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Spatiotemporal trends of temperature and precipitation extremes across contrasting climatic zones of China during 1956-2015

机译:1956 - 2015年中国对比度气候区的温度和降水极值时空趋势

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摘要

Spatiotemporal changes of temperature and precipitation extremes from 1956 to 2015 were analyzed at 200 representative weather stations evenly distributed in the temperate continental zone (TCZ), temperate monsoon zone (TMZ), mountain plateau zone (MPZ), and (sub) tropical monsoon zone (SMZ) of China, using 16 extreme temperature and 11 extreme precipitation indexes. The results showed that warm days (TX90p) and warm nights (TN90p) increased significantly, while cool days (TX10p) and cool nights (TN10p) decreased significantly in the whole China. Overall increasing trends were found for maximum and minimum daily maximum temperature (TXx and TXn) and maximum and minimum daily minimum temperature (TNx and TNn). Warm indexes, including summer days (SU25), tropical nights (TR20), warm spell duration indicator (WSDI), and growing season length (GSL), showed increasing trends, whereas cold indexes such as frost days (FD0), ice days (ID0), cold spell duration indicator (CSDI), and diurnal temperature range (DTR) showed decreasing trends. These extreme temperature indexes exhibited high correlations with mean air temperature. MPZ exhibited the most remarkable change magnitudes among the four zones, while the smallest changes occurred in SMZ. An accelerating warming trend was particularly observed since 1986. Nationally, only daily rainfall intensity (SDII) showed significantly increasing trends, while the increasing trends of other precipitation indexes were not significant. Apart from consecutive wet days (CWD), changes of precipitation extremes presented increasing trends. PRCPTOT and R10mm exhibited the highest correlation coefficient across contrasting climatic zones. Regionally averaged precipitation totals were decreasing in TMZ during 1956-1985, but increasing trends were identified after 1985. The upward tendency of precipitation totals in MPZ and the west part of TCZ may alleviate the pressure of water shortage in arid and semi-arid regions of China, but the upward trend in SMZ, especially in the coastal areas of southeastern China, may aggravate the risk of flood-induced disasters in these regions.
机译:从1956年到2015年的时间变化,在温带大陆区(TCZ),温带季风区(TMZ),山地平原区(MPZ)和(亚)热带季风区(Sub)热带季风区的200个代表性的天气站,分析了2056年至2015年的温度和降水极值的极端变化(SMZ)中国,使用16个极端温度和11个极端降水指标。结果表明,温暖的日子(TX90P)和温暖的夜晚(TN90P)显着增加,而整个中国的凉爽日子(TX10P)和凉爽的夜晚(TN10P)显着下降。总体上升趋势是最大和最小每日最高温度(TXX和TXN)和最大和最小每日最低温度(TNX和TNN)的最大值和最小值的趋势。温暖的指数,包括夏日(SU25),热带夜晚(TR20),温暖的法术持续时间指示器(WSDI)和生长季节长度(GSL)表现出越来越大的趋势,而冷指数如霜冻日(FD0),冰天( ID0),冷法术持续时间指示符(CSDI)和昼夜温度范围(DTR)显示出降低趋势。这些极端温度指数表现出与平均空气温度的高相关性。 MPZ在四个区域中表现出最显着的变化幅度,而SMZ发生的最小变化。自1986年以来特别观察到加速变暖趋势。国家,只有日常降雨强度(SDII)显示出显着增加的趋势,而其他降水指标的增加趋势并不显着。除了连续潮湿的日子(CWD)外,极端降水的变化提高了趋势。 PRCPTOT和R10MM横跨对比度气候区的相关系数最高。在1956年至1985年期间,TMZ的区域平均降水量下降,但在1985年之后确定了趋势的增加。MPZ中降水总量的上升趋势和TCZ的西部趋势可能会缓解干旱和半干旱地区的水资源短缺压力中国,但SMZ的上升趋势,特别是在中国东南部的沿海地区,可能会加剧这些地区洪水引起的灾害的风险。

著录项

  • 来源
    《Theoretical and applied climatology》 |2019年第4期|1877-1897|共21页
  • 作者单位

    Northwest A&F Univ Minist Educ Key Lab Agr Soil & Water Engn Arid & Semiarid Are Yangling 712100 Shaanxi Peoples R China;

    Northwest A&F Univ Minist Educ Key Lab Agr Soil & Water Engn Arid & Semiarid Are Yangling 712100 Shaanxi Peoples R China|Northwest A&F Univ Inst Water Saving Agr Arid Areas China Yangling 712100 Shaanxi Peoples R China|Northwest A&F Univ Coll Water Resources & Architectural Engn Yangling 712100 Shaanxi Peoples R China;

    Northwest A&F Univ Minist Educ Key Lab Agr Soil & Water Engn Arid & Semiarid Are Yangling 712100 Shaanxi Peoples R China|Northwest A&F Univ Inst Water Saving Agr Arid Areas China Yangling 712100 Shaanxi Peoples R China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Global warming; Temperature extremes; Precipitation extremes; RClimdex; Mann-Kendall test;

    机译:全球变暖;温度极端;降低极端;Rclimdex;Mann-Kendall测试;

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