文章摘要
王 涛, 于冬雪, 杨 强.陕北黄土高原地区降水时空变化特征Journal of Water Resources and Water Engineering[J].,2014,25(6):24-28
陕北黄土高原地区降水时空变化特征
Characteristics of spatial-temporal change of precipitation in loess plateau area of northern Shaanxi
  
DOI:10.11705/j.issn.1672-643X.2014.06.005
中文关键词: 降水指数  线性趋势  Mann-Kendall检验  黄土高原
英文关键词: precipitation index  linear trend  Mann-Kendall test  loess plateau
基金项目:国家自然科学基金项目(41271103); 西安科技大学博士启动基金项目(2012QDJ029)
Author NameAffiliation
WANG Tao1, YU Dongxue2, YANG Qiang3 (1.西安科技大学 测绘科学与技术学院 陕西 西安 710054 2.江西信息应用职业技术学院环境工程系 江西 南昌 330043 3.南京林业大学 土木工程学院 江苏 南京210037) 
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中文摘要:
      以位于陕北黄土高原地区的6个气象站点1959-2011年逐日降水数据为基础,选择降水量、降水强度、日最大降水、有降水日数、中雨日数和大雨日数6个降水指数,利用线性趋势法、Mann-Kendall突变检验法及IDW空间插值方法,分析了陕北黄土高原地区近53 a降水时空变化特征。结果表明:①陕北黄土高原地区有降水日数减少趋势显著,降水强度增加趋势显著,其它指数均呈不显著的减少趋势。1960-1969年为陕北黄土高原地区降水多发期,而1990-1999年为匮乏期。②陕北黄土高原地区降水强度于1984年发生增加突变,有降水日数于1980年发生减少突变。③陕北黄土高原地区降水强度以延安地区为高值中心,吴起为低值中心;其它指数均以洛川为高值中心,横山为低值中心,呈自南而北的递减规律,表现出对季风气候过程的响应。有降水日数持续减少和降水强度持续增加将会导致陕北黄土高原地区土壤侵蚀加剧,应予以重视。
英文摘要:
      Based on the data of daily precipitation in 6 meteorological stations at loess plateau area of northern Shaanxi from 1959 to 2011, the paper chose six precipitation indexes including rainfall, intensity of rainfall, the maximum rainfall of day, the number of day rainfall, days of moderate rain and heavy rain, and used methods of linear trend, Mann-Kendall abrupt test, and IDW spatial interpolation to analyze the Characteristics of spatial-temporal change of precipitation in loess plateau area of northern Shaanxi in 53 years. Results show that:① the number of day rainfall decreases obviously while the intensity of rainfall increases obviously.Other precipitation indexes decrease insignificantly. Precipitation in the area occurred frequently in 1960s and was shortage in 1990s. ②The intensity of precipitation occured abrupt increase in 1984, while the number of day rainfall happened abrupt decrease in 1980. ③The high value center of intensity of precipitation is in Yan'an, while low value center is in Wuqi. However, the high value center of other indexes is in Luochuan,while the low value center is in Hengshan. Those value center of precipitation indexes show decreased tendency from south to north, which reflect the response to monsoon process. The decrease of number of rainfall day and the increase of intensity of precipitation will lead to soil erosion in loess plateau which can be taken attention.
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