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DOI10.1111/geb.13214
Mountain treelines climb slowly despite rapid climate warming
Lu, Xiaoming; Liang, Eryuan; Wang, Yafeng; Babst, Flurin; Camarero, J. Julio
通讯作者Liang, ER (通讯作者)
发表日期2021
ISSN1466-822X
EISSN1466-8238
起始页码305
结束页码315
卷号30期号:1
英文摘要Aim To better understand how climate change drives altitudinal treeline dynamics at large spatial scales. Location Northern Hemisphere. Time period 1901-2018. Major taxa studied Tree species that constitute alpine treelines. Methods We conducted a meta-analysis of annual treeline shift rates at 143 sites from 38 published studies. For each site, we calculated current change rates in annual or seasonal temperatures, precipitation and drought (standardized precipitation evapotranspiration index). We then evaluated relationships between treeline shift rates, and site characteristics and climate using standard and partial correlation analyses, as well as generalized linear models. These analyses were conducted at the hemispheric scale and for two geographic subsets of subarctic (north of 60 degrees N) and temperate regions (south of 60 degrees N). Results Treelines ascended at 88.8%, remained stable at 10.5% and descended at 0.7% of the sites. The mean hemispheric shift rate (0.354 m/year) was half of what would be expected from climate warming alone. Treeline shifts were significantly faster in subarctic than temperate regions. The precipitation effect was more important than temperature for predicting treeline shift rate. In the subarctic regions, autumn precipitation mostly determined treeline shift rates. In the temperate region, warmer temperatures and higher autumn precipitation accelerated shift rates, whereas wetter springs reduced them. Autumn precipitation and winter mean minimum temperature best explained the treeline shift rates across the Northern Hemisphere. Main conclusions A combination of thermal and hydrological factors drives treeline shift rates across the Northern Hemisphere, with precipitation assuming an important modifying role of the general temperature-driven treeline ascent. Regional treeline shift rates, therefore, co-depend on drying and wetting trends, which should be considered in future estimates of global change impacts on alpine ecosystems.
关键词ROCKY-MOUNTAINSALPINE TREELINERANGE SHIFTSGROWTHTEMPERATURERECRUITMENTELEVATIONDYNAMICSVARIABILITYMOISTURE
英文关键词alpine biomes; climate trend; climate warming; Northern Hemisphere; precipitation; temperature; treeline shift rate
语种英语
WOS研究方向Environmental Sciences & Ecology ; Physical Geography
WOS类目Ecology ; Geography, Physical
WOS记录号WOS:000588719900001
来源期刊GLOBAL ECOLOGY AND BIOGEOGRAPHY
来源机构中国科学院青藏高原研究所
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/260485
推荐引用方式
GB/T 7714
Lu, Xiaoming,Liang, Eryuan,Wang, Yafeng,et al. Mountain treelines climb slowly despite rapid climate warming[J]. 中国科学院青藏高原研究所,2021,30(1).
APA Lu, Xiaoming,Liang, Eryuan,Wang, Yafeng,Babst, Flurin,&Camarero, J. Julio.(2021).Mountain treelines climb slowly despite rapid climate warming.GLOBAL ECOLOGY AND BIOGEOGRAPHY,30(1).
MLA Lu, Xiaoming,et al."Mountain treelines climb slowly despite rapid climate warming".GLOBAL ECOLOGY AND BIOGEOGRAPHY 30.1(2021).
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