Critical role of water conditions in the responses of autumn phenology of marsh wetlands to climate change on the Tibetan Plateau
The Tibetan Plateau, housing 20% of China's wetlands, plays a vital role in the regional carbon cycle. Examining the phenological dynamics of wetland vegetation in response to climate change is crucial for understanding its impact on the ecosystem. Despite this importance, the specific effects...
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| Veröffentlicht in: | Global change biology 2024-01, Vol.30 (1), p.e17097-n/a |
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| creator | Shen, Xiangjin Shen, Miaogen Wu, Chaoyang Peñuelas, Josep Ciais, Philippe Zhang, Jiaqi Freeman, Chris Palmer, Paul I. Liu, Binhui Henderson, Mark Song, Zhaoliang Sun, Shaobo Lu, Xianguo Jiang, Ming |
| description | The Tibetan Plateau, housing 20% of China's wetlands, plays a vital role in the regional carbon cycle. Examining the phenological dynamics of wetland vegetation in response to climate change is crucial for understanding its impact on the ecosystem. Despite this importance, the specific effects of climate change on wetland vegetation phenology in this region remain uncertain. In this study, we investigated the influence of climate change on the end of the growing season (EOS) of marsh wetland vegetation across the Tibetan Plateau, utilizing satellite‐derived Normalized Difference Vegetation Index (NDVI) data and observational climate data. We observed that the regionally averaged EOS of marsh vegetation across the Tibetan Plateau was significantly (p |
| doi_str_mv | 10.1111/gcb.17097 |
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This study investigated the influence of climate change on the end of the growing season (EOS) of marsh wetland vegetation across the Tibetan Plateau. The responses of EOS to climate change varied spatially across the plateau, indicating a regulatory role for hydrological conditions in marsh phenology. As soil moisture decreased, the delaying effect of increasing preseason maximum temperatures gradually weakened and even reversed, while the delaying effect of increased preseason precipitation was strengthened. Our findings underscore the importance of considering water conditions in phenology simulations conducted by terrestrial ecosystem models in cold and dry regions worldwide.</description><identifier>ISSN: 1354-1013</identifier><identifier>EISSN: 1365-2486</identifier><identifier>DOI: 10.1111/gcb.17097</identifier><identifier>PMID: 38273510</identifier><language>eng</language><publisher>England: Blackwell Publishing Ltd</publisher><subject>autumn phenology ; Carbon cycle ; Climate change ; Climate effects ; Climatic data ; Continental interfaces, environment ; Daytime ; Ecosystem models ; Environment models ; Environmental impact ; Growing season ; Hydrology ; marsh wetlands ; Marshes ; Normalized difference vegetative index ; Ocean, Atmosphere ; Phenology ; Plateaus ; Precipitation ; Rainfall ; Sciences of the Universe ; Soil ; Soil moisture ; Soil temperature ; Tibetan Plateau ; Vegetation ; water condition ; Wetlands</subject><ispartof>Global change biology, 2024-01, Vol.30 (1), p.e17097-n/a</ispartof><rights>2023 John Wiley & Sons Ltd.</rights><rights>Copyright © 2024 John Wiley & Sons Ltd.</rights><rights>Distributed under a Creative Commons Attribution 4.0 International License</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c3877-6a54f2a4803be9a824a51821ed121a95a294ffb5c5542918ea463c98d2e545583</citedby><cites>FETCH-LOGICAL-c3877-6a54f2a4803be9a824a51821ed121a95a294ffb5c5542918ea463c98d2e545583</cites><orcidid>0000-0002-7215-0150 ; 0000-0002-2967-6288 ; 0000-0001-6163-8209</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1111%2Fgcb.17097$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1111%2Fgcb.17097$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>230,314,776,780,881,1411,4010,27900,27901,27902,45550,45551</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/38273510$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink><backlink>$$Uhttps://hal.science/hal-04574832$$DView record in HAL$$Hfree_for_read</backlink></links><search><creatorcontrib>Shen, Xiangjin</creatorcontrib><creatorcontrib>Shen, Miaogen</creatorcontrib><creatorcontrib>Wu, Chaoyang</creatorcontrib><creatorcontrib>Peñuelas, Josep</creatorcontrib><creatorcontrib>Ciais, Philippe</creatorcontrib><creatorcontrib>Zhang, Jiaqi</creatorcontrib><creatorcontrib>Freeman, Chris</creatorcontrib><creatorcontrib>Palmer, Paul I.