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Spatiotemporal analysis of precipitation trends during 1961-2010 in Hubei province, central China

机译:中国中部湖北省1961-2010年降水趋势的时空分析

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摘要

Precipitation is an important climatic parameter, and its variability severely affects regional hydrological processes and water resource management. In order to explore the changing spatial and temporal characteristics of precipitation-related indices, including precipitation amounts indices, extreme precipitation indices, and precipitation concentration indices, in Hubei province, central China during 1961-2010, several precipitation-related indices series were analyzed using the Mann-Kendall test, Pettitt test, and inverse distance weighted interpolation method in this paper. The results are as follows: (1) A clear south-north gradient is apparent in the spatial distribution of the majority of precipitation-related indices, while the distribution of other indices (i.e., CDD, PCD, and PCP) is just the opposite. Most part of Hubei province can experience mixed positive and negative trends in precipitation-related indices. (2) The majority of precipitation-related indices exhibit an increasing trend, but most of which are not significant. July has the largest positive trend, with a regional average of 14.76 mm/decade. As for extreme precipitation indices, there exist large variations in Hubei, especially in R95pTOT. Besides, no obvious trends are shown in precipitation concentration indices. (3) With the exception of consecutive dry days (CDD), most of extreme precipitation indices are strongly correlated with annual mean precipitation (AMP) in Hubei. And the extreme precipitation indices are well correlated with each other except CDD and consecutive wet days (CWD). For six precipitation-related indices (i.e., SDII, RX1day, RX5day, R95pTOT R99pTOT, and PCD), there are significant positive relationships with Northern Hemisphere Subtropical High (NHSH) but significant negative relationships with Northern Hemisphere Polar Vortex (NHPV). Furthermore, the majority of precipitation-related indices have significant negative correlations with East Asian summer monsoon index (EASMI) and South China Sea summer monsoon index (SCSSMI), and the correlation coefficient with EASMI is higher than that with SCSSMI.
机译:降水是重要的气候参数,其变化严重影响区域水文过程和水资源管理。为了探讨降水量指数,极端降水量指数和降水集中度指数等与降水有关的指数的时空变化特征,分析了1961-2010年湖北省中部与降水有关的指数系列。本文采用Mann-Kendall检验,Pettitt检验和反距离加权插值方法。结果如下:(1)大多数与降水有关的指数的空间分布上都有明显的南北梯度,而其他指数(即CDD,PCD和PCP)的分布恰好相反。湖北省大部分地区降水相关指数的正负趋势混合。 (2)大多数与降水有关的指数都呈上升趋势,但大多数并不显着。 7月份是最大的积极趋势,十年平均值为14.76毫米。至于极端降水指数,湖北尤其是R95pTOT的变化很大。此外,降水浓度指数没有明显的趋势。 (3)除连续干旱日(CDD)外,湖北大部分极端降水指数与年平均降水(AMP)密切相关。除CDD和连续湿日(CWD)外,极端降水指数之间具有很好的相关性。对于六个与降水有关的指数(即SDII,RX1day,RX5day,R95pTOT,R99pTOT和PCD),与北半球副热带高压(NHSH)有显着的正相关,而与北半球极涡(NHPV)则有显着的负相关。此外,大多数与降水有关的指数与东亚夏季风指数(EASMI)和南海夏季风指数(SCSSMI)呈显着负相关,与EASMI的相关系数高于与SCSSMI的相关系数。

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  • 来源
    《Theoretical and applied climatology》 |2016年第2期|385-399|共15页
  • 作者

    Wang Ranghui; Li Cheng;

  • 作者单位

    Nanjing Univ Informat Sci & Technol, Sch Environm Sci & Engn, Nanjing 210044, Jiangsu, Peoples R China;

    Nanjing Univ Informat Sci & Technol, Sch Geog & Remote Sensing, Nanjing 210044, Jiangsu, Peoples R China;

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  • 入库时间 2022-08-18 03:33:35

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