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首页> 外文期刊>Quaternary International >Changes in precipitation extremes over the 'Three-River Headwaters' region, hinterland of the Tibetan Plateau, during 1960-2012
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Changes in precipitation extremes over the 'Three-River Headwaters' region, hinterland of the Tibetan Plateau, during 1960-2012

机译:1960-2012年青藏高原腹地“三河源头”地区的极端降水变化

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摘要

Based on daily precipitation from 12 meteorological stations over hinterland of the Tibetan Plateau observed by the China Meteorological Administration in 1960-2012, changes in ten selected indices of precipitation extremes are investigated. The results demonstrate that very wet day precipitation, extremely wet day precipitation, simple daily intensity index, wet day precipitation, heavy precipitation days, and heavier precipitation days over the "Three-River Headwaters" region exhibit increasing trends during the study period, with wet day precipitation statistically significant. However, non-significant decreasing trends are found for other indices, including maximum 1-day precipitation, maximum 5-day precipitation, and consecutive wet days with exception of consecutive dry days. Additionally, the stations with significant variations are mainly distributed over the northern "Three-River Headwaters" region. Additionally, abrupt changes in non-significant increasing trend for R95p and R99p are observed in 2007 and 2006, respectively, and major periodic variations with periods of a 6-year and a 20-year occurring in the extreme precipitation. The contribution of extreme precipitation to total precipitation has non-significant increase in the research region. Changes in small scale atmospheric circulation indicate that the main part of the moisture over the study area is from the Indian Ocean via southwesterly wind during the summer monsoon period.
机译:根据中国气象局在1960-2012年间观测到的青藏高原腹地12个气象站的日降水量,研究了十个选定的极端降水指数的变化。结果表明,在“三河源头”地区,极湿日降水,极湿日降水,简单日强度指数,湿日降水,重降水日和较重降水日在研究期内呈增加趋势,其中日降水量具有统计学意义。但是,其他指数没有明显下降趋势,包括最大的1天降水,最大的5天降水以及连续的湿天(连续的干旱天除外)。此外,变化很大的站点主要分布在北部的“三河源头”地区。此外,分别在2007年和2006年观测到R95p和R99p的非显着增加趋势的突然变化,并且在极端降水中出现了周期为6年和20年的主要周期性变化。在研究区域,极端降水对总降水的贡献没有显着增加。小规模大气环流的变化表明,研究区的大部分水分在夏季风期间来自印度洋,通过西南风。

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  • 来源
    《Quaternary International》 |2014年第13期|105-115|共11页
  • 作者

    Liguo Cao; Shaoming Pan;

  • 作者单位

    School of Geographic and Oceanographic Sciences, Nanjing University, Nanjing 210023, China;

    School of Geographic and Oceanographic Sciences, Nanjing University, Nanjing 210023, China;

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  • 正文语种 eng
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