合的向下短波辐照度和反照率的月均方根误差(RMSE)为15.1 W m 〜(-2)和0.05;上下长波通量的RMSE分别为13.3 W和8.4 W m〜(-2)。全波净辐射的RMSE低至18.9 W m〜(-2)。与长期观察向下的短波辐照度的9个站点相比,融合数据表示年代际变化的相关性高于使用单个产品时的年代际变化,这表明融合数据集在气候和环境研究中的应用潜力。关键点验证了青藏高原的地表辐射收支平衡采用多元线性回归方法整合了多个数据集融合的数据日照与其他台站的吻合得很好

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