Emerging glacier forelands alter carbon dynamics on the Tibetan Plateau
作者机构:College of Earth and Environmental SciencesLanzhou UniversityLanzhou 730000China Key Laboratory of Cryospheric Science and Frozen Soil EngineeringNorthwest Institute of Eco-Environment and ResourcesChinese Academy of SciencesLanzhou 730000China School of Geography and Ocean SciencesNanjing UniversityNanjing 210023China Department of Environmental&Geographical ScienceUniversity of Cape TownRondebosch 7701South Africa
出 版 物:《Journal of Mountain Science》 (山地科学学报(英文))
年 卷 期:2024年第21卷第9期
页 面:2871-2875页
核心收录:
学科分类:07[理学] 070601[理学-气象学] 0705[理学-地理学] 0706[理学-大气科学] 070501[理学-自然地理学]
基 金:supported by the National Natural Science Foundation of China(42322105,42271132) Outstanding Youth Fund of Gansu Province(23JRRA612)
主 题:Glacier Climate warming Carbon release Tibetan Plateau
摘 要:The critical challenge of ongoing climate warming is resulting in glacier melting globally,a process accompanied by the formation of substantial glacier *** phenomenon emerges as a pivotal area of study,especially in the Tibetan Plateau(TP),known as the Third Pole and the Asian Water *** particular,the rapid retreat of temperate glaciers in the southeastern TP has led to the formation of expansive glacier *** forelands are not merely evidence of climate shifts but are also key areas for transformative carbon ***,the newly exposed land surface actively adjusts the balance of dissolved organic carbon,especially in meltwater,and influences the release of greenhouse gases from a range of sources including glacial lakes,subglacial sediments,and supraglacial/proglacial *** processes play a crucial role in the dynamics of atmospheric carbon *** from our intensive and detailed observations over several years,this perspective not only emphasizes the importance of the underexplored impact of glacier forelands on carbon cycles but also opens a window into understanding potential future trajectories in a warming world.