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Changes in Extreme Precipitation Over Dry and Wet Regions of China During 1961-2014

机译:1961 - 2014年中国干湿地区极端降水的变化

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摘要

Changes in extreme precipitation differ among regions (e.g., dry and wet regions), causing different adverse effects on human life, social economy, and natural ecosystems on a warming planet. In this study, we use the 95th percentile-based threshold to define extreme precipitation. The spatiotemporal changes in extreme precipitation and temperature-extreme precipitation scaling relationship between dry and wet regions of mainland China during 1961-2014 are analyzed using two gridded data sets of precipitation and temperature observations. Extreme precipitation increased faster in dry regions (3.9% frequency and 2.8% relative intensity per decade) compared to wet regions (2.5% frequency and 2.1% relative intensity per decade) over the past 54 years. Despite the negative regression relationship between mean precipitation and temperature in wet regions, extreme precipitation has a positive relationship with temperature. The regression coefficient in relative intensity against temperature change is 6% per °C in wet regions. The frequency increases significantly (p < 0.01) faster as temperature increases in wet regions (11.1% per °C) compared with dry regions (6.9% per °C). These results suggest that precipitation extremes increase for both dry and wet regions, and faster trends are observed in dry regions. However, the same magnitude of warming causes more extreme precipitation in wet regions. Therefore, more extreme precipitation in future may raise the risk of flooding in both dry and wet regions, particularly for wet regions, due to the stronger relative intensity and faster increases against warming.
机译:极端降水的变化在地区(例如,干燥和湿地区)不同,导致对暖行星的人生,社会经济和自然生态系统产生不同的不利影响。在这项研究中,我们使用基于95百分位的阈值来定义极端降水。 1961 - 2014年中国大陆干旱地区的极端降水和温度 - 极端降水缩放关系的时空变化,采用了两个网格和温度观测分析了两种。与过去54年相比,干燥区域的极端降水量在干燥区域(每十年的相对强度为2.8%)增加(每十年2.5%和2.1%)。尽管湿地区的平均沉淀和温度之间存在负面回归关系,但极端沉淀具有与温度的阳性关系。在潮湿区域中,相对强度的回归系数在温度变化中为6%。随着干燥区域(每°C)的温度增加(每℃11.1%/℃)的温度增加,频率显着增加(P <0.01)。这些结果表明,干燥和湿地区的降水量增加,在干燥区域观察到更快的趋势。然而,相同的升温量导致湿地区的极端沉淀。因此,由于相对强度较强,更加极高的湿地,更加极端的降水可能会增加干燥和湿地区的洪水,特别是对于湿地区的风险。

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  • 作者单位

    Key Laboratory of Geographical Processes and Ecological Security in Changbai Mountains Ministry of Education School of Geographical Sciences Northeast Normal University Changchun China;

    Key Laboratory of Geographical Processes and Ecological Security in Changbai Mountains Ministry of Education School of Geographical Sciences Northeast Normal University Changchun China;

    Key Laboratory of Geographical Processes and Ecological Security in Changbai Mountains Ministry of Education School of Geographical Sciences Northeast Normal University Changchun China;

    Key Laboratory of Geographical Processes and Ecological Security in Changbai Mountains Ministry of Education School of Geographical Sciences Northeast Normal University Changchun China;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 地球物理学;
  • 关键词

    Changes; Extreme Precipitation; Wet Regions;

    机译:变化;极端降水;湿地区;

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