</creatorcontrib><creatorcontrib>Liu, Binhui</creatorcontrib><creatorcontrib>Henderson, Mark</creatorcontrib><creatorcontrib>Song, Zhaoliang</creatorcontrib><creatorcontrib>Sun, Shaobo</creatorcontrib><creatorcontrib>Lu, Xianguo</creatorcontrib><creatorcontrib>Jiang, Ming</creatorcontrib><title>Critical role of water conditions in the responses of autumn phenology of marsh wetlands to climate change on the Tibetan Plateau</title><title>Global change biology</title><addtitle>Glob Chang Biol</addtitle><description>The Tibetan Plateau, housing 20% of China's wetlands, plays a vital role in the regional carbon cycle. Examining the phenological dynamics of wetland vegetation in response to climate change is crucial for understanding its impact on the ecosystem. Despite this importance, the specific effects of climate change on wetland vegetation phenology in this region remain uncertain. In this study, we investigated the influence of climate change on the end of the growing season (EOS) of marsh wetland vegetation across the Tibetan Plateau, utilizing satellite‐derived Normalized Difference Vegetation Index (NDVI) data and observational climate data. We observed that the regionally averaged EOS of marsh vegetation across the Tibetan Plateau was significantly (p < .05) delayed by 4.10 days/decade from 2001 to 2020. Warming preseason temperatures were found to be the primary driver behind the delay in the EOS of marsh vegetation, whereas preseason cumulative precipitation showed no significant impact. Interestingly, the responses of EOS to climate change varied spatially across the plateau, indicating a regulatory role for hydrological conditions in marsh phenology. In the humid and cold central regions, preseason daytime warming significantly delayed the EOS. However, areas with lower soil moisture exhibited a weaker or reversed delay effect, suggesting complex interplays between temperature, soil moisture, and EOS. Notably, in the arid southwestern regions of the plateau, increased preseason rainfall directly delayed the EOS, while higher daytime temperatures advanced it. Our results emphasize the critical role of hydrological conditions, specifically soil moisture, in shaping marsh EOS responses in different regions. Our findings underscore the need to incorporate hydrological factors into terrestrial ecosystem models, particularly in cold and dry regions, for accurate predictions of marsh vegetation phenological responses to climate change. This understanding is vital for informed conservation and management strategies in the face of current and future climate challenges.
This study investigated the influence of climate change on the end of the growing season (EOS) of marsh wetland vegetation across the Tibetan Plateau. The responses of EOS to climate change varied spatially across the plateau, indicating a regulatory role for hydrological conditions in marsh phenology. As soil moisture decreased, the delaying effect of increasing preseason maximum temperatures gradually weakened and even reversed, while the delaying effect of increased preseason precipitation was strengthened. Our findings underscore the importance of considering water conditions in phenology simulations conducted by terrestrial ecosystem models in cold and dry regions worldwide.</description><subject>autumn phenology</subject><subject>Carbon cycle</subject><subject>Climate change</subject><subject>Climate effects</subject><subject>Climatic data</subject><subject>Continental interfaces, environment</subject><subject>Daytime</subject><subject>Ecosystem models</subject><subject>Environment models</subject><subject>Environmental impact</subject><subject>Growing season</subject><subject>Hydrology</subject><subject>marsh wetlands</subject><subject>Marshes</subject><subject>Normalized difference vegetative index</subject><subject>Ocean, Atmosphere</subject><subject>Phenology</subject><subject>Plateaus</subject><subject>Precipitation</subject><subject>Rainfall</subject><subject>Sciences of the Universe</subject><subject>Soil</subject><subject>Soil moisture</subject><subject>Soil temperature</subject><subject>Tibetan Plateau</subject><subject>Vegetation</subject><subject>water