首页> 外文会议>Remote Sensing and Hydrology Symposium >Temporal and spatial variations of precipitation in the Jinsha River basin during 1961-2010
【24h】

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

机译:1961 - 2010年锦沙河流域降水的时间和空间变化

获取原文

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:在流域尺度知道降水的变化就是研究对水资源和水文过程与气候变化的影响非常重要。为了实现降水对长时间尺度金沙江流域的时间和空间变化和一些极端的指标,一些典型的降水指数是基于对1961年至2010年为研究区域逐日降水资料进行分析。结果表明,AP具有一定的上升趋势没有通过显着性检验,而AP,而下游河段流域略有下降。 PFS无明显变化,而MP经过一年(除了在九月和十二月降雨)有轻微上升趋势。此外,AP和PFS表现出明显的空间差异,以及更高的降水区位于下游流域尤其是在横断山区。 LRD和MRD在上部和中部区域略有增加,而它们在较低的盆略有下降。 HRD增加了最全流域的,但它在源区及周边德格站有下降趋势,但没有通过显着性检验。 DD和CDD在一年中表现出相似的空间变化规律,并曾在上部和中部盆地明显的下降趋势,而他们在下游流域明显的上升趋势。 CWD在整个盆地几乎降低,并且在较低的盆地的一小部分显著降低。典型的降水指数随时间的变化可以确认干燥的气候和金沙江流域下游连旱事件的发生可能增加的趋势。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号