Freeze‐thaw activity and some of its geomorphic implications in the abisko mountains, Swedish Lappland
作者:
Rolf Nyberg,
期刊:
Permafrost and Periglacial Processes
(WILEY Available online 1993)
卷期:
Volume 4,
issue 1
页码: 37-47
ISSN:1045-6740
年代: 1993
DOI:10.1002/ppp.3430040104
出版商: John Wiley&Sons, Ltd
关键词: Freeze‐thaw activity;Frost shattering;Soil temperature;Solifluction;Frost creep
数据来源: WILEY
摘要:
AbstractFreeze‐thaw activity was studied at two mountain sites in Swedish Lappland, a debris‐mantled slope with small rockwalls at 1200 m altitude and a solifluction slope at 1050 m altitude. During the snow‐free period, there was a low intensity of short‐term frost cycles at the rockwall site, implying that current frost shattering of bedrock is mainly due to the annual freeze cycle. At the solifluction site, during a period with net surficial soil movements of up to 3 cm, short‐term frost cycles were absent below 0.1 m depth in the ground, suggesting a dominance of pure solifluction over frost creep. A considerable variability in near‐ground temperatures implies thatin situmeasurements, rather than meteorological screen data, are essential in assessments of frost action in high mount
点击下载:
PDF
(824KB)
返 回