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

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 spatiotempo...

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Main Authors: Jinrun He, Jinglong Fan, Zhentao Lv, Shengyu Li
Format: Article
Language:English
Published: MDPI AG 2025-01-01
Series:Remote Sensing
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Online Access:https://www.mdpi.com/2072-4292/17/1/152
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author Jinrun He
Jinglong Fan
Zhentao Lv
Shengyu Li
author_facet Jinrun He
Jinglong Fan
Zhentao Lv
Shengyu Li
author_sort Jinrun He
collection DOAJ
description 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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spelling doaj-art-2ee6fdbe8f754535be596284126d263e2025-01-10T13:20:25ZengMDPI AGRemote Sensing2072-42922025-01-0117115210.3390/rs17010152Response of Natural Forests and Grasslands in Xinjiang to Climate Change Based on Sun-Induced Chlorophyll FluorescenceJinrun He0Jinglong Fan1Zhentao Lv2Shengyu Li3National Engineering Technology Research Center for Desert-Oasis Ecological Construction, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, 818 South Beijing Road, Urumqi 830011, ChinaNational Engineering Technology Research Center for Desert-Oasis Ecological Construction, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, 818 South Beijing Road, Urumqi 830011, ChinaNational Engineering Technology Research Center for Desert-Oasis Ecological Construction, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, 818 South Beijing Road, Urumqi 830011, ChinaNational Engineering Technology Research Center for Desert-Oasis Ecological Construction, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, 818 South Beijing Road, Urumqi 830011, ChinaIn 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.https://www.mdpi.com/2072-4292/17/1/152sun-induced chlorophyll fluorescence (SIF)standardized precipitation evapotranspiration index (SPEI)natural forests and grasslandsclimate changespatiotemporal variation characteristics
spellingShingle Jinrun He
Jinglong Fan
Zhentao Lv
Shengyu Li
Response of Natural Forests and Grasslands in Xinjiang to Climate Change Based on Sun-Induced Chlorophyll Fluorescence
Remote Sensing
sun-induced chlorophyll fluorescence (SIF)
standardized precipitation evapotranspiration index (SPEI)
natural forests and grasslands
climate change
spatiotemporal variation characteristics
title Response of Natural Forests and Grasslands in Xinjiang to Climate Change Based on Sun-Induced Chlorophyll Fluorescence
title_full Response of Natural Forests and Grasslands in Xinjiang to Climate Change Based on Sun-Induced Chlorophyll Fluorescence
title_fullStr Response of Natural Forests and Grasslands in Xinjiang to Climate Change Based on Sun-Induced Chlorophyll Fluorescence
title_full_unstemmed Response of Natural Forests and Grasslands in Xinjiang to Climate Change Based on Sun-Induced Chlorophyll Fluorescence
title_short Response of Natural Forests and Grasslands in Xinjiang to Climate Change Based on Sun-Induced Chlorophyll Fluorescence
title_sort response of natural forests and grasslands in xinjiang to climate change based on sun induced chlorophyll fluorescence
topic sun-induced chlorophyll fluorescence (SIF)
standardized precipitation evapotranspiration index (SPEI)
natural forests and grasslands
climate change
spatiotemporal variation characteristics
url https://www.mdpi.com/2072-4292/17/1/152
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AT zhentaolv responseofnaturalforestsandgrasslandsinxinjiangtoclimatechangebasedonsuninducedchlorophyllfluorescence
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