遥感降水数据空间降尺度及干旱时空监测
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张寒博(1996—), 男, 汉族, 河南开封人, 硕士研究生, 主要从事遥感原理与应用研究。E-mail: 2120191109@glut.edu.cn

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S423.3

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广西八桂学者专项(GUTQDJJ2017096);国家自然科学基金项目(42061059);广西自然科学基金项目(2020GXNSFBA297160);广西空间信息与测绘重点实验室项目(191851016);桂林理工大学科研启动基金项目(GUTQDJJ2019046, GUTQDJJ2019172)


Spatial Downscaling of Remote Sensing Precipitation Data and Spatiotemporal Monitoring of Drought
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    摘要:

    在全球气候变暖的背景下, 干旱灾害日趋频发。为全面精细研究华中地区降水的时空变化, 结合水汽(PWV)、增强型植被指数(EVI)等数据, 基于地理加权回归模型, 结合克里金插值分别对2010—2019年的GPM IMERG和TRMM 3B43数据进行空间降尺度, 并利用区域内53个气象站数据进行精度评价。对优选的降尺度数据采用变异系数法、Theil-Sen Median趋势分析耦合Mann-Kendall显著性检验方法及Hurst指数法, 分析了华中地区的降水时空变化特征及其可持续性特征, 并对未来降水趋势进行预测, 最后构建归一化降水距平百分率(NPA)、标准化降水蒸散指数(SPEI12)来实现研究区的干旱时空监测。结果表明: 降尺度处理后降水细节增强, 能有效改善原始数据的高估现象, GPM数据降尺度数据比TRMM降尺度数据更接近实测数据; 近10年华中地区降水时空分布差异较大, 降水较高波动变化和高波动变化共占全区69.21%;10年间降水变化以非显著变化为主, 其中, 轻微增加地区占全区54.88%, 轻微减小地区占全区40.41%;10年间降水变化趋势以弱(27.33%)、中(34.93%)持续性为主; 华中地区降水未来趋势以持续增加为主, 主要分布在区域北部, 未来趋势无法确定的地区占全区21.63%, 主要集中在湖南; 华中地区NPA空间分布有很大差异性, 整体上处于无旱、轻旱灾害状态, NPA与SPEI12有较好的相关性, 且所有年份均通过了0.05显著性检验, 在一定程度上能反映华中地区的干旱情况。

    Abstract:

    In the context of global warming, drought disasters are becoming more frequent. In order to comprehensively and finely study the temporal and spatial changes of precipitation in central China from 2010 to 2019, this study combined remote sensing data of water vapor (PWV), enhanced vegetation index (EVI), elevation, slope, and aspect, based on the geographically weighted regression model combined with Kriging Interpolation (GWRK), the GPM IMERG and TRMM 3B43 data from 2010 to 2019 were spatially downscaled, and the data of 53 meteorological stations in the area were used for accuracy evaluation. For the optimized downscaling data, the coefficient of variation method, Theil-Sen Median trend analysis coupled with the Mann-Kendall significance test method and the Hurst index method were used to analyze the temporal and spatial characteristics of precipitation changes and sustainability characteristics in Central China, and future precipitation trends were predicted. Finally, the NPA (Normalized Precipitation Anomaly) and the SPEI12 (standardized precipitation evapotranspiration indices) were constructed to realize the spatio-temporal monitoring of drought in the study area. The research results showed that the details of the precipitation data are enhanced after downscaling, and the overestimation of the original data can be effectively improved. The downscaling data of GPM data was closer to the measured data than the downscaling data of TRMM. In the past 10 years, the temporal and spatial distribution of precipitation in Central China were quite different, with high fluctuations and high fluctuations in precipitation accounting for 69.21% of the entire region. The precipitation changes during the 10 years were dominated by non-significant changes, of which slightly increased areas accounted for 54.88% of the entire region, and slightly decreased areas accounted for 40.41% of the entire region. The future trend of precipitation in Central China was dominated by a continuous increase, mainly distributed in the northern part of the region. Areas with uncertain future trends accounted for 21.63% of the entire region, mainly concentrated in Hunan. There were great differences in the spatial distribution of NPA in Central China. As a whole, it was in a state of drought-free and light-drought disasters. NPA and SPEI12 had a relatively good correlation, and all years had passed the 0.05 significance test, which can be to a certain extent Reflect the drought in Central China. Downscaling data can reflect the temporal and spatial dynamic changes of precipitation in more detail, and is of great significance for accurate monitoring of drought and flood disasters, guiding agricultural production and promoting sustainable economic development.

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张寒博, 窦世卿, 温颖, 徐勇, 张楠, 苗林林.遥感降水数据空间降尺度及干旱时空监测[J].水土保持学报,2022,36(1):153~160

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  • 收稿日期:2021-07-06
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  • 在线发布日期: 2022-01-25
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