草地学报 ›› 2021, Vol. 29 ›› Issue (S1): 93-103.DOI: 10.11733/j.issn.1007-0435.2021.Z1.011

• 研究论文 • 上一篇    下一篇

青海省草地植被干旱评估及驱动力分析研究

赵梦凡1,2, 周秉荣1,2, 赵彤1,2, 周华坤3, 校瑞香1,2, 颜亮东1,2, 李璠1,2   

  1. 1. 青海省气象科学研究所, 青海 西宁 810001;
    2. 青海省防灾减灾重点实验室, 青海 西宁 810001;
    3. 中科院西北高原生物研究所/青海省寒区恢复生态学重点实验室, 青海 西宁 810008
  • 收稿日期:2021-04-15 修回日期:2021-06-02 出版日期:2021-10-30 发布日期:2021-11-17
  • 通讯作者: 周秉荣,E-mail:zbr0515@foxmail.com
  • 作者简介:赵梦凡(1991-),女,陕西宝鸡人,助理工程师,主要从事农业气象与生态环境研究,E-mail:zhaomengfan1001@163.com
  • 基金资助:
    青海省科技成果转化项目(2018-SF-142);中国气象局旱区特色农业气象灾害监测预警与风险管理重点实验室开放基金项目(CAMF-201904);中央级公益性科研院所基本科研业务费专项(IDM2018011);青海省气象局面上项目(QXMS2021-47)资助

Drought Evaluation and Driving Force Analysis of Grassland in Qinghai Province

ZHAO Meng-fan1,2, ZHOU Bing-rong1,2, ZHAO Tong1,2, ZHOU Hua-kun3, XIAO Rui-xiang1,2, YAN Liang-dong1,2, LI Fan1,2   

  1. 1. Qinghai Academy of Meteorological Sciences, Xining, Qinghai Province 810001, China;
    2. Key Laboratory for Disaster Prevention and Mitigation in Qinghai, Xining, Qinghai Province 810001, China;
    3. Northwest Institute of Plateau Biology, Chinese Academy of Science/Key laboratory of restoration ecology of cold area in Qinghai Province, Xining, Qinghai Province 810008, China
  • Received:2021-04-15 Revised:2021-06-02 Online:2021-10-30 Published:2021-11-17

摘要: 为了研究青海省草地植被干旱特征及驱动因子,以青海省草地植被覆盖区域为对研究对象,采用水量平衡和作物需水量等方法构建干旱评估模型,评估青海省草地植被干旱时空分布特征和发生趋势,并探讨形成干旱的关键驱动因素,结果表明:整个生长季东部农业区、环青海湖区、祁连山区大部草地植被基本维持轻旱和无旱,严重干旱区域集中在青南牧区的低覆盖度草地,干旱空间总体分布基本表现为低覆盖度>中覆盖度>高覆盖度;草地植被在整个生长季的干旱灾害类型以轻旱为主,中旱次之,重旱和特旱发生频率较低,极端干旱强度呈增加态势;降水和蒸散在整个干旱发生过程中驱动作用最大,且均为负向影响,随着干旱等级加重,蒸散逐渐代替降水成为影响干旱的最重要驱动因子。风速整体上对干旱的影响表现为正向,气温、日照时数和水汽压对干旱影响作用较小。

关键词: 草地植被, 干旱, 变化特征, 驱动因子

Abstract: This study was aimed to find out the drought characteristics and driving factors of grassland in Qinghai Province. The grassland coverage area in Qinghai Province was selected as the sampling site. The temporal and spatial distribution characteristics and occurrence trend of grassland drought in Qinghai Province were evaluated according to the water balance and crop water requirement and the key driving factors of drought were explored. The results showed that:during the whole growing season, the grassland in the eastern agricultural area, the peripheral area of the Qinghai Lake and the Qilian mountain area maintained light drought and no drought. The serious drought areas were mainly distributed in the southern Qinghai Pastoral Area and some low coverage grassland areas. The spatial distribution of drought was low coverage grassland > medium coverage grassland > high coverage grassland;the drought disaster type of grassland in the whole growing season was mainly light drought, followed by medium drought, the frequency of severe drought and special drought was low, and the intensity of extreme drought was increasing;precipitation and evapotranspiration played the largest driving role in the whole drought process, and they were all negative. With the aggravation of drought grade, evapotranspiration gradually replaced precipitation as the most important driving factor. On the whole, wind speed has a positive effect on drought, while temperature, sunshine hours, and water vapor pressure have little effect on drought.

Key words: Grassland, Drought, Change characteristics, Driving factors

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