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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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 |
work_keys_str_mv |
AT nimazhapbadmaev monitoringnetworkforatmosphericandsoilparametersmeasurementsinpermafrostareaofburyatiarussianfederation AT aleksandrbazarov monitoringnetworkforatmosphericandsoilparametersmeasurementsinpermafrostareaofburyatiarussianfederation |
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