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Temporal and spatial variations of precipitation in the Jinsha River basin during 1961-2010

机译:1961-2010年金沙江流域降水的时空变化

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摘要

Knowing the variations of precipitation at the basin scale is very important to study the impacts of climate change on water resources and hydrological processes. To achieve the temporal and spatial variations of precipitation on long time scales and some extreme indicators in the Jinsha River basin, some typical precipitation indices were analysed based on daily precipitation data for 1961-2010 for the research area. The results showed that AP had a certain increasing tendency without passing the significance test, while AP in the lower reach of the basin decreased slightly. PFS had no obvious changes, while MP through a year (except rainfall in September and December) had a slight increasing tendency. In addition, AP and PFS showed obvious spatial differences, and the higher rainfall area was located in the lower basin especially in the Hengduan Mountain area. LRD and MRD increased slightly in the upper and middle regions, while they decreased slightly in the lower basin. HRD increased over most of the whole basin, but it had a decreasing tendency in the headwater region and around Dege station but did not pass the significance test. DD and CDD in one year showed similar spatial change patterns and had an obvious decreasing tendency in the upper and middle basin, while they had an obvious increasing tendency in the lower basin. CWD almost decreased over the whole basin, and decreased significantly in a small part of the lower basin. The temporal changes of the typical precipitation indices may confirm the possible increasing tendency for occurrence of drier climate and even drought events in the downstream of Jinsha River basin.
机译:了解流域规模的降水变化对于研究气候变化对水资源和水文过程的影响非常重要。为了实现金沙江流域长期降水量的时空变化和一些极端指标,基于1961-2010年该地区日降水量数据,分析了一些典型的降水指数。结果表明,未通过显着性检验的AP有一定的上升趋势,而盆地下游的AP略有下降。 PFS没有明显变化,而一年中的MP呈上升趋势(9月和12月除外)。此外,AP和PFS表现出明显的空间差异,较高的降雨区位于盆地下部,尤其是横断山区。上部和中部地区的LRD和MRD略有增加,而下部盆地则略有下降。在整个盆地的大部分区域,HRD都增加了,但在源头地区和德格站附近,HRD呈下降趋势,但未通过显着性检验。一年中的DD和CDD表现出相似的空间变化规律,上中盆地呈明显下降趋势,下盆地呈明显上升趋势。在整个盆地中,CWD几乎下降,而在下部盆地的一小部分中,CWD显着下降。典型降水指数的时间变化可能证实金沙江流域下游出现更干燥气候甚至干旱事件的可能增加趋势。

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  • 来源
  • 会议地点 Guangzhou(CN)
  • 作者单位

    State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, Institute of Water Resources of Hydropower Research, Beijing 100038, China,School of Hydropower Information Engineering, Huazhong University of Science and Technology, Wuhan 430074, China;

    School of Hydropower Information Engineering, Huazhong University of Science and Technology, Wuhan 430074, China;

    School of Hydropower Information Engineering, Huazhong University of Science and Technology, Wuhan 430074, China;

    School of Hydropower Information Engineering, Huazhong University of Science and Technology, Wuhan 430074, China;

    National Climate Center, China Meteorological Administration, Beijing 100081, China;

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

    precipitation indices; temporal and spatial variations; Jinsha River basin;

    机译:降水指数时空变化;金沙江流域;

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