DOI: 10.5194/tc-9-109-2015
Scopus记录号: 2-s2.0-84921377329
论文题名: Thermal characteristics of permafrost in the steep alpine rock walls of the Aiguille du Midi (Mont Blanc Massif, 3842 m a.s.l)
作者: Magnin F ; , Deline P ; , Ravanel L ; , Noetzli J ; , Pogliotti P
刊名: Cryosphere
ISSN: 19940416
出版年: 2015
卷: 9, 期: 1 起始页码: 109
结束页码: 121
语种: 英语
英文关键词: bedrock
; fracture network
; permafrost
; snow cover
; temperature gradient
; thawing
; Alps
; Haute Savoie
; Mont Blanc
; Savoy Alps
; Western Alps
英文摘要: Permafrost and related thermo-hydro-mechanical processes are thought to influence high alpine rock wall stability, but a lack of field measurements means that the characteristics and processes of rock wall permafrost are poorly understood. To help remedy this situation, in 2005 work began to install a monitoring system at the Aiguille du Midi (3842 m a.s.l). This paper presents temperature records from nine surface sensors (eight years of records) and three 10 m deep boreholes (4 years of records), installed at locations with different surface and bedrock characteristics. In line with previous studies, our temperature data analyses showed that: micro-meteorology controls the surface temperature, active layer thicknesses are directly related to aspect and ranged from <2 m to nearly 6 m, and that thin accumulations of snow and open fractures are cooling factors. Thermal profiles empirically demonstrated the coexistence within a single rock peak of warm and cold permafrost (about g'1.5 to g'4.5 °C at 10 m depth) and the resulting lateral heat fluxes. Our results also extended current knowledge of the effect of snow, in that we found similar thermo-insulation effects as reported for gentle mountain areas. Thick snow warms shaded areas, and may reduce active layer refreezing in winter and delay its thawing in summer. However, thick snow thermo-insulation has little effect compared to the high albedo of snow which leads to cooler conditions at the rock surface in areas exposed to the sun. A consistent inflection in the thermal profiles reflected the cooling effect of an open fracture in the bedrock, which appeared to act as a thermal cutoff in the sub-surface thermal regime. Our field data are the first to be obtained from an Alpine permafrost site where borehole temperatures are below g'4 °C, and represent a first step towards the development of strategies to investigate poorly known aspects in steep bedrock permafrost such as the effects of snow cover and fractures. © Author(s) 2015. Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/75351
Appears in Collections: 影响、适应和脆弱性 气候变化与战略
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作者单位: EDYTEM Lab, Université de Savoie, CNRS, Le Bourget-du-Lac, France; Glaciology and Geomorphodynamics Group, Department of Geography, University of Zurich, Zurich, Switzerland; ARPA Valle d'Aosta, Saint-Christophe, Italy
Recommended Citation:
Magnin F,, Deline P,, Ravanel L,et al. Thermal characteristics of permafrost in the steep alpine rock walls of the Aiguille du Midi (Mont Blanc Massif, 3842 m a.s.l)[J]. Cryosphere,2015-01-01,9(1)