DOI: 10.1016/j.gloplacha.2013.02.002
论文题名: Forest buffers soil temperature and postpones soil thaw as indicated by a three-year large-scale soil temperature monitoring in the forest-steppe ecotone in Inner Asia
作者: Hu G. ; Liu H. ; Anenkhonov O.A. ; Korolyuk A.Y. ; Sandanov D.V. ; Guo D.
刊名: Global and Planetary Change
ISSN: 0921-8312
出版年: 2013
卷: 104 起始页码: 1
结束页码: 6
语种: 英语
英文关键词: Forest-steppe ecotone
; Northern China
; Soil freeze and thaw
; Soil temperature
; Southern Siberia
Scopus关键词: Automatic record
; Biotic process
; Buffering effect
; Cold season
; Forest buffer
; Forest soils
; Forest-steppe ecotone
; High Latitudes
; Impacted soil
; Northern China
; Northern Hemispheres
; Positive correlations
; Regional scale
; SIBERIA
; Snowmelt
; Soil freezing
; Soil hydrological
; Soil temperature
; Soil thawing
; Vegetation cover
; Warm seasons
; Forestry
; Soil mechanics
; Soils
; Thawing
; Temperature
; drought stress
; ecotone
; forest ecosystem
; freeze-thaw cycle
; freezing
; infiltration
; monitoring
; Northern Hemisphere
; snowmelt
; soil temperature
; soil water
; steppe
; thawing
; vegetation cover
; China
; Freezing
; Siberia
; Soil
; Temperature
; Thawing
; China
; Siberia
英文摘要: Increases in soil temperature affect both soil biotic process and the soil hydrological cycle in the mid and high latitudes of the Northern Hemisphere. Using a three-year automatic record of soil temperature in paired forest and steppe plots along a temperature gradient from northern China to southern Siberia in Russia, collected from 2008-2011, we investigated how vegetation cover has impacted soil temperature at a regional scale, with focus on soil freezing/thawing timing. We found that there was a buffering effect of forests on soil temperature, as indicated by cooler soil temperatures in the warm season and warmer soil temperatures in the cold season. Forest soil thawed about 15. days later than steppe soil at the same site. At a regional scale, the onset date of soil freezing showed significant positive correlation with cold season soil temperature in both forest and steppe. The onset date of soil thawing was significantly negatively correlated with cold season mean daily soil temperature (DST) in the steppe, but showed no significant correlation in the forest. In terms of space-for-time-substitution, it could be implied that forest might face an increased likelihood of drought by impeding snowmelt infiltration, under the present warming trend in soil temperature. © 2013 Elsevier B.V. URL: https://www.scopus.com/inward/record.uri?eid=2-s2.0-84874798369&doi=10.1016%2fj.gloplacha.2013.02.002&partnerID=40&md5=0ae7dc884a72ce4f664aef3702db2c2f
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/11218
Appears in Collections: 全球变化的国际研究计划
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作者单位: Department of Ecology, College of Urban and Environmental Sciences, Peking University, Beijing 100871, China
Recommended Citation:
Hu G.,Liu H.,Anenkhonov O.A.,et al. Forest buffers soil temperature and postpones soil thaw as indicated by a three-year large-scale soil temperature monitoring in the forest-steppe ecotone in Inner Asia[J]. Global and Planetary Change,2013-01-01,104.