globalchange  > 影响、适应和脆弱性
DOI: 10.5194/tc-11-635-2017
Scopus记录号: 2-s2.0-85014290956
论文题名:
Soil moisture redistribution and its effect on inter-annual active layer temperature and thickness variations in a dry loess terrace in Adventdalen, Svalbard
作者: Schuh C; , Frampton A; , Hvidtfeldt Christiansen H
刊名: Cryosphere
ISSN: 19940416
出版年: 2017
卷: 11, 期:1
起始页码: 635
结束页码: 651
语种: 英语
英文关键词: annual variation ; crustal thickness ; data assimilation ; freeze-thaw cycle ; frozen ground ; hydrological modeling ; latent heat flux ; permafrost ; soil moisture ; soil temperature ; Adventdalen ; Arctic ; Spitsbergen ; Svalbard ; Svalbard and Jan Mayen
英文摘要: High-resolution field data for the period 2000-2014 consisting of active layer and permafrost temperature, active layer soil moisture, and thaw depth progression from the UNISCALM research site in Adventdalen, Svalbard, is combined with a physically based coupled cryotic and hydrogeological model to investigate active layer dynamics. The site is a loess-covered river terrace characterized by dry conditions with little to no summer infiltration and an unsaturated active layer. A range of soil moisture characteristic curves consistent with loess sediments is considered and their effects on ice and moisture redistribution, heat flux, energy storage through latent heat transfer, and active layer thickness is investigated and quantified based on hydro-climatic site conditions. Results show that soil moisture retention characteristics exhibit notable control on ice distribution and circulation within the active layer through cryosuction and are subject to seasonal variability and site-specific surface temperature variations. The retention characteristics also impact unfrozen water and ice content in the permafrost. Although these effects lead to differences in thaw progression rates, the resulting inter-annual variability in active layer thickness is not large. Field data analysis reveals that variations in summer degree days do not notably affect the active layer thaw depths; instead, a cumulative winter degree day index is found to more significantly control inter-annual active layer thickness variation at this site. A tendency of increasing winter temperatures is found to cause a general warming of the subsurface down to 10 m depth (0.05 to 0.26 °Cyr-1, observed and modelled) including an increasing active layer thickness (0.8 cm yr-1, observed and 0.3 to 0.8 cm yr-1, modelled) during the 14-year study period.
Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/75588
Appears in Collections:影响、适应和脆弱性
气候变化与战略

Files in This Item:

There are no files associated with this item.


作者单位: Department of Physical Geography, Stockholm University, Stockholm, Sweden; Bolin Centre for Climate Change, Stockholm University, Stockholm, Sweden; Department of Arctic Geology, University Centre in Svalbard, Longyearbyen, Norway

Recommended Citation:
Schuh C,, Frampton A,, Hvidtfeldt Christiansen H. Soil moisture redistribution and its effect on inter-annual active layer temperature and thickness variations in a dry loess terrace in Adventdalen, Svalbard[J]. Cryosphere,2017-01-01,11(1)
Service
Recommend this item
Sava as my favorate item
Show this item's statistics
Export Endnote File
Google Scholar
Similar articles in Google Scholar
[Schuh C]'s Articles
[, Frampton A]'s Articles
[, Hvidtfeldt Christiansen H]'s Articles
百度学术
Similar articles in Baidu Scholar
[Schuh C]'s Articles
[, Frampton A]'s Articles
[, Hvidtfeldt Christiansen H]'s Articles
CSDL cross search
Similar articles in CSDL Cross Search
[Schuh C]‘s Articles
[, Frampton A]‘s Articles
[, Hvidtfeldt Christiansen H]‘s Articles
Related Copyright Policies
Null
收藏/分享
所有评论 (0)
暂无评论
 

Items in IR are protected by copyright, with all rights reserved, unless otherwise indicated.