Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/113185
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dc.contributorDepartment of Land Surveying and Geo-Informatics-
dc.creatorMukhtar, H-
dc.creatorYang, Y-
dc.creatorXu, M-
dc.creatorWu, J-
dc.creatorAbbas, S-
dc.creatorWei, D-
dc.creatorZhao, W-
dc.date.accessioned2025-05-29T07:59:08Z-
dc.date.available2025-05-29T07:59:08Z-
dc.identifier.issn0094-8276-
dc.identifier.urihttp://hdl.handle.net/10397/113185-
dc.language.isoenen_US
dc.publisherWiley-Blackwell Publishing, Inc.en_US
dc.rights© 2025. The Author(s).en_US
dc.rightsThis is an open access article under the terms of the Creative Commons Attribution-NonCommercial-NoDerivs License (http://creativecommons.org/licenses/by-nc-nd/4.0/), which permits use and distribution in any medium, provided the original work is properly cited, the use is non-commercial and no modifications or adaptations are made.en_US
dc.rightsThe following publication Mukhtar, H., Yang, Y., Xu, M., Wu, J., Abbas, S., Wei, D., & Zhao, W. (2025). Elevation-dependent vegetation greening and its responses to climate changes in the south slope of the Himalayas. Geophysical Research Letters, 52, e2024GL113276 is available at https://doi.org/10.1029/2024GL113276.en_US
dc.titleElevation-dependent vegetation greening and its responses to climate changes in the South Slope of the Himalayasen_US
dc.typeJournal/Magazine Articleen_US
dc.identifier.volume52-
dc.identifier.issue4-
dc.identifier.doi10.1029/2024GL113276-
dcterms.abstractThe South Slope of the Himalayas (SSH) is witnessing dynamic shifts in vegetation greenness driven by climatic conditions across elevation variability. Here, we analyzed greening patterns of natural vegetated surfaces along the elevational gradient and examined their connection to climate changes from 2000 to 2022. Over 50% area of SSH exhibited significant greening, with higher rates in Central Himalayas (CH) and Western Himalayas (WH) compared to Eastern Himalayas (EH). The relative change rate (RCR) showed a notable increasing vegetation greenness from ∼2,600 to ∼5,000 m, followed by a decreasing trend in all subregions. Results showed that air temperature promoted the vegetation greening significantly in the high mountains but caused heat stress in lowlands of CH and WH. Precipitation supported growth in the middle mountains across the region except EH, which faced waterlogging stress. These findings are valuable for understanding vegetation changes under future climate changes and advancing our knowledge of ecosystem responses.-
dcterms.accessRightsopen accessen_US
dcterms.bibliographicCitationGeophysical research letters, 28 Feb. 2025, v. 52, no. 4, e2024GL113276-
dcterms.isPartOfGeophysical research letters-
dcterms.issued2025-02-28-
dc.identifier.scopus2-s2.0-85218977193-
dc.identifier.eissn1944-8007-
dc.identifier.artne2024GL113276-
dc.description.validate202505 bcch-
dc.description.oaVersion of Recorden_US
dc.identifier.FolderNumberOA_Othersen_US
dc.description.fundingSourceOthersen_US
dc.description.fundingTextThe National Natural Science Foundation of China (42222109); the Science and Technology Program Project of the Tibet Autonomous Region (XZ202401ZY0060); the West Light Scholar of the Chinese Academy of Sciences (XBZG\u2010ZDSYS\u2010202202); the Science and Technology Research Program of the Institute of Mountain Hazards and Environment (IMHE\u2010CXTD\u201002)en_US
dc.description.pubStatusPublisheden_US
dc.description.oaCategoryCCen_US
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