热量资源； 时空变化； 年平均气温； 积温； 无霜冻期；伊犁河谷," /> 热量资源； 时空变化； 年平均气温； 积温； 无霜冻期；伊犁河谷,"/> heat resources,spatiotemporal variation,mean annual temperature,accumulated temperature,frost free period,Ili River Basin,"/> 近51 a伊犁河谷热量资源时空变化
干旱区研究

干旱区研究 ›› 2014, Vol. 31 ›› Issue (3): 472-480.

• 天气与气候 • 上一篇    下一篇

近51 a伊犁河谷热量资源时空变化

徐娇媚1,徐文修2，李大平2   

  1. 1.新疆农业大学草业与环境科学学院，新疆 乌鲁木齐 830052； 2.新疆农业大学农学院，新疆 乌鲁木齐 830052
  • 收稿日期:2013-01-19 修回日期:2013-05-20 出版日期:2014-05-15 发布日期:2014-05-30
  • 作者简介:徐娇媚（1987-），女，在读硕士研究生，研究方向为农业生态学.E-mail： xujiaomei1987@sina.com
  • 基金资助:

    国家自然基金（31260312）

Spatiotemporal Variation of Heat Resources in the Ili River  Basin in Recent 51 Years

XU Jiao-mei1, XU Wen-xiu2, LI Da-ping2   

  1. 1. Collage of Practaculture and Environment Sciences, Xinjiang Agricultural University, Urumqi 830052, China;
    2. Collage of Agronomy, Xinjiang Agricultural University, Urumqi 830052, China
  • Received:2013-01-19 Revised:2013-05-20 Published:2014-05-15 Online:2014-05-30

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被引次数

38

摘要： 基于伊犁河谷10个气象站1960—2010年年平均气温、≥0 ℃和≥10 ℃积温及无霜冻期气象资料，采用线性趋势分析、[WTBX]t-检验、[WTBZ]Kriging空间插值等方法，对伊犁河谷近51 a的热量资源时空变化特征进行分析。结果表明：① 热量资源的空间分布总体呈现平原地区多山区少的特点；② 近51 a伊犁河谷的热量资源呈增加趋势，年平均气温、≥0 ℃和≥10 ℃积温及持续日数、无霜冻期分别以0.43 ℃·（10a）-1、89.9 ℃·d·（10a）-1、88.0 ℃·d·（10a）-1、4.0 d·（10a）-1、3.2 d·（10a）-1和5.4 d·（10a）-1的倾向率上升，51 a来分别增加了2.2 ℃、458.5 ℃·d、448.8 ℃·d、20.4 d、16.3 d和27.5 d。并且各热量资源要素在20世纪90年代中后期发生突变，突变后年平均气温、≥0 ℃持续日数和无霜冻期在平原地区增幅最大，在山间盆地增幅较小。≥0 ℃与≥10 ℃积温在丘陵地区增加最明显，在山间盆地增加最少。而≥10 ℃持续日数在山间盆地增加最多，在平原地区增加最少。

关键词: font-size: 10.5pt, mso-bidi-font-family: 宋体, mso-font-kerning: 1.0pt, mso-ansi-language: EN-US, mso-fareast-language: ZH-CN, 热量资源； 时空变化； 年平均气温； 积温； 无霜冻期；伊犁河谷')">mso-bidi-language: AR-SA">热量资源； 时空变化； 年平均气温； 积温； 无霜冻期；伊犁河谷

Abstract: Based on the data from 10 meteorological stations in the Ili River Basin during the period from 1960 to 2010, the spatiotemporal change of heat resources in this area in recent 51 years were analyzed using the methods of linear regression, Ttest and spatial interpolation. The results showed that, spatially, it was richer in heat resources in plain than in the mountainous regions. The mean annual temperature, accumulated temperatures ≥0 ℃ and ≥10 ℃ and their durations as well as the frost free period were increased by 0.43 ℃·（10a）-1, 89.9 ℃·d·(10a)-1, 88.0 ℃·d·(10a)-1, 4.0 d ·(10a)-1, 3.2 d·(10a)-1 and 5.4 d·(10a)-1, equally 2.2 ℃, 458.5 ℃·d, 448.8 ℃·d, 20.4 d, 16.3 d and 27.5 d, respectively. The variations occurred mostly from the late 1990s. After mutation, the change ranges of the mean annual temperature, duration of temperature ≥0 ℃ and frost free period were the highest in plain but the lowest in the mountainous regions. The change ranges of the accumulated temperature ≥0 ℃ and ≥10 ℃ were the most significant in the hilly area but the least in the mountainous regions. The change range of the duration of temperature ≥10 ℃ was the highest in the mountainous regions but the least in plain.

Key words: font-size: 10.5pt, mso-bidi-font-family: 宋体, mso-font-kerning: 1.0pt, mso-ansi-language: EN-US, mso-fareast-language: ZH-CN, heat resources')">mso-bidi-language: AR-SA" lang="EN-US">heat resources, spatiotemporal variation, mean annual temperature, accumulated temperature, frost free period, Ili River Basin