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Effects of Land Surface Temperature on the Frequency of Convective Precipitation in the Tokyo Area

机译:东京地区地面温度对对流降水频率的影响

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This study uses statistical evaluation by correlation analysis to examine the effects of thermal environment on the frequency of convective precipitation in the Greater Tokyo Area between 12:00 and 18:00 on summer days from 1997 to 2006. To extract the frequency of convective precipitation we used Automated Meteorological Data Acquisition System radar data to obtain detailed rainfall distribution maps, and to extract the urban thermal environment we used surface temperature data from a National Oceanic and Atmospheric Administration weather satellite. Results were a coefficient of determination of 0.01, indicating no clear relation between surface temperature and convective rain frequency in the study area. Examining the convective rain frequency distribution map in conjunction with an elevation map of the area indicates that higher elevation is a better predictor of increased frequency of convective rainfall than is surface temperature. Because this indicates that orographic precipitation has a large influence in the study area, we used an elevation map to exclude hilly and mountainous regions, regions bordering flat areas (under the assumption that wind could easily move orographic precipitation to such areas), and regions containing marine areas. Doing so resulted in a coefficient of determination of 0.38, a clear signal that differences in the thermal environment in the Greater Tokyo Area have an effect on the frequency of convective precipitation. We next focused on metropolitan Tokyo, the most developed part of the region and the part experiencing the most frequent occurrences of convective precipitation, and we performed correlation analysis considering parameters related to buildings. Results indicate that orographic precipitation has a strong influence in metropolitan Tokyo as well, so we excluded those areas that were excluded from the Greater Tokyo Area analysis and again performed correlation analysis. However, we found no clear relation of convective precipitation frequency with surface temperature or building parameters.
机译:本研究采用相关分析进行统计评估,以检验1997年至2006年夏季热环境对大东京地区12:00至18:00期间对流降水频率的影响。我们使用了自动气象数据采集系统的雷达数据来获得详细的降雨分布图,并使用美国国家海洋与大气管理局气象卫星的地表温度数据提取了城市的热环境。结果的确定系数为0.01,表明研究区域的表面温度和对流雨频率之间没有明确的关系。对流降雨频率分布图与该地区的高程图一起检查表明,高海拔比表面温度更好地预测了对流降雨频率的增加。因为这表明地形降水对研究区域影响很大,所以我们使用了海拔图来排除丘陵和山区,与平坦区域接壤的区域(在假定风很容易将地形降水移动到此类区域的假设下)以及海洋区域。这样做得出的确定系数为0.38,这清楚地表明大东京地区的热环境差异会对对流降水的频率产生影响。接下来,我们将重点放在东京都会区,该地区最发达的部分以及对流降水发生最频繁的部分,然后考虑与建筑物相关的参数进行相关分析。结果表明,地形降水对东京都会区也有很强的影响,因此我们排除了大东京地区分析中排除的那些区域,然后再次进行了相关分析。但是,我们发现对流降水频率与地表温度或建筑物参数之间没有明确的关系。

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