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首页> 外文期刊>ournal of the Meteorological Society of Japan >High Temporal Rainfall Estimations from Himawari-8 Multiband Observations Using the Random-Forest Machine-Learning Method
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High Temporal Rainfall Estimations from Himawari-8 Multiband Observations Using the Random-Forest Machine-Learning Method

机译:使用随机森林机器学习方法从Himawari-8多波段观测中估算高时间降雨

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摘要

?We introduce a novel rainfall-estimating algorithm with a random-forest machine-learning method only from Infrared (IR) observations. As training data, we use nine-band brightness temperature (BT) observations, obtained from IR radiometers, on the third-generation geostationary meteorological satellite (GEO) Himawari-8 and precipitation radar observations from the Global Precipitation Measurement core observatory. The Himawari-8 Rainfall-estimating Algorithm (HRA) enables us to estimate the rain rate with high spatial and temporal resolution (i.e., 0.04° every 10 min), covering the entire Himawari-8 observation area (i.e., 85°E-155°W, 60°S-60°N) based solely on satellite observations. We conducted a case analysis of the Kanto–Tohoku heavy rainfall event to compare HRA rainfall estimates with the near-real-time version of the Global Satellite Mapping of Precipitation (GSMaP_NRT), which combines global rainfall estimation products with microwave and IR BT observations obtained from satellites. In this case, HRA could estimate heavy rainfall from warm-type precipitating clouds. The GSMaP_NRT could not estimate heavy rainfall when microwave satellites were unavailable. Further, a statistical analysis showed that the warm-type heavy rain seen in the Asian monsoon region occurred frequently when there were small BT differences between the 6.9-μm and 7.3-μm of water vapor (WV) bands (ΔT6.9-7.3). Himawari-8 is the first GEO to include the 6.9-μm band, which is sensitive to middle-to-upper tropospheric WV. An analysis of the WV multibands' weighting functions revealed that ΔT6.9-7.3 became small when the WV amount in the middle-to-upper troposphere was small and there were optically thick clouds with the cloud top near the middle troposphere. Statistical analyses during boreal summer (August and September 2015 and July 2016) and boreal winter (December 2015 and January and February 2016) indicate that HRA has higher estimation accuracy for heavy rain from warm-type precipitating clouds than a conventional rain estimation method based on only one IR band.
机译:我们引入了一种新颖的降雨估算算法,该算法仅从红外(IR)观测值中使用随机森林机器学习方法。作为训练数据,我们使用从IR辐射计获得的第三波段地球静止气象卫星(GEO)Himawari-8上的九波段亮度温度(BT)观测值和全球降水测量核心天文台的降水雷达观测值。 Himawari-8降雨量估算算法(HRA)使我们能够以高时空分辨率(即每10分钟0.04°)估算降雨率,覆盖整个Himawari-8观测区域(即85°E-155) °W,60°S-60°N)仅基于卫星观测。我们对关东至东北的强降雨事件进行了案例分析,以比较HRA的降雨估计值与近实时版本的全球降水图(GSMaP_NRT),该模型将全球降雨估计产品与获得的微波和IR BT观测值结合在一起从卫星。在这种情况下,HRA可以估计来自暖型降水云的强降雨。当微波卫星不可用时,GSMaP_NRT无法估计暴雨。此外,统计分析表明,当在6.9μm和7.3μm的水汽(WV)波段之间的BT差异较小时,在亚洲季风区看到的暖型大雨频繁发生(ΔT6.9-7.3) 。 Himawari-8是第一个包含6.9μm波段的GEO,该波段对中高层对流层WV敏感。对WV多频带加权函数的分析表明,当对流层中上层对流层的WV量较小时,ΔT6.9-7.3变小,并且在对流层中层附近存在光学上厚的云层,云顶。北方夏季(2015年8月和2015年9月以及2016年7月)和北方冬季(2015年12月和2016年1月和2016年2月)的统计分析表明,与基于传统降水量估算方法的HRA相比,HRA对暖雨云的暴雨估算精度更高。只有一个红外波段。

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