Monitoring Network for Atmospheric and Soil Parameters Measurements in Permafrost Area of Buryatia, Russian Federation

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....

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Main Authors: Nimazhap Badmaev, Aleksandr Bazarov
Format: Article
Language:English
Published: MDPI AG 2018-12-01
Series:Geosciences
Subjects:
Online Access:http://www.mdpi.com/2076-3263/9/1/6
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spelling doaj-2963927612fc4367b11774055efdc3382020-11-25T00:13:13ZengMDPI AGGeosciences2076-32632018-12-0191610.3390/geosciences9010006geosciences9010006Monitoring Network for Atmospheric and Soil Parameters Measurements in Permafrost Area of Buryatia, Russian FederationNimazhap Badmaev0Aleksandr Bazarov1Institute of General and Experimental Biology of the Siberian Branch, Russian Academy of Sciences, 6, Sakhyanovoy str., Ulan-Ude 670047, RussiaInstitute of Physical Material Science of the Siberian Branch, Russian Academy of Sciences, 6, Sakhyanovoy str., Ulan-Ude 670047, RussiaThe 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.http://www.mdpi.com/2076-3263/9/1/6atmosphere and soil measurement complexclimate changepermafrost typestemperature regime of soilscontrolfreezing and thawing of soils“mirror imaging”
collection DOAJ
language English
format Article
sources DOAJ
author Nimazhap Badmaev
Aleksandr Bazarov
spellingShingle Nimazhap Badmaev
Aleksandr Bazarov
Monitoring Network for Atmospheric and Soil Parameters Measurements in Permafrost Area of Buryatia, Russian Federation
Geosciences
atmosphere and soil measurement complex
climate change
permafrost types
temperature regime of soils
control
freezing and thawing of soils
“mirror imaging”
author_facet Nimazhap Badmaev
Aleksandr Bazarov
author_sort Nimazhap Badmaev
title Monitoring Network for Atmospheric and Soil Parameters Measurements in Permafrost Area of Buryatia, Russian Federation
title_short Monitoring Network for Atmospheric and Soil Parameters Measurements in Permafrost Area of Buryatia, Russian Federation
title_full Monitoring Network for Atmospheric and Soil Parameters Measurements in Permafrost Area of Buryatia, Russian Federation
title_fullStr Monitoring Network for Atmospheric and Soil Parameters Measurements in Permafrost Area of Buryatia, Russian Federation
title_full_unstemmed Monitoring Network for Atmospheric and Soil Parameters Measurements in Permafrost Area of Buryatia, Russian Federation
title_sort monitoring network for atmospheric and soil parameters measurements in permafrost area of buryatia, russian federation
publisher MDPI AG
series Geosciences
issn 2076-3263
publishDate 2018-12-01
description 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.
topic atmosphere and soil measurement complex
climate change
permafrost types
temperature regime of soils
control
freezing and thawing of soils
“mirror imaging”
url http://www.mdpi.com/2076-3263/9/1/6
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