condition</subject><subject>Wetlands</subject><issn>1354-1013</issn><issn>1365-2486</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2024</creationdate><recordtype>article</recordtype><recordid>eNp1kU1v1DAQQC1ERUvhwB9AlriUQ1p_Js6xrKBFWqkcytlynMkmlWMvdsJqj_3nOKQUCQlfbM88vZnRIPSOkkuaz9XONpe0InX1Ap1RXsqCCVW-XN5SFJRQfopep_RACOGMlK_QKVes4pKSM_S4icM0WONwDA5w6PDBTBCxDb7NieATHjyeesAR0j5_IS2Qmad59Hjfgw8u7I5LbDQx9fgAkzO-TXgK2LphzDZse-N3Wb6K7ocGJuPxN5dzZn6DTjrjErx9us_R9y-f7ze3xfbu5uvmeltYrqqqKI0UHTNCEd5AbRQTRlLFKLSUUVNLw2rRdY20UgpWUwVGlNzWqmUghZSKn6OPq7c3Tu9j7iwedTCDvr3e6iVGhKyE4uwnzezFyu5j-DFDmvQ4JAsuTwZhTjoXqKuMlySjH_5BH8IcfZ5koRQtayX53-I2hpQidM8dUKKXHeq8Q_17h5l9_2ScmxHaZ_LP0jJwtQKHwcHx_yZ9s_m0Kn8BBcykZw</recordid><startdate>202401</startdate><enddate>202401</enddate><creator>Shen, Xiangjin</creator><creator>Shen, Miaogen</creator><creator>Wu, Chaoyang</creator><creator>Peñuelas, Josep</creator><creator>Ciais, Philippe</creator><creator>Zhang, Jiaqi</creator><creator>Freeman, Chris</creator><creator>Palmer, Paul I.</creator><creator>Liu, Binhui</creator><creator>Henderson, Mark</creator><creator>Song, Zhaoliang</creator><creator>Sun, Shaobo</creator><creator>Lu, Xianguo</creator><creator>Jiang, Ming</creator><general>Blackwell Publishing Ltd</general><general>Wiley</general><scope>NPM</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7SN</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H97</scope><scope>L.G</scope><scope>7X8</scope><scope>1XC</scope><orcidid>https://orcid.org/0000-0002-7215-0150</orcidid><orcidid>https://orcid.org/0000-0002-2967-6288</orcidid><orcidid>https://orcid.org/0000-0001-6163-8209</orcidid></search><sort><creationdate>202401</creationdate><title>Critical role of water conditions in the responses of autumn phenology of marsh wetlands to climate change on the Tibetan Plateau</title><author>Shen, Xiangjin ; Shen, Miaogen ; Wu, Chaoyang ; Peñuelas, Josep ; Ciais, Philippe ; Zhang, Jiaqi ; Freeman, Chris ; Palmer, Paul I. ; Liu, Binhui ; Henderson, Mark ; Song, Zhaoliang ; Sun, Shaobo ; Lu, Xianguo ; Jiang, Ming</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c3877-6a54f2a4803be9a824a51821ed121a95a294ffb5c5542918ea463c98d2e545583</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2024</creationdate><topic>autumn phenology</topic><topic>Carbon cycle</topic><topic>Climate change</topic><topic>Climate effects</topic><topic>Climatic data</topic><topic>Continental interfaces, environment</topic><topic>Daytime</topic><topic>Ecosystem models</topic><topic>Environment models</topic><topic>Environmental impact</topic><topic>Growing season</topic><topic>Hydrology</topic><topic>marsh wetlands</topic><topic>Marshes</topic><topic>Normalized difference vegetative index</topic><topic>Ocean, Atmosphere</topic><topic>Phenology</topic><topic>Plateaus</topic><topic>Precipitation</topic><topic>Rainfall</topic><topic>Sciences of the Universe</topic><topic>Soil</topic><topic>Soil moisture</topic><topic>Soil temperature</topic><topic>Tibetan Plateau</topic><topic>Vegetation</topic><topic>water condition</topic><topic>Wetlands</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Shen, Xiangjin</creatorcontrib><creatorcontrib>Shen, Miaogen</creatorcontrib><creatorcontrib>Wu, Chaoyang</creatorcontrib><creatorcontrib>Peñuelas, Josep</creatorcontrib><creatorcontrib>Ciais, Philippe</creatorcontrib><creatorcontrib>Zhang, Jiaqi</creatorcontrib><creatorcontrib>Freeman, Chris</creatorcontrib><creatorcontrib>Palmer, Paul I.</creatorcontrib><creatorcontrib>Liu, Binhui</creatorcontrib><creatorcontrib>Henderson, Mark</creatorcontrib><creatorcontrib>Song, Zhaoliang</creatorcontrib><creatorcontrib>Sun, Shaobo</creatorcontrib><creatorcontrib>Lu, Xianguo</creatorcontrib><creatorcontrib>Jiang, Ming</creatorcontrib><collection>PubMed</collection><collection>CrossRef</collection><collection>Ecology Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 3: Aquatic Pollution & Environmental Quality</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>MEDLINE - Academic</collection><collection>Hyper Article en Ligne (HAL)</collection><jtitle>Global change biology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Shen, Xiangjin</au><au>Shen, Miaogen</au><au>Wu, Chaoyang</au><au>Peñuelas, Josep</au><au>Ciais, Philippe</au><au>Zhang, Jiaqi</au><au>Freeman, Chris</au><au>Palmer, Paul I.