Author:
Badmaev Nimazhap,Bazarov Aleksandr
Abstract
The monitoring network for the measurement of atmospheric and soil climate parameters was created at the southern boundary of the permafrost zone within the territory of the Republic of Buryatia, Russian Federation. Based on the obtained data, the processes of soil freezing and thawing were studied. Negative temperatures in cold soils occurred within 5.5–6 months, whereas the subsoil was in a thawed state most of the year. On the contrary, permafrost-affected soils were thawed for 4.5–5 months, remaining frozen in the subsoil for most of the year. We propose referring to the observed spatial–temporal differences in the temperature dynamics as the “mirror imaging” of the distribution of heat and cold (frost) in the studied soils of the permafrost zone.
Subject
General Earth and Planetary Sciences
Reference19 articles.
1. The Ecological Atlas of the Baikal Basin,2015
2. The Frozen Earth: Fundamentals of Geocryology;Williams,1989
3. Integrated Regional Changes in Arctic Climate Feedbacks: Implications for the Global Climate System
4. Global temperature change
5. Soils and Temperature Regimes of the Central Buryatia and the West Transbaikal Mountains,2009
Cited by
11 articles.
订阅此论文施引文献
订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献