中国农业气象 ›› 2015, Vol. 36 ›› Issue (06): 683-691.doi: 10.3969/j.issn.1000-6362.2015.06.004

• 论文 • 上一篇    下一篇

北疆地区生长季参考作物蒸散量的时空变化特征及其敏感性分析

李思思,张飞云,白 磊,李兰海   

  1. 1.中国科学院新疆生态与地理研究所/荒漠与绿洲生态国家重点实验室,乌鲁木齐 830011;2.中国科学院大学,北京 100049
  • 收稿日期:2015-03-23 出版日期:2015-12-20 发布日期:2015-12-17
  • 作者简介:李思思(1988-),女,硕士生,主要从事水文水资源研究。E-mail:lisisidili13@163.com
  • 基金资助:
    新疆维吾尔自治区重点实验室专项资金(2014KL015);自然科学基金(41401030)

Spatiotemporal Variation and Sensitivity of Reference Crop Evapotranspiration during Growth Season in Northern Xinjiang

LI Si-si, ZHANG Fei-yun, BAI Lei, LI Lan-hai   

  1. 1. Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences/ State Key Laboratory of Desert and Oasis Ecology, Urumqi 830011, China; 2.University of Chinese Academy of Sciences, Beijing 100049
  • Received:2015-03-23 Online:2015-12-20 Published:2015-12-17

摘要: 基于北疆地区20个气象站点1966-2012年逐日气象数据,采用Penman-Monteith公式计算各站生长季逐日参考作物蒸散量(ET0),利用线性趋势分析、M-K突变检验、因子贡献率、敏感系数等方法,对该地区ET0的时空变化规律及其对气象要素的敏感性进行分析。结果表明,北疆地区生长季ET0多年平均值为939.43mm,47a间以16.30mm×10a-1的速率呈极显著下降趋势(P水汽压>风速>日照时数。水汽压升高、风速减小、日照时数减少对ET0的减小作用超过温度上升对ET0的增大作用,是导致近47a北疆地区ET0总体呈下降趋势的根本原因。

关键词: 参考作物蒸散量, Penman-Monteith公式, 贡献率, 敏感性, 北疆地区

Abstract: Based on daily meteorological data from 20 meteorological stations from 1966 to 2012, ET0 was calculated during crops growing season by using the Penman-Monteith equation. The spatiotemporal variation of ET0 and its sensitivity to key climatic factors were analyzed by using of the Mann-Kendall test, the factors' dedication rate, and sensitive coefficients. The results showed that the average ET0 in Northern Xinjiang was 939.43mm, and the ET0 decreased at the rate of 16.30mm·10y-1 in last 47 years, with an abrupt change in 1981 according to the Mann-Kendall trend test. Low ET0 values occurred in mountain regions, while high values were found in the Junggar basin and piedmont plain. Average wind speed played the most important role with regards to changes in ET0, followed by temperature, vapor pressure, and sunshine hours. ET0 was sensitive to vapor pressure negatively, and sensitive to temperature, average wind speed, and sunshine hours positively in Northern Xinjiang. The values of sensitive coefficients to climatic factors were temperature, vapor pressure, wind speed, and sunshine hours. The promoting effect of elevated vapor pressure, less wind speed, and less sunshine hours on ET0 was stronger than the reducing effect of increased temperature, which was the key reason that ET0 decreased generally during crops growth season in Northern Xinjiang.

Key words: Reference crop evapotranspiration, Penman-Monteith equation, Contribution rate, Sensitivity, Northern Xinjiang