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三江源多年冻土活动层厚度变化特征研究

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作为多年冻土与外界大气间水热交换的主要场所,活动层及其变化特征显著影响着地―气间水热交换、碳循环、地表及地下水文过程、地形地貌、生态系统和寒区工程建筑物安全。本文利用三江源区内多年冻土活动层厚度的实测数据,基于修正Stefan模型对三江源区多年冻土活动层厚度的空间分布特征及其未来变化趋势进行了研究,并对可能影响活动层厚度变化的因素进行了讨论。结果表明,1981-2018年,活动层厚度增大的速率达7。2 cm∙(10a)-1。未来活动层厚度仍呈现增大的趋势,增大最明显的是三江源中部地区。2006-2049年,活动层厚度以4。3 cm∙(10a)-1(RCP6。0)到6。8 cm∙(10a)-1(RCP8。5)速率增大;2050-2099年,以0。04 cm∙(10a)-1(RCP2。6)到5。6 cm∙(10a)-1(RCP8。5)速率增大,明显小于前50年的增大速率,活动层厚度增大速率变缓。对活动层厚度变化影响因素分析表明,影响最大的是年平均气温,年降水量的影响并不明显,而NDVI对活动层厚度有一定的影响。本文的结果将会对三江源区的水源涵养、气候调节和生态安全等方面产生重要影响。
Research on the variation characteristics of active layer thickness of permafrost in the Three River Source Region
The active layer,which is the primary area for permafrost and atmosphere to exchange heat and wa-ter,and its morphological changes have a significant impact on ecosystems,topography and geomorphology,surface and subsurface hydrological processes,carbon cycle,and safety of engineering structures in cold cli-mates.In this paper,the spatial distribution characteristics of active layer thickness in the Three River Source Region(TRSR)and its future changes are studied based on the modified Stefan model,and the factors that may affect the variation of active layer thickness are discussed.The results show that the thickness of active layer has been increasing at a rate of 7.2 cm∙(10a)-1 from 1981 to 2018,and will continue to increase in the future,most significantly in the central part of the TRSR.From 2006 to 2049,the active layer thickness increases at a rate of 4.3 cm∙(10a)-1(RCP6.0)to 6.8 cm∙(10a)-1(RCP8.5);from 2050 to 2099,it increases at a rate of 0.04 cm∙(10a)-1(RCP2.6)to 4.8 cm∙(10a)-1(RCP8.5),which is significantly less than the rate of increase in the pre-vious 50 years.The rate of increase in active layer thickness has slowed down.Analysis of the factors influenc-ing the variation of active layer thickness shows that the greatest influence is on mean annual air temperature,while the influence of annual precipitation is not significant,and NDVI has some influence on active layer thick-ness.This result will have an important impact on the water conservation,climate regulation,and ecological se-curity of the TRSR.

the Three River Source RegionQinghai-Xizang Plateaupermafrostclimate changeactive layer thickness

徐晓明、吴青柏

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中国科学院 西北生态环境资源研究院 冰冻圈科学与冻土工程重点实验室,甘肃 兰州 730000

中国科学院西北生态环境资源研究院 青海北麓河高原冻土工程安全国家野外科学观测研究站,甘肃 兰州 730000

三江源 青藏高原 多年冻土 气候变化 活动层

中国国家铁路集团有限公司科技研究开发计划项目

P2021G047

2024

冰川冻土
中国地理学会 中国科学院寒区旱区环境与工程研究所

冰川冻土

CSTPCD
影响因子:2.546
ISSN:1000-0240
年,卷(期):2024.46(5)