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2000-2022年青藏高原植被覆盖地形分异效应

龚成麒 苏中波 黄新惠 董晓华 马耀明 魏冲 喻丹 李璐 张特 彭涛

生态学报2026,Vol.46Issue(10):5571-5586,16.
生态学报2026,Vol.46Issue(10):5571-5586,16.DOI:10.20103/j.stxb.202509012262

2000-2022年青藏高原植被覆盖地形分异效应

Study on the topographic differentiation effects of vegetation coverage on the Tibetan Plateau from 2000-2022

龚成麒 1苏中波 2黄新惠 3董晓华 1马耀明 4魏冲 1喻丹 1李璐 1张特 1彭涛1

作者信息

  • 1. 三峡大学水利与环境学院,宜昌 443002||三峡大学三峡库区生态环境教育部工程研究中心,宜昌 443002
  • 2. 荷兰特文特大学地理信息科学与对地观测学院,恩斯赫德7500 AE
  • 3. 长江水利委员会水文局长江三峡水文水资源勘测局,宜昌 443000
  • 4. 三峡大学水利与环境学院,宜昌 443002||中国科学院青藏高原研究所青藏高原地球系统与资源环境重点实验室地气作用与气候效应团队,北京 100101||中国科学院大学地球与行星科学学院,北京 100049||兰州大学大气科学学院,兰州 730000||中国科学院青藏高原研究所西藏珠穆朗玛特殊大气过程与环境变化国家野外科学观测研究站,定日 858200||中国科学院加德满都科教中心,北京 100101||中国科学院中国-巴基斯坦地球科学研究中心,伊斯兰堡45320
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摘要

Abstract

Understanding the vegetation distribution patterns across different topographic conditions of the Tibetan Plateau is essential for assessing alpine climate responses,ecosystem conservation,and biodiversity maintenance.This study investigates the spatial differentiation of vegetation on the Tibetan Plateau under varying elevation,slope,and aspect conditions,based on Enhanced Vegetation Index(EVI)data from 2000 to 2022 and DEM-derived topographic information.Trend analysis and topographic correction methods were employed to assess vegetation dynamics.The results show that:(1)overall,76.45%of the vegetation exhibited an improving trend,and this improvement was mainly distributed in regions such as the Hoh Xil Mountains,the Qiangtang-Wenjia Ri area,and the northern Bayan Har Mountains.These areas generally showed stable or gradually enhanced vegetation conditions throughout the study period.In contrast,2.2%of the vegetation experienced significant degradation,primarily located in the Qaidam Basin,the eastern Dongbuli Mountains,and the western Bayan Har Mountains.(2)Vegetation located on sunny slopes generally exhibited better growth conditions than vegetation on shady slopes.This pattern may be related to the fact that climate warming has intensified permafrost thawing and snowmelt on sunny slopes,which in turn increases the amount of available soil moisture.At the same time,a longer duration of sunshine on sunny slopes can further enhance vegetation photosynthesis,and the combined effect of increased water availability and extended solar radiation may jointly promote vegetation growth.(3)The EVI values showed an overall linear decrease with increasing elevation.However,in the 2000-3000 m elevation range,EVI values were anomalously low,even lower than those in the 3000-4000 m range.This pattern is mainly attributed to the Qaidam Basin,which dominates this elevation band.The surrounding mountains block moisture transport into the basin,leading to extremely low precipitation and sparse vegetation cover.When the elevation exceeds 4000 m,EVI values generally fall below 0.2,indicating that vegetation becomes increasingly limited and gradually disappears as environmental constraints strengthen with elevation.Findings(2)and(3)differ from the commonly reported conclusions that"low elevation,gentle slopes,and shady aspects favor vegetation growth,and that vegetation indices typically show a nonlinear relationship with elevation(increasing first and then decreasing)."This suggests that vegetation dynamics on the Tibetan Plateau do not follow the same ecological patterns observed in non-plateau regions.Therefore,ecological conservation strategy should prioritize the 2000-3000 m elevation zone,where vegetation cover is constrained by limited precipitation,and future efforts should strengthen long-term ecological monitoring and biodiversity protection in key degradation areas such as the Qaidam Basin and western Bayan Har Mountains to promote vegetation restoration and ecosystem stability.

关键词

植被变化/增强植被指数/地形分异效应/青藏高原

Key words

vegetation change/enhanced vegetation index/topographic differentiation effects/Tibetan Plateau

引用本文复制引用

龚成麒,苏中波,黄新惠,董晓华,马耀明,魏冲,喻丹,李璐,张特,彭涛..2000-2022年青藏高原植被覆盖地形分异效应[J].生态学报,2026,46(10):5571-5586,16.

基金项目

第二次青藏高原科学考察与研究项目(2019QZKK0103) (2019QZKK0103)

国家自然科学基金项目(52109058) (52109058)

长江科学院水利部长江中下游河湖治理与防洪重点实验室开放基金(CKWV20241170/KY) (CKWV20241170/KY)

生态学报

OACHSSCD

1000-0933

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