长江科学院院报 ›› 2021, Vol. 38 ›› Issue (4): 43-49.DOI: 10.11988/ckyyb.20200088

• 水土保持与生态修复 • 上一篇    下一篇

三峡水库蓄水前后植被覆盖对气候的响应

田梦琦1,2, 周建中1,2, 张勇传1,2, 贾本军1,2, 陈璐1,2   

  1. 1.华中科技大学 土木与水利工程学院,武汉 430074;
    2.华中科技大学 数字流域科学与技术湖北省重点实验室,武汉 430074
  • 收稿日期:2020-02-10 修回日期:2020-05-28 出版日期:2021-04-01 发布日期:2021-04-17
  • 通讯作者: 周建中(1959-),男,湖北武汉人,教授,硕士,研究方向为水电能源复杂系统优化先进理论与方法。E-mail: jz.zhou@hust.edu.cn
  • 作者简介:田梦琦(1996-),女,河南安阳人,博士研究生,研究方向为水文水资源。E-mail: tmq@hust.edu.cn
  • 基金资助:
    国家自然科学基金重点项目(U1865202,91547208);国家十三五重点研发计划项目(2016YFC0402205)

Response of Vegetation Cover to Climate Before and After Impoundment in Three Gorges Reservoir

TIAN Meng-qi1,2, ZHOU Jian-zhong1,2, ZHANG Yong-chuan1,2, JIA Ben-jun1,2, CHEN Lu1,2   

  1. 1. School of Civil and Hydraulic Engineering,Huazhong University of Science and Technology,Wuhan 430074, China;
    2. Hubei Key Laboratory of Digital Valley Science and Technology,Huazhong University of Science and Technology, Wuhan 430074, China
  • Received:2020-02-10 Revised:2020-05-28 Published:2021-04-01 Online:2021-04-17

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摘要： 为揭示三峡水库蓄水前后区域植被覆盖对气候变化的响应规律,基于SPOT NDVI和实际观测气象数据,采用偏相关系数法分析了三峡水库蓄水前后长江上游干流区间寸滩至宜昌段及外围100 km的气象因子与植被覆盖的相关性,同时对其非线性映射关系进行了研究。结果表明:在长江上游干流区间寸滩至宜昌段及外围100 km区域内,植被覆盖对气温和降水变化的动态响应具有较强的空间异质性,且气温是植被覆盖变化的主要驱动因素;二次函数可有效刻画植被覆盖对气温的响应规律,且较好地解释了植被覆盖-气温响应关系中的物理机制;植被覆盖对气温的响应规律在一定程度上受三峡水库蓄水影响,且随着与河道距离的增加,植被覆盖对气温的响应受蓄水影响程度递减。

关键词: 植被覆盖, NDVI, 气候响应, 蓄水, 三峡水库

Abstract: The aim of this research is to reveal the response of vegetation cover to climate change before and after the Three Gorges impoundment. The correlation between vegetation cover and climate factors in the upstream of the Yangtze River from Cuntan to Yichang and 100 km around was analyzed by using partial correlation coefficient method based on SPOT NDVI and observed meteorological data. Meanwhile, the non-linear mapping relationship was also investigated. Results unveiled high spatial heterogeneity of the dynamic response of vegetation cover to temperature and precipitation in the study area. Temperature is the major driving factor of vegetation cover variations. Second-order non-linear mapping effectively characterizes the response of vegetation cover to temperature, and well explains the physical mechanism of the relationship between vegetation cover and temperature. The response of vegetation cover to temperature is affected by the impoundment of the Three Gorges Reservoir to a certain extent, and the influence degree attenuates with the distancing from the river.

Key words: vegetation cover, normalized difference vegetation index(NDVI), climate response, impoundment, Three Gorges Reservoir

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