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首页> 外文期刊>Mountain Research & Development >Spatial Downscaling of Monthly TRMM Precipitation Based on EVI and Other Geospatial Variables Over the Tibetan Plateau From 2001 to 2012
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Spatial Downscaling of Monthly TRMM Precipitation Based on EVI and Other Geospatial Variables Over the Tibetan Plateau From 2001 to 2012

机译:基于EVI和其他地理空间变量的青藏高原2001年至2012年月度TRMM降水的空间缩减

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Abstract Recent developments in hydrological modeling and biomass retrieval in complex mountain areas have heightened the need for accurate precipitation data at high spatial resolution. The Tropical Rainfall Measuring Mission (TRMM) provides rainfall estimates for certain climate models in mountain ranges where rain gauges are lacking. TRMM precipitation estimates, however, inherently have large uncertainties because of their coarse spatial resolution. In this study, we investigate a statistical downscaling calibration procedure to derive high-spatial-resolution (1-km) precipitation maps for the Tibetan Plateau using the satellite-based data set Enhanced Vegetation Index (EVI) from the Moderate Resolution Imaging Spectroradiometer, a digital elevation model from the Shuttle Radar Topography Mission, and the TRMM 3B43 product. Spatial downscaling from 0.25° to 1 km was achieved by using the nonparametric statistic relationships between precipitation and EVI, altitude, slope, aspect, latitude, and longitude. An additive method was used to calibrate the downscaled precipitation data. The best 1-km resolution annual precipitation data for 2001–2012 over the Tibetan Plateau were generated through downscaling and additive calibration for most cases. The results show that the method improves the accuracy of rainfall estimates. Monthly 1-km precipitation data were also obtained by disaggregating 1-km annual downscaled estimates with monthly fractions of annual total precipitation. Monthly precipitation predictions are in good agreement with rain gauge data. The calibration of the monthly product with rain gauge data significantly reduced the bias value. Overall we conclude that the methodology is useful for areas with varied climate conditions and complex topography. These results have practical implications for calculating hydrological balances, mapping aboveground biomass, and assessing regional climate change.
机译:摘要复杂山区水文模拟和生物量获取的最新发展迫切需要高空间分辨率的准确降水数据。热带雨量测量任务(TRMM)为缺乏雨量计的山脉的某些气候模型提供了雨量估算。但是,TRMM降水估算由于其粗糙的空间分辨率而固有地具有较大的不确定性。在这项研究中,我们研究了一种统计缩减校准程序,该程序使用中分辨率成像光谱仪(ADS)基于卫星的数据集增强植被指数(EVI)得出青藏高原的高空间分辨率(1公里)降水图。航天飞机雷达地形任务的数字高程模型和TRMM 3B43产品。通过使用降水与EVI,海拔,坡度,纵横比,纬度和经度之间的非参数统计关系,可以实现从0.25°到1 km的空间缩小。使用加法来校准降尺度的降水数据。在大多数情况下,通过缩小尺度和累加标定可以得出青藏高原2001-2012年最佳的1 km分辨率年降水量数据。结果表明,该方法提高了降雨估算的准确性。通过将1 km的年度缩水估计值与年度总降水量的每月分数进行分解,也可以获得1 km的月降水量数据。月降水量预测与雨量计数据吻合良好。使用雨量计数据对月度产品进行校准大大降低了偏差值。总的来说,我们得出的结论是,该方法对于气候条件变化和地形复杂的地区很有用。这些结果对计算水文平衡,绘制地上生物量以及评估区域气候变化具有实际意义。

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