In-situ monitoring of the time evolution of the effective thermal conductivity of snow

被引:43
|
作者
Morin, S. [1 ,2 ]
Domine, F. [2 ]
Arnaud, L. [2 ]
Picard, G. [2 ]
机构
[1] Meteo France, Ctr Etud Neige, CNRS, CNRM GAME, F-38400 St Martin Dheres, France
[2] Univ Grenoble 1, CNRS, LGGE, F-38400 St Martin Dheres, France
关键词
Thermal conductivity; Snow; Heated-needle probe; SEASONAL SNOW; MODEL; MICROSTRUCTURE; COVER; HEAT; TEMPERATURE; DEPENDENCE;
D O I
10.1016/j.coldregions.2010.02.008
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
We report on a 3-month long time series of in-situ measurements of the effective thermal conductivity (keg) of snow at 6 heights in an Alpine snowpack in the Mont-Blanc mountain range, France, at an altitude of 2400 m. Measurements were carried out automatically every 2 days using heated-needle probes embedded in the snowpack. The experimental procedure used is presented in detail and demonstrates the applicability of single heated-needle probes for the evaluation of keg in snow, both for long-term measurements within the snowpack and occasional use in the field. Results based on 139 automatically collected data show k(eff) values ranging between 0.04 and 0.35 Wm(-1) K-1. and a consistent pattern of effective thermal conductivity increase throughout the measurements campaign. The temporal rate of change of keff varies up to 0.01 W m(-1) K-1 day(-1), with maximum values just after snowfall. (C) 2010 Elsevier B.V. All rights reserved.
引用
收藏
页码:73 / 80
页数:8
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