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刘艳艳, 张耀宗, 王 东, 张多勇.1960—2020年黄土高原地区降水特征时空格局研究水资源与水工程学报[J].,2025,36(5):121-127
1960—2020年黄土高原地区降水特征时空格局研究
Spatio-temporal patterns of precipitation from 1960 to 2020 over the Loess Plateau
  
DOI:10.11705/j.issn.1672-643X.2025.05.14
中文关键词:  降水量  降水日数  降水强度  时空分布  黄土高原
英文关键词:precipitation amount  precipitation days  precipitation intensity  spatio-temporal distribution  the Loess Plateau
基金项目:国家社会科学基金项目(22XZS022);2023年甘肃省高校青年博士支持项目(2023QB-018); 庆阳市重点研发计划项目(社会发展类) (QY-STK-2023B-109)
作者单位
刘艳艳1,2, 张耀宗1,2, 王 东1,2, 张多勇3 (1.陇东学院 地理与城乡规划学院 甘肃 庆阳 745000 2.庆阳市水土保持与荒漠化防治遥感技术创新中心甘肃 庆阳 745000 3.北方民族大学 鄂尔多斯盆地历史地理研究中心 宁夏 银川 750021) 
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中文摘要:
      掌握黄土高原降水的时空变化特征对区域水资源管理与生态环境保护具有重要意义。基于黄土高原地区292个气象站点1960—2020年的日降水观测数据,采用Mann-Kendall趋势检验和线性趋势分析方法,系统分析了降水量、降水日数和降水强度的时空变化特征。结果表明:多年平均年降水量为433 mm,降水日数为80 d,降水强度为5.3 mm/d,三者均呈现由东南向西北递减的空间格局;降水日数的空间分布范围为36~134 d,其中60~100 d区间占主要部分;降水强度的空间分布范围为3.1~9.1 mm/d,6.0 mm/d等值线在东经111°以西呈纬向分布特征;区域降水量总体呈减少趋势,气候倾向率为-4 mm/10a,降水日数呈减少趋势,降水强度无显著变化;时间变化趋势的空间差异显著,以临夏-兰州-庆阳-延安-太原一线为界,以南地区降水量呈减少趋势,以北地区呈增加趋势;降水指标的空间格局呈现明显的年代际演变特征,1990s降水日数减少最为显著,2010 s降水量和降水强度增强。研究揭示了黄土高原降水变化的复杂性和区域差异性,为该区域水资源管理和气候变化适应提供了科学依据。
英文摘要:
      Understanding the spatio-temporal variations of precipitation is crucial for regional water resources management and ecological environment protection in Loess Plateau. Based on daily precipitation observations from 292 meteorological stations across the Loess Plateau from 1960 to 2020, this study analyzes the spatio-temporal characteristics of precipitation amount, precipitation days, and precipitation intensity using the Mann-Kendall trend test and linear trend analysis. The results indicate that the long-term mean annual precipitation was 433 mm, with an average of 80 precipitation days and a precipitation intensity of 5.3 mm/day. All three indicators exhibited a decreasing spatial gradient from southeast to northwest. The number of precipitation days ranged from 36 to 134, dominating by the range of 60-100. Precipitation intensity varied from 3.1 to 9.1 mm/day, with the 6 mm/day isohyet showing a zonal distribution west of 111°E longitude. Over the past 61 years, the region has experienced an overall decreasing trend in precipitation amount, with a climatic tendency rate of -4 mm·(10a)-1. The number of precipitation days has also declined, whereas precipitation intensity showed no significant change. A pronounced spatial disparity in temporal trends is observed on both sides of the Linxia-Lanzhou-Qingyang-Yan’an-Taiyuan line, precipitation has generally decreased south to the line but increased north to it. The spatial pattern of precipitation indicators presented distinct interdecadal variations. The 1990s witnessed the most substantial decrease in precipitation days, while the 2010s saw increases in both precipitation amount and intensity. These findings highlight the complexity and regional heterogeneity of precipitation changes across the Loess Plateau, which can provide a scientific basis for water resources management and climate change adaptation in the region.
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