</au><au>Liu, Binhui</au><au>Henderson, Mark</au><au>Song, Zhaoliang</au><au>Sun, Shaobo</au><au>Lu, Xianguo</au><au>Jiang, Ming</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Critical role of water conditions in the responses of autumn phenology of marsh wetlands to climate change on the Tibetan Plateau</atitle><jtitle>Global change biology</jtitle><addtitle>Glob Chang Biol</addtitle><date>2024-01</date><risdate>2024</risdate><volume>30</volume><issue>1</issue><spage>e17097</spage><epage>n/a</epage><pages>e17097-n/a</pages><issn>1354-1013</issn><eissn>1365-2486</eissn><abstract>The Tibetan Plateau, housing 20% of China's wetlands, plays a vital role in the regional carbon cycle. Examining the phenological dynamics of wetland vegetation in response to climate change is crucial for understanding its impact on the ecosystem. Despite this importance, the specific effects of climate change on wetland vegetation phenology in this region remain uncertain. In this study, we investigated the influence of climate change on the end of the growing season (EOS) of marsh wetland vegetation across the Tibetan Plateau, utilizing satellite‐derived Normalized Difference Vegetation Index (NDVI) data and observational climate data. We observed that the regionally averaged EOS of marsh vegetation across the Tibetan Plateau was significantly (p < .05) delayed by 4.10 days/decade from 2001 to 2020. Warming preseason temperatures were found to be the primary driver behind the delay in the EOS of marsh vegetation, whereas preseason cumulative precipitation showed no significant impact. Interestingly, the responses of EOS to climate change varied spatially across the plateau, indicating a regulatory role for hydrological conditions in marsh phenology. In the humid and cold central regions, preseason daytime warming significantly delayed the EOS. However, areas with lower soil moisture exhibited a weaker or reversed delay effect, suggesting complex interplays between temperature, soil moisture, and EOS. Notably, in the arid southwestern regions of the plateau, increased preseason rainfall directly delayed the EOS, while higher daytime temperatures advanced it. Our results emphasize the critical role of hydrological conditions, specifically soil moisture, in shaping marsh EOS responses in different regions. Our findings underscore the need to incorporate hydrological factors into terrestrial ecosystem models, particularly in cold and dry regions, for accurate predictions of marsh vegetation phenological responses to climate change. This understanding is vital for informed conservation and management strategies in the face of current and future climate challenges.
This study investigated the influence of climate change on the end of the growing season (EOS) of marsh wetland vegetation across the Tibetan Plateau. The responses of EOS to climate change varied spatially across the plateau, indicating a regulatory role for hydrological conditions in marsh phenology. As soil moisture decreased, the delaying effect of increasing preseason maximum temperatures gradually weakened and even reversed, while the delaying effect of increased preseason precipitation was strengthened. Our findings underscore the importance of considering water conditions in phenology simulations conducted by terrestrial ecosystem models in cold and dry regions worldwide.</abstract><cop>England</cop><pub>Blackwell Publishing Ltd</pub><pmid>38273510</pmid><doi>10.1111/gcb.17097</doi><tpages>15</tpages><orcidid>https://orcid.org/0000-0002-7215-0150</orcidid><orcidid>https://orcid.org/0000-0002-2967-6288</orcidid><orcidid>https://orcid.org/0000-0001-6163-8209</orcidid></addata></record> |
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| source | Wiley Online Library Journals Frontfile Complete |
| subjects | autumn phenology Carbon cycle Climate change Climate effects Climatic data Continental interfaces, environment Daytime Ecosystem models Environment models Environmental impact Growing season Hydrology marsh wetlands Marshes Normalized difference vegetative index Ocean, Atmosphere Phenology Plateaus Precipitation Rainfall Sciences of the Universe Soil Soil moisture Soil temperature Tibetan Plateau Vegetation water condition Wetlands |
| title | Critical role of water conditions in the responses of autumn phenology of marsh wetlands to climate change on the Tibetan Plateau |
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