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中国农学通报 ›› 2017, Vol. 33 ›› Issue (2): 106-114.doi: 10.11924/j.issn.1000-6850.casb16030195

• 资源 环境 生态 土壤 气象 • 上一篇    下一篇

1961—2013年青海省柴达木盆地日照时数的 变化特征及其影响因素

肖莲桂   

  1. 青海省天峻县气象局
  • 收稿日期:2016-03-28 修回日期:2016-12-29 接受日期:2016-06-14 出版日期:2017-02-09 发布日期:2017-02-09
  • 通讯作者: 肖莲桂
  • 基金资助:
    2016 年青海省气象局面上项目“ISOS 新型自动站能见度与人工观测能见度对比分析研究”(201609);国家自然科学基金地区科学基金项 目“青藏高原地区气溶胶变化特征”(41161009)。

Sunshine Hours Variation Characteristics and Influencing Factors in Qaidam Basin During 1961-2013

  • Received:2016-03-28 Revised:2016-12-29 Accepted:2016-06-14 Online:2017-02-09 Published:2017-02-09

摘要: 为了了解近50 年来青海省柴达木盆地日照时数的分布规律和变化趋势及其变化原因,利用1961—2013 年青海省柴达木盆地9 个气象站日照时数、气温、云量、降水、风速和水汽压等月资料,通过统计学方法和突变检验等方法,对柴达木盆地日照时数的气候变化特征进行分析。结果表明:近53 年来青海省柴达木盆地日照时数在全年及四季均呈现出显著减少的年际变化特征,1990 年前后日照时数由明显偏多变为明显偏少。年日照时数呈现出从西北部向东南部减小的分布格局特点,最大值在西北部的冷湖站,最小值在东南部的茶卡站。春夏秋3 季日照时数的分布特征与年日照时数的分布特征相似,冬季的分布特征为从南部向北部逐渐减小。年日照时数气候倾向率分布特征以大柴旦和格尔木为分界线,形成东西2 个明显的下降区域,其中东西2 个区域日照时数下降最大的为冷湖和茶卡站。柴达木盆地年日照时数在1995 年发生突变。影响青海省柴达木盆地日照时数的主要因子是云量,而次要因子表现略有不同。

关键词: 农村居民点, 农村居民点, 空间分布, 特征, 环境, 宁夏中部干旱带

Abstract: The paper aims to understand the distribution rule and trend of sunshine hours, and their changing reasons in the Qaidam Basin of Qinghai over the past 50 years. The authors used the statistical method and abrupt change test to analyze the variation characteristics of sunshine hours, based on the monthly data of sunshine hours, temperature, cloud cover, precipitation, wind velocity, vapor pressure from 9 meteorological stations in Qaidam Basin. The results showed that: the annual variation characteristics of sunshine hours in the Qaidam Basin significantly decreased in the whole year and the four seasons, the variation characteristics of sunshine hours reached a turning point in 1990; the distribution pattern of annual sunshine hours decreased from the northwest to the southeast, the maximum value was in the Lenghu station, and the minimum value was in the Chaka station; the distribution characteristics of sunshine hours in spring, summer, autumn were similar to that of annual distribution, though the distribution characteristics in winter gradually decreased from the south to the north; Dachaidan and Golmud were taken as the dividing line of distribution characteristics of the climate tendency rate of annual sunshine hours, there were two obvious decline regions, of which the maximum decrease was in Lenghu and Chaka station; the annual sunshine hours had a mutation in 1995 in Qaidam Basin; the main factor affecting sunshine hours in Qaidam Basin in Qinghai was cloud cover, while the secondary factor was slightly different.

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