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Long-term Changes in Japanese Extreme Precipitation Analyzed with APHRO_JP_EX

机译:APHRO_JP_EX分析日本极端降水的长期变化

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The authors constructed a dataset of historical extreme precipitation indices in Japan named APHRO_JP_EX. This dataset contains more than 40 annual indices derived from daily precipitation. Although the spatial coverage is limited to the land of Japan, the uniqueness of these data with their long period (1900-2009) and high resolution (0.05 x 0.05 degrees) is useful not only for climate research but also for application to studies such as risk assessment of hydrological disasters. Using this dataset, we analyzed trends and annual variations of these indices to quantify the effects of global warming on local extreme precipitation in Japan. The number of wet days has significantly decreased all over Japan, especially in the northeastern part, where about 20 wet days per year have been lost during the past century. The annual mean precipitation has slightly decreased in most regions. Looking at the regional average of all of Japan, increased heavy precipitation intensity is distinct. The local changes in heavy precipitation are larger in the western part; however, they are not significant in many areas due to large annual variations. When the former and the latter halves of the 20th century are compared, increases in the annual variations of heavy precipitation indices are remarkable in the latter period. While indices of wet spells and dry spells show clear regionality in their trends, wet-spell indices have been decreasing on the Japan Sea side and dry-spell indices have been increasing on the Pacific Ocean side, though both results indicate a progression of meteorological dryness. After the beginning of the 20th century, in which surface temperatures were rising, precipitation in Japan has become more extreme overall; however, we found regional differences in these signals.
机译:作者构建了一个日本历史极端降水指数数据集,命名为APHRO_JP_EX。该数据集包含来自每日降水的40多个年度指数。尽管空间覆盖范围仅限于日本土地,但这些数据的长期(1900-2009年)和高分辨率(0.05 x 0.05度)的独特性不仅可用于气候研究,而且可用于诸如水文灾害风险评估。使用此数据集,我们分析了这些指数的趋势和年度变化,以量化全球变暖对日本局部极端降水的影响。在整个日本,尤其是在东北部地区,整个日本的湿天数已大大减少,在过去的一个世纪中,东北地区每年大约损失20天的湿天。在大多数地区,年平均降水量略有下降。从全日本的地区平均值来看,强降水强度的增加是明显的。西部地区强降水的局部变化较大。但是,由于每年变化很大,它们在许多领域并不重要。当比较20世纪的前半部分和后半部分时,后期的强降水指数年变化显着增加。尽管湿法和干法指数的趋势显示出明显的区域性,但日本海侧的湿法指数一直在下降,而太平洋侧的干法指数却一直在增加,尽管这两个结果均表明气象干旱的发展。 20世纪初,由于地表温度上升,日本的降水总体上变得更加极端。但是,我们发现这些信号存在地区差异。

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