Response of middle-taiga permafrost landscapes of Central Siberia to global warming in the late 20th and early 21st centuries

被引：1

作者：

Medvedkov, Alexey A. ^{[1
]}

机构：

[1] Lomonosov Moscow State Univ, Fac Geog, Dept World Phys Geog & Geoecol, Leninskiye Gory 1, Moscow 119991, Russia

来源：

INTERNATIONAL CONFERENCE AND EARLY CAREER SCIENTISTS SCHOOL ON ENVIRONMENTAL OBSERVATIONS, MODELLING AND INFORMATION SYSTEMS (ENVIROMIS-2016) | 2016年 / 48卷

关键词：

D O I：

10.1088/1755-1315/48/1/012009

中图分类号：

X [环境科学、安全科学];

学科分类号：

08 ; 0830 ;

摘要：

In this paper, regional features of a climatogenic response of the middle-taiga permafrost landscapes of Central Siberia, as well as corresponding transformations of the exodynamic processes, are considered. Lithological-geomorphologic and landscape-geocryological data are analyzed with large amounts of actual data and results of monitoring surveys. Specific features of an ecotone localization of middle-taiga permafrost landscapes and their typical physiognomic characteristics are described. A comprehensive investigation of representative key sites makes it possible to discover the response of different types of permafrost landscapes to regional climate warming. A rapid increase in the active layer depth, slower creep, transformations of the moving kurums, intensive solifluction, and a local replacement of solifluction by landslides-earthflows are revealed within ecotone landscapes of the cryolithozone.

引用

页数：8

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