Monitoring of soil temperature and snow cover depth in the Irkutsk Region
Long-term data (1964–2000) from weather stations within the territory of Irkutsk region are analyzed in the paper. Quantitative assessment was made of the soil temperature response at a depth of 1.6 m to the modern climate changes. The majority of cases showed the tendency of soil temperature to ris...
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| Format: | Article |
| Language: | Russian |
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Nauka
2015-04-01
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| Series: | Лëд и снег |
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| Online Access: | https://ice-snow.igras.ru/jour/article/view/148 |
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| _version_ | 1849240809463873536 |
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| author | I. E. Trofimova A. S. Balybina |
| author_facet | I. E. Trofimova A. S. Balybina |
| author_sort | I. E. Trofimova |
| collection | DOAJ |
| description | Long-term data (1964–2000) from weather stations within the territory of Irkutsk region are analyzed in the paper. Quantitative assessment was made of the soil temperature response at a depth of 1.6 m to the modern climate changes. The majority of cases showed the tendency of soil temperature to rise; however, the values of linear trends are not always statistically significant. The snow depth varies slightly. The connection of soil temperature with air temperature and snow cover depth is discussed. The local physical-geographical conditions influence on the background of sufficiently significant relations between some parameters. |
| format | Article |
| id | doaj-art-7d84d943fbd640cdac8e6449e70bb0cc |
| institution | Kabale University |
| issn | 2076-6734 2412-3765 |
| language | Russian |
| publishDate | 2015-04-01 |
| publisher | Nauka |
| record_format | Article |
| series | Лëд и снег |
| spelling | doaj-art-7d84d943fbd640cdac8e6449e70bb0cc2025-08-20T04:00:26ZrusNaukaЛëд и снег2076-67342412-37652015-04-01521626810.15356/2076-6734-2012-1-62-68142Monitoring of soil temperature and snow cover depth in the Irkutsk RegionI. E. Trofimova0A. S. Balybina1Institute of Geography, Siberian Branch of the Russian Academy of Sciences, IrkutskInstitute of Geography, Siberian Branch of the Russian Academy of Sciences, IrkutskLong-term data (1964–2000) from weather stations within the territory of Irkutsk region are analyzed in the paper. Quantitative assessment was made of the soil temperature response at a depth of 1.6 m to the modern climate changes. The majority of cases showed the tendency of soil temperature to rise; however, the values of linear trends are not always statistically significant. The snow depth varies slightly. The connection of soil temperature with air temperature and snow cover depth is discussed. The local physical-geographical conditions influence on the background of sufficiently significant relations between some parameters.https://ice-snow.igras.ru/jour/article/view/148аir temperaturelinear trendssoil temperaturesnow cover. |
| spellingShingle | I. E. Trofimova A. S. Balybina Monitoring of soil temperature and snow cover depth in the Irkutsk Region Лëд и снег аir temperature linear trends soil temperature snow cover. |
| title | Monitoring of soil temperature and snow cover depth in the Irkutsk Region |
| title_full | Monitoring of soil temperature and snow cover depth in the Irkutsk Region |
| title_fullStr | Monitoring of soil temperature and snow cover depth in the Irkutsk Region |
| title_full_unstemmed | Monitoring of soil temperature and snow cover depth in the Irkutsk Region |
| title_short | Monitoring of soil temperature and snow cover depth in the Irkutsk Region |
| title_sort | monitoring of soil temperature and snow cover depth in the irkutsk region |
| topic | аir temperature linear trends soil temperature snow cover. |
| url | https://ice-snow.igras.ru/jour/article/view/148 |
| work_keys_str_mv | AT ietrofimova monitoringofsoiltemperatureandsnowcoverdepthintheirkutskregion AT asbalybina monitoringofsoiltemperatureandsnowcoverdepthintheirkutskregion |