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首页> 外文期刊>Hydrology and Earth System Sciences >Geostatistical assessment of warm-season precipitation observations in Korea based on the composite precipitation and satellite water vapor data
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Geostatistical assessment of warm-season precipitation observations in Korea based on the composite precipitation and satellite water vapor data

机译:基于复合沉淀和卫星水蒸气数据的韩国暖季降水观测的地质统计学评价

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Among the meteorological disasters, heavy rain-falls cause the second largest damage in Korea, following typhoons. To manage the potential disasters due to heavy rainfalls, understanding the observational characteristics of precipitation is of utmost importance. In this study, we investigate the spatial and temporal characteristics of warmseason precipitation in Korea, according to the precipitation types, by conducting the geostatistical analyses such as an autocorrelogram, Moran's I and general G on the composite (radar + station) precipitation data. The e-folding distance of precipitation ranges from 15 to 35 km, depending on the spatial distribution, rather than intensity, of precipitation, whereas the e-folding time ranges from 1 to 2 h. The directional analyses revealed that the warm-season precipitation systems in Korea, especially those with a high precipitation amount, have high spatial autocorrelations in the southwest-northeast and west-east directions, in association with the frontal rainfalls, convection bands, etc. Furthermore, the cluster versus dispersion patterns and the hot versus cold spots are analyzed through Moran's I and general G, respectively. Water vapor, represented by the brightness temperature, from three Himawari-8 water vapor bands also shows similar characteristics with precipitation but with strong spatial correlation over a much longer distance (similar to 100 km), possibly due to the continuity of water vapor. We found that, under the e-folding-based standard, the current observation network of Korea is sufficient to capture the characteristics of most precipitation systems; however, under a strict stan-dard (e.g., autocorrelation of 0.6), a higher-resolution observation network is essentially required - especially in local areas with frequent heavy rainfalls - depending on the directional features of precipitation systems. Establishing such an observation network based on the characteristics of precipitation enables us to improve
机译:在气象灾害中,大雨下降导致韩国后的第二大损害,后来。为了管理潜在的灾害因降雨而导致的潜在灾害,了解降水的观察特性至关重要。在这项研究中,根据沉淀类型,调查韩国的最终降水量的空间和时间特征,通过进行自动化图,莫兰的I和一般g在复合(雷达+站)降水数据上进行地统计学分析。降水的电子折叠距离范围为15至35 km,根据空间分布,而不是沉淀,而不是强度,而e折叠时间为1至2小时。定向分析显示,韩国的暖季降水系统,尤其是降水量高,在西南部和西部方向上具有高空间自相关,与前部降雨,对流乐队等相关,通过Moran的I和General G分析集群与色散模式和热与冷点。由亮度温度表示的水蒸气,来自三个Himawari-8水蒸气带也显示出类似的沉淀特性,但在更长的距离(类似于100km)的情况下具有强烈的空间相关性,可能是由于水蒸气的连续性。我们发现,在基于电子折叠的标准下,韩国的当前观察网络足以捕获大多数降水系统的特性;然而,在一个严格的斯坦 - DARD(例如,0.6的自相关)下,基本上是一种更高分辨率的观察网络 - 特别是在频繁降雨的局部区域 - 取决于降水系统的方向特征。根据降水特性建立这样的观察网络,使我们能够改进

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