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Future changes in precipitation and water resources for Kanto Region in Japan after application of pseudo global warming method and dynamical downscaling

机译:应用伪全球变暖方法和动态降尺度后日本关东地区降水和水资源的未来变化

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Highlights ? More dry years around Kanto Region in Japan in future climate. ? Lower relative humidity and more stable stratification can cause low future rainfall. ? More frequent small precipitation events in future climate. ? No significant tendency in variation of mean annual precipitation. ? Increasing heavy rainfall frequency can cause difficult water resources management. Abstract Study region The Kanto region, Japan. Study focus Detailed assessment of present and future climate conditions and their effects on water resources in the Kanto region of Japan using a modified pseudo global warming dynamical downscaling method with a numerical weather prediction model. New hydrological insights In future climate conditions, results on the change in annual precipitation are scattered, with significant variations in mean annual precipitation and the standard deviation in very limited areas. In contrast, minimum annual precipitation is found to decrease and years with low rainfall to be more frequent. During the drier summer season, the minimum accumulated rainfall is expected to become smaller across a wide region in the future. In addition, frequency distributions of future daily precipitation show a decrease of weak precipitation and an increase of heavy precipitation. Such variations are unfavorable for water recharge and indicate that water resources management will become increasingly difficult in the future because of global warming. The lower rainfall conditions are due to the lower relative humidity, more frequent stable stratifications and sub-synoptic atmospheric conditions leading to higher-pressure anomalies around Japan.
机译:强调 ?在未来的气候下,日本关东地区将出现更干旱的年份。 ?较低的相对湿度和更稳定的分层可能会导致未来降雨减少。 ?在未来的气候中,小降水事件更加频繁。 ?年平均降水量变化无明显趋势。 ?大雨频率增加会导致水资源管理困难。摘要研究地区日本关东地区。研究重点使用改进的伪全球变暖动态降尺度方法和数值天气预报模型,对日本关东地区当前和未来的气候条件及其对水资源的影响进行详细评估。新的水文见解在未来的气候条件下,年降水量变化的结果是分散的,年平均降水量和标准偏差在非常有限的区域内有很大变化。相反,发现最低年降水量减少,而降水量少的年份更为频繁。在夏季较干燥的季节,预计将来在大范围地区的最小累积降雨量将变小。另外,未来日降水的频率分布显示弱降水减少,强降水增加。这种变化不利于补给水,并且表明由于全球变暖,未来水资源管理将变得越来越困难。较低的降雨条件是由于较低的相对湿度,更频繁的稳定分层和亚热带天气条件导致日本各地的高压异常。

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