中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Varying response of vegetation to sea ice dynamics over the Arctic

文献类型:期刊论文

作者Yu, Linfei1,3; Leng, Guoyong1,3; Python, Andre2,4
刊名SCIENCE OF THE TOTAL ENVIRONMENT
出版日期2021-12-10
卷号799页码:15
关键词Arctic Cumulative response Lagged response Sea ice dynamics Vegetation
ISSN号0048-9697
DOI10.1016/j.scitotenv.2021.149378
通讯作者Leng, Guoyong(lenggy@igsnrr.ac.cn)
英文摘要Recent reduction of sea ice may have contributed to vegetation growth over the Arctic through albedo feedback effects to atmospheric warming. Understanding the varying response of vegetation to sea ice dynamics is critical for predicting future climate change over the Arctic and middle-high latitudes. Instead of looking at the direct response characteristics, we perform a systematic analysis of the time-lag and time-cumulation responses of vegetation to sea ice dynamics, using a long-term Arctic Normalized Difference Vegetation Index (NDVI) dataset and three sea ice indices (sea ice concentration (SIC), sea ice area (SIA) and sea ice extent (SIE)) from 1982 to 2015. The results show that annual NDVI in the Arctic has exhibited a significant (p < 0.05) increase during 1982 to 2015, while a significant (p < 0.05) decrease is detected for annual SIC, SIA and SIE. The results of a regression analysis on NDVI identify a lag time of 7-months, 8-months and 9-months for vegetation response to SIC, SIA and SIE in February, March and April, respectively, while no evident lag response is observed in summer except for August. For the cumulation response, NDVI in February, March and April shows the largest response to the previous 5, 7 and 9 months of sea ice variations, respectively, while a short cumulation response of 1 to 3 months is found in summer. The differences in the spatial patterns of lagged time are usually not statistically significant in autumn and winter. A shorter lag response (1-3 month) is found in the Yamalia region in June. Further analysis suggests that vegetation response to sea ice dynamics depends on bio - climatic characteristics and soil pH, with vegetation responding faster to sea ice changes in acidic soil. This study provides observational evidences on the varying response of vegetation to sea ice dynamics over the Arctic, which has great implications for predicting vegetation-climate feedback and climate change. (c) 2021 Elsevier B.V. All rights reserved.
WOS关键词SHRUB EXPANSION ; TEMPERATURE ; IMPACTS ; DROUGHT ; ALASKA
资助项目National Key Research and Development Program of China[2020YFA0608502] ; National Natural Science Foundation of China[42077420]
WOS研究方向Environmental Sciences & Ecology
语种英语
WOS记录号WOS:000701266700009
出版者ELSEVIER
资助机构National Key Research and Development Program of China ; National Natural Science Foundation of China
源URL[http://ir.igsnrr.ac.cn/handle/311030/165948]  
专题中国科学院地理科学与资源研究所
通讯作者Leng, Guoyong
作者单位1.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
2.Univ Oxford, Big Data Inst, Oxford OX3 7LF, England
3.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Water Cycle & Related Land Surface Proc, Beijing 100101, Peoples R China
4.Zhejiang Univ, Ctr Data Sci, Hangzhou 310058, Peoples R China
推荐引用方式
GB/T 7714
Yu, Linfei,Leng, Guoyong,Python, Andre. Varying response of vegetation to sea ice dynamics over the Arctic[J]. SCIENCE OF THE TOTAL ENVIRONMENT,2021,799:15.
APA Yu, Linfei,Leng, Guoyong,&Python, Andre.(2021).Varying response of vegetation to sea ice dynamics over the Arctic.SCIENCE OF THE TOTAL ENVIRONMENT,799,15.
MLA Yu, Linfei,et al."Varying response of vegetation to sea ice dynamics over the Arctic".SCIENCE OF THE TOTAL ENVIRONMENT 799(2021):15.

入库方式: OAI收割

来源:地理科学与资源研究所

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