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中国农学通报 ›› 2016, Vol. 32 ›› Issue (8): 147-153.doi: 10.11924/j.issn.1000-6850.casb15110118

• 资源 环境 生态 土壤 气象 • 上一篇    下一篇

1981—2014年西藏0℃界限温度变化趋势的时空分布

马鹏飞1,杜 军1,杜晓辉2   

  1. (1西藏自治区气候中心,拉萨 850001;2拉萨市气象局,拉萨 850001)
  • 收稿日期:2015-11-23 修回日期:2015-12-15 接受日期:2015-12-24 出版日期:2016-03-18 发布日期:2016-03-18
  • 通讯作者: 杜军
  • 基金资助:
    公益性行业(气象)科研专项“青藏高原多源实测气象数据集的研制”(GYHY201306029)。

Spatial and Temporal Distribution of 0℃ Boundary Temperature Change in Tibet During 1981-2014

Ma Pengfei1, Du Jun1, Du Xiaohui2   

  1. (1Tibet Climatic Centre, Lhasa 850001; 2Lhasa Meteorological Service, Lhasa 850001)
  • Received:2015-11-23 Revised:2015-12-15 Accepted:2015-12-24 Online:2016-03-18 Published:2016-03-18

摘要: 在气候变暖背景下,分析西藏0℃界限温度变化的时空分布特征,以期合理开发农业气候资源。利用西藏38个站点1981—2014年逐日平均气温资料,采用气候倾向率、M-K和距平等统计方法,对西藏≥0℃初日、终日、持续日数及积温的时空分布特征进行分析。结果表明:近34年西藏平均每10年≥0℃初日提早3.1天、终日推迟1.9天、持续日数延长5.0天和积温增加83.2℃·d,这种变化在低海拔地区表现的更明显。大部分站点≥0℃界限温度都表现初日提早、终日推迟、持续日数延长和积温增多的年代际变化特征。≥0℃初日和积温的突变点出现在21世纪初,终日突变时间早,发生在20世纪80年代后期,而持续日数在90年代中后期出现了突变。

关键词: 流域, 流域, 生态服务价值, 土地利用, 评价方法

Abstract: Under the background of climate warming, the authors studied the change characteristics of 0℃ boundary temperature in Tibet, in order to rationally develop agricultural climate resources. Based on the daily air temperature data of 38 meteorological stations from 1981 to 2014, by using the linear trend method, the M-K method and anomaly, several elements were analyzed, including the beginning day, terminal day, duration and accumulated temperature of the daily temperature above 0℃ stably. The results showed that the beginning day was in advanced with a rate of 3.1 d/10 a, the ending day was delayed with a rate of 1.9 d/10 a, the duration was increased 5.0 days per decade, and the accumulated temperature of the daily temperature above 0℃ stably had an increasing trend, which increased 83.2℃ per decade in Tibet, and the change was more obvious in lower altitude. It was also found that the inter-decadal variation trend of the critical temperature ≥0℃ presented the characteristics of earlier beginning day, delayed terminal day, prolonged duration and increased accumulated temperature in most part of Tibet. In Tibet, the climate mutation point of the first day and the accumulated temperature occurred in the early 21st century, the mutation time of the terminal day was in the late 1980s and that of the duration was in the mid-late 1990s.

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