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Analysis of precipitation characteristics on the loess plateau between 1965 and 2014, based on high-density gauge observations

机译:基于高密度计观测资料的1965至2014年黄土高原降水特征分析

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摘要

The Loess Plateau is ecologically vulnerable and one of the most severely eroded areas in China. In this study, we used daily precipitation data from 170 meteorological stations for the period 1965 to 2014 to systematically analyze the spatiotemporal variability of annual precipitation on the plateau, and to determine the dominant factors influencing changes in annual precipitation. The average annual precipitation is between 400 mm and 600 mm in most regions of the plateau, and precipitation is concentrated in the summer months (June to August). The greatest precipitation is in the southeastern region, but the amount has declined over the past 50 years. Morever, there have been decreases in extreme precipitation events in the southeastern region, and only minor changes in the continuous drought. Erosive rainfall is closely related to the total annual precipitation across the Loess Plateau region, and has decreased along with the decreases in annual precipitation, especially in the southeastern region. Changes in erosive rainfall account for >80% of interannual precipitation variability over large areas of the Loess Plateau. The variability in annual precipitation on the plateau is mainly affected by changes in the intensity and frequency of precipitation; changes in the length of the rainy season have only a minimal effect. Precipitation frequency contributes about 30% to interannual precipitation variability across the region as a whole. However, the eastern region is predominantly affected by changes in precipitation intensity, which contributes about 70% of the variability. These results provide valuable information to determine the dominant factor(s) influencing annual precipitation on the Loess Plateau, and may also be useful in the prevention and control of drought and soil erosion on the plateau.
机译:黄土高原生态脆弱,是中国最严重的侵蚀地区之一。在这项研究中,我们使用了1965年至2014年期间170个气象站的日降水量数据,系统地分析了高原年降水量的时空变化,并确定了影响年降水量变化的主要因素。在高原的大部分地区,年平均降水量在400 mm至600 mm之间,并且降水集中在夏季月份(6月至8月)。东南部地区是最大的降雨地区,但在过去的50年中,降水量下降了。此外,东南部地区的极端降水事件有所减少,而持续干旱仅发生了很小的变化。黄土高原地区侵蚀性降雨与年总降水量密切相关,并且随着年降水量的减少而减少,特别是在东南地区。在黄土高原的大部分地区,侵蚀性降雨的变化占年际降水变化的80%以上。高原年降水量的变化主要受降水强度和频率变化的影响。雨季长度的变化影响很小。降水频率占整个区域年际降水变化的大约30%。但是,东部地区主要受降水强度变化的影响,这贡献了约70%的变异性。这些结果为确定影响黄土高原年降水量的主要因素提供了有价值的信息,也可能有助于预防和控制高原干旱和土壤侵蚀。

著录项

  • 来源
    《Atmospheric research》 |2018年第11期|264-274|共11页
  • 作者单位

    State Key Laboratory of Earth Surface Processes and Resource Ecology, Faculty of Geographical Science, Beijing Normal University;

    State Key Laboratory of Earth Surface Processes and Resource Ecology, Faculty of Geographical Science, Beijing Normal University;

    State Key Laboratory of Earth Surface Processes and Resource Ecology, Faculty of Geographical Science, Beijing Normal University;

    State Key Laboratory of Earth Surface Processes and Resource Ecology, Faculty of Geographical Science, Beijing Normal University;

    State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, China Institute of Water Resources and Hydropower Research;

    Key Laboratory of Agricultural Non-point Source Pollution Control, Ministry of Agriculture, Institute of Agricultural Resources and Regional Planning, Chinese Academy of Agricultural Sciences;

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

    Interannual variability; Loess plateau; Precipitation; Variance decomposition;

    机译:年际变化;黄土高原;降水;方差分解;

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