Response of Natural Forests and Grasslands in Xinjiang to Climate Change Based on Sun-Induced Chlorophyll Fluorescence

被引:0
|
作者
He, Jinrun [1 ,2 ]
Fan, Jinglong [1 ,3 ]
Lv, Zhentao [1 ,2 ]
Li, Shengyu [1 ,4 ]
机构
[1] Chinese Acad Sci, Xinjiang Inst Ecol & Geog, Natl Engn Technol Res Ctr Desert Oasis Ecol Constr, 818 South Beijing Rd, Urumqi 830011, Peoples R China
[2] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
[3] Taklimakan Desert Ecosyst Field Observat & Res Stn, Qiemo 841900, Peoples R China
[4] Chinese Acad Sci, Xinjiang Inst Ecol & Geog, Mosowan Desert Res Stn, Shihezi 832061, Peoples R China
关键词
sun-induced chlorophyll fluorescence (SIF); standardized precipitation evapotranspiration index (SPEI); natural forests and grasslands; climate change; spatiotemporal variation characteristics; DROUGHT; VEGETATION; IMPACT; PRODUCTIVITY; REDUCTION;
D O I
10.3390/rs17010152
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
In arid regions, climatic fluctuations significantly affect vegetation structure and function. Sun-induced chlorophyll fluorescence (SIF) can quantify certain physiological parameters of vegetation but has limitations in characterizing responses to climate change. This study analyzed the spatiotemporal differences in response to climate change across various ecological regions and vegetation types from 2000 to 2020 in Xinjiang. According to China's ecological zoning, R1 (Altai Mountains-Western Junggar Mountains forest-steppe) and R5 (Pamir-Kunlun Mountains-Altyn Tagh high-altitude desert grasslands) represent two ecological extremes, while R2-R4 span desert and forest-steppe ecosystems. We employed the standardized precipitation evapotranspiration index (SPEI) at different timescales to represent drought intensity and frequency in conjunction with global OCO-2 SIF products (GOSIF) and the normalized difference vegetation index (NDVI) to assess vegetation growth conditions. The results show that (1) between 2000 and 2020, the overall drought severity in Xinjiang exhibited a slight deterioration, particularly in northern regions (R1 and R2), with a gradual transition from short-term to long-term drought conditions. The R4 and R5 ecological regions in southern Xinjiang also displayed a slight deterioration trend; however, R5 remained relatively stable on the SPEI24 timescale. (2) The NDVI and SIF values across Xinjiang exhibited an upward trend. However, in densely vegetated areas (R1-R3), both NDVI and SIF declined, with a more pronounced decrease in SIF observed in natural forests. (3) Vegetation in northern Xinjiang showed a significantly stronger response to climate change than that in southern Xinjiang, with physiological parameters (SIF) being more sensitive than structural parameters (NDVI). The R1, R2, and R3 ecological regions were primarily influenced by long-term climate change, whereas the R4 and R5 regions were more affected by short-term climate change. Natural grasslands showed a significantly stronger response than forests, particularly in areas with lower vegetation cover that are more structurally impacted. This study provides an important scientific basis for ecological management and climate adaptation in Xinjiang, emphasizing the need for differentiated strategies across ecological regions to support sustainable development.
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页数:25
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