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中国农学通报 ›› 2016, Vol. 32 ›› Issue (2): 135-141.doi: 10.11924/j.issn.1000-6850.casb15080157

• 资源 环境 生态 土壤 气象 • 上一篇    下一篇

西南地区1960—2013年参考作物蒸散量时空变化特征及成因分析

张伟伟,王 允,张国斌   

  1. (西北师范大学地理与环境科学学院,兰州 730070)
  • 收稿日期:2015-08-31 修回日期:2015-10-20 接受日期:2015-10-23 出版日期:2016-01-28 发布日期:2016-01-28
  • 通讯作者: 张伟伟
  • 基金资助:
    国家自然科学基金(41061022)。

Temporal and Spatial Change of Reference Crop Evapotranspiration and Its Cause Analysis in Southwest China During 1960-2013

Zhang Weiwei, Wang Yun, Zhang Guobin   

  1. (College of Geography and Environment Science, Northwest Normal University, Lanzhou 730070)
  • Received:2015-08-31 Revised:2015-10-20 Accepted:2015-10-23 Online:2016-01-28 Published:2016-01-28

摘要: 基于西南地区108个气象站点1960—2013年逐日气温、降水、风速、日照时数、太阳总辐射和相对湿度数据,应用Penman-Monteith模型和ArcGIS反距离加权插值法,分析其参考作物蒸散量时空变化及影响因素。结果表明:近54年来,西南地区参考作物蒸散量在波动中呈降低趋势,其变化倾向率为 -4.509 mm/10 a,其中降低幅度以20世纪90年代最大,距平值为-19.526 mm,增幅却以70年代最显著,为12.744 mm,特别是在20世纪70年代至21世纪初,参考作物蒸散量大幅下降,最低值出现在2000年,为628.264 mm;从季节变化看,春夏季呈降低、秋冬季却有上升的趋势。参考作物蒸散量存在明显的空间差异,表现为:以云贵高原西部为高值中心,向四周递减,且低值区分布面积远大于高值区,高值区位于云南高原和广西丘陵部分地区,低值区分布在四川盆地、贵州高原、松潘高原和滇西北高海拔地区。影响西南地区参考作物蒸散量的因子主要以日照时数、风速和相对湿度为主,但各区所受主控因子却不尽相同。

关键词: 萎凋, 萎凋, 红茶, 理化变化, 影响因子, 工艺技术

Abstract: Based on the daily temperature, precipitation, wind speed, sunshine hours, total solar radiation and related humidity data of the 108 meteorological stations in southwest China during 1960 to 2013, the authors used the methods of Penman-Monteith model and inverse distance weighted interpolation, to analyze the temporal-spatial variations and the possible influential factors of the reference crop evapotranspiration (ET0) in this region. The results were as follows: (1) the annual mean value of ET0 was decreasing in fluctuation and the decreasing rate was -4.509 mm/10 a in recent 54 years, ET0 had the most significant reduction in 1990s and the most increase of 12.744 mm in 1970s; from late 1970s to the beginning of the 21st centuries, ET0 decreased significantly; (2) on the seasonal scale, the change trend of ET0 decreased in spring and summer, but increased in autumn and winter; (3) the change trend of the reference crop evapotranspiration had obvious differences in the space, there was an obviously high value center in Yunnan-Guizhou Plateau and it decreased gradually in the surrounding area; the distribution area of low value was far greater than that of high value, the high value area was located in the Yunnan Plateau-Guangxi Basin and the low value was distributed in Sichuan Basin, Guizhou Plateau, Songpan Plateau and the high altitude area in northwest Yunnan; (4) influencing factors of reference crop evapotranspiration were mainly sunshine hours, wind speed and relative humidity in southwest region, but the main control factor was not the same in all regions.

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