首页|基于风云三号G星/中分辨率光谱成像仪-降水型近红外通道数据的大气可降水量反演

基于风云三号G星/中分辨率光谱成像仪-降水型近红外通道数据的大气可降水量反演

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中分辨率光谱成像仪-降水型(MERSI-RM)是中国首颗低倾角轨道气象卫星风云三号G星(FY-3G)的主要载荷之一。FY-3G的过境时间与FY-3D和Terra等大多数极轨气象卫星存在明显差异,基于FY-3G/MERSI-RM开发的大气可降水量(PWV)数据对于天气系统等研究具有重要意义。然而,目前尚缺乏可获取的MERSI-RM PWV数据。为填补这一空白,本文面向MERSI-RM开发了一套半经验PWV反演算法。该算法首先对MERSI-RM数据和地基PWV数据进行时空匹配,继而基于东半球的匹配结果完成水汽反演模型的构建。该算法仅通过一个简单的公式就可以实现水汽反演,具有极高的反演效率。基于西半球地基数据的验证结果显示,使用半经验反演算法开发的MERSI-RM PWV数据的均方根误差和相对误差分别为0。20 cm和0。10。与基于常用的辐射传输模型算法开发的MERSI-RM PWV数据相比,使用本文提出的半经验PWV反演算法开发的MERSI-RM PWV数据,误差至少减小了 33%;与当前被广泛使用的Terra/中分辨率成像光谱仪(MODIS)官方PWV数据(MOD05)相比,误差至少减小了 65%。上述结果表明,本文面向MERSI-RM开发的PWV反演算法具有较高的反演精度。为对半经验反演算法进行更加全面的评估,并提供更多的建模方法选择,本文还测试了基于随机分配数据构建的PWV反演模型。使用地基数据的验证结果显示,基于上述两种方法构建的PWV反演模型的反演精度的差别可忽略不计。实际应用时,用户可对上述建模方法进行自由选择。
Precipitable Water Vapor Retrieval Based on Near-Infrared Channel Data from FengYun-3G Satellite/Medium Resolution Spectral Imager-Rainfall Mission
Objective The FengYun(FY)-3G satellite is China's first meteorological satellite in a low-inclination orbit,and the medium resolution spectral imager-rainfall mission(MERSI-RM)is one of its primary payloads.Due to the unique overpass times of FY-3G compared to most polar-orbiting meteorological satellites,such as FY-3D and Terra,the precipitable water vapor(PWV)data derived from FY-3G/MERSI-RM is critical for studies on weather systems and climate change.However,there is currently a lack of accessible MERSI-RM PWV data.To address this issue,we develop a semi-empirical PWV retrieval algorithm for the near-infrared(NIR)channels at 0.865 and 0.940 pm from FY-3G/MERSI-RM.Methods The relationship between the natural logarithm of the water vapor absorption transmittance(WVAT)in the NIR water vapor absorption(WVA)channel and the slant column water vapor content along the sun-earth-satellite path is closely correlated and can be expressed by a quadratic equation.The NIR PWV retrieval model for MERSI-RM is established based on this correlation.Initially,average ground-based PWV data from the Aerosol Robotic Network(AERONET)obtained within a 30-min window of satellite transit are matched with the average MERSI-RM data within a 10 km×10 km area centered on the ground stations.Subsequently,the three coefficients of the quadratic equation are solved based on these matching results,completing the construction of the MERSI-RM PWV retrieval model.To ensure that AERONET PWV data can be used both for establishing the PWV retrieval model and for the quality assessment of the retrieval results,the matching data are divided into two independent sets based on the locations of the ground stations:data from the eastern hemisphere are used to construct the MERSI-RM PWV retrieval model,while data from the western hemisphere are used to validate the MERSI-RM PWV retrieval results.Results and Discussions Validation results using ground-based data show that the root mean square error(RMSE)and relative error(RE)of MERSI-RM PWV data,developed using the semi-empirical algorithm,are 0.20 cm and 0.10,respectively.In contrast,the RMSE and RE of MERSI-RM PWV data,developed using the traditional retrieval algorithm based on a radiative transfer model,are 0.35 cm and 0.15,respectively.Meanwhile,the RMSE and RE of MODIS PWV data are 0.57 cm and 0.39,respectively.Compared to MODIS PWV data,MERSI-RM PWV data,developed based on the semi-empirical algorithm,exhibit a 65%reduction in absolute error and a 74%reduction in relative error.Given that MODIS PWV data are widely acknowledged for their high accuracy,it can be concluded that the MERSI-RM PWV data developed using the semi-empirical algorithm also exhibit high accuracy.In comparison to MERSI-RM PWV data developed using the retrieval algorithm based on a radiative transfer model,the absolute error of the MERSI-RM PWV data derived using the semi-empirical algorithm is reduced by 43%,while the relative error is reduced by 33%.The lower accuracy observed in MERSI-RM PWV data and MODIS PWV data developed based on the radiative transfer model is primarily attributed to noticeable systematic errors.In contrast,the MERSI-RM PWV data obtained using the semi-empirical algorithm do not exhibit this issue.The success of the semi-empirical algorithm is attributed to its PWV retrieval model,which is constructed based on matching results between satellite observations and ground-based data.In other words,the errors in satellite observations are considered in the retrieval model.To provide a more comprehensive evaluation of the semi-empirical algorithm and offer additional choices for model construction methods,we also assess the PWV retrieval model constructed based on randomly allocated data.Validation results based on ground-based data show that the retrieval accuracy of the model constructed using randomly allocated data is equivalent to that of the retrieval model constructed using data obtained from the eastern hemisphere.Conclusions We introduce a semi-empirical PWV retrieval algorithm tailored specifically for FY-3G/MERSI-RM.This algorithm effectively tackles the current challenge of unavailable PWV data from FY-3G satellite observations.It does not rely on complex radiative transfer models but instead utilizes a quadratic equation,resulting in remarkably efficient PWV retrieval.Compared to traditional methods based on radiative transfer models,this semi-empirical approach achieves notably higher retrieval accuracy.The errors in MERSI-RM PWV data,obtained using the algorithm,are reduced by at least 33%compared to those derived from models based on radiative transfer.Moreover,when contrasted with the widely utilized MODIS official PWV data(MOD05),this semi-empirical algorithm diminishes errors in MERSI-RM PWV data by a minimum of 65%.These results underscore the high accuracy and efficiency of the semi-empirical PWV retrieval algorithm for MERSI-RM,making it suitable for large-scale PWV data development.

remote sensing retrievalprecipitable water vaporFengYun-3G satellitemedium resolution spectral imager-rainfall mission

谢艳清、袁德帅、樊程、张立国、王田野、梁伟、肖前循、张苗苗、温渊、李云端、李正强

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上海航天技术研究院上海卫星工程研究所,上海 201109

中国科学院空天信息创新研究院,北京 100094

遥感反演 大气可降水量 风云三号G星 中分辨率光谱成像仪-降水型

国家自然科学基金民用航天技术预先研究项目国家重点研发计划国家重点研发计划遥感科学国家重点实验室开放基金

42301463D0102062022YFB39018002022YFB3901805OFSLRSS202322

2024

光学学报
中国光学学会 中国科学院上海光学精密机械研究所

光学学报

CSTPCD北大核心
影响因子:1.931
ISSN:0253-2239
年,卷(期):2024.44(12)