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应用生态学报 ›› 2025, Vol. 36 ›› Issue (7): 2131-2138.doi: 10.13287/j.1001-9332.202507.022

• 研究论文 • 上一篇    下一篇

祁连山南坡植被物候对气候变化响应的地形效应

张燚1,2, 曹广超1,2,3*, 赵美亮1,2, 张倩1,2   

  1. 1青海师范大学青藏高原地表过程与生态保育教育部重点实验室, 西宁 810008;
    2青海师范大学地理科学学院青海省自然地理与环境过程重点实验室, 西宁 810008;
    3青海省人民政府-北京师范大学高原科学与可持续发展研究院, 西宁 810008
  • 收稿日期:2024-12-06 接受日期:2025-05-08 出版日期:2025-07-18 发布日期:2026-01-18
  • 通讯作者: *E-mail: caoguangchao@qhnu.edu.cn
  • 作者简介:张 燚, 女, 2000年生, 硕士研究生。主要从事植被物候遥感监测研究。E-mail: zhangyis6@163.com
  • 基金资助:
    青海省自然科学基金项目(2023-ZJ-907M)

Topographic effects on vegetation phenology in response to climate change on the southern slope of Qilian Mountains, Northwest China

ZHANG Yi1,2, CAO Guangchao1,2,3*, ZHAO Meiliang1,2, ZHANG Qian1,2   

  1. 1Key Laboratory of Tibetan Plateau Land Surface Processes and Ecological Conservation (Ministry of Education), Qinghai Normal University, Xining 810008, China;
    2Qinghai Provincial Key Laboratory of Physical Geography and Environmental Process, College of Geographical Science, Qinghai Normal University, Xining 810008, China;
    3Academy of Plateau Science and Sustainability, People’s Government of Qinghai Province and Beijing Normal University, Xining 810008, China
  • Received:2024-12-06 Accepted:2025-05-08 Online:2025-07-18 Published:2026-01-18

摘要: 祁连山南坡属于典型山地生态系统,研究其复杂地形与气候变化交互作用下的植被物候响应机制对揭示生态适应性规律具有重要科学价值。本研究基于2002—2020年MODIS NDVI数据,结合地形因子和气象数据,利用相关分析和结构方程模型定量解析地形因子在植被物候响应气候变化中的作用。结果表明:2002—2020年间,研究区植被返青期、枯黄期和生长季长度分别以0.33、0.19和0.51 d·a-1的速率显著提前、推迟和延长,且空间上呈西北-东南梯度分异;该区植被物候对气温和降水的响应具有空间异质性,与地形因子存在关联,受不同环境条件及水热组合模式的共同调控;海拔对植被物候影响最显著,坡向次之。海拔和坡向通过气象因子对植被物候的影响具有累积作用,而坡度通过气象因子对植被物候的影响相互间具有抵消作用。

关键词: 地形因子, 植被物候, 气候变化, 祁连山南坡

Abstract: The southern slope of the Qilian Mountains is a typical mountain ecosystem. To understand the vegetation phenological response mechanisms under the interaction between complex terrain and climate change is of significance in revealing ecological adaptability laws. Based on MODIS NDVI data from 2002 to 2020, combined with topographic and meteorological datasets, we used correlation analysis and structural equation modeling to quantitatively assess the role of topography in mediating vegetation phenological responses to climate change. The results showed that the start of the growing season, end of the growing season, and length of the growing season in the study area advanced, delayed, and extended at rates of 0.33, 0.19, and 0.51 d·a-1, respectively, with spatial differentiation exhibiting a distinct northwest-southeast gradient. Regional vegetation phenology displayed spatial heterogeneity in its responses to the changes in temperature and precipitation, modulated by topographic factors and jointly governed by diverse environmental conditions and hydrothermal regimes. Elevation had the most pronounced influence on vegetation phenology, followed by aspect. Elevation and aspect exerted cumulative effects on vegetation phenology through meteorological factors, while the influence of slope on vegetation phenology through meteorological factors was offset by each other.

Key words: terrain factor, vegetation phenology, climate change, southern slope of Qilian Mountains