Assessment of the Snow Cover Effect on Soil Surface Temperature from Observational Data
- Authors: Sherstiukov A.B.1, Anisimov O.A.2
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Affiliations:
- All-Russian Research Institute of Hydrometeorological Information–World Data Center
- State Hydrological Institute
- Issue: Vol 43, No 2 (2018)
- Pages: 72-78
- Section: Article
- URL: https://bakhtiniada.ru/1068-3739/article/view/230877
- DOI: https://doi.org/10.3103/S1068373918020024
- ID: 230877
Cite item
Abstract
A method is proposed for calculating the effective thermal conductivity of snow cover based on the data on snow surface temperature and soil temperature measured at weather stations. The quantitative estimates of the snow cover effect on soil temperature are presented. The spatial differences in this effect are described. The results obtained significantly enhance the opportunities of applying simple models to forecast permafrost conditions under the climate change.
About the authors
A. B. Sherstiukov
All-Russian Research Institute of Hydrometeorological Information–World Data Center
Author for correspondence.
Email: artem@meteo.ru
Russian Federation, ul. Koroleva 6, Obninsk, Kaluga oblast, 249035
O. A. Anisimov
State Hydrological Institute
Email: artem@meteo.ru
Russian Federation, Vtoraya liniya 23, V.O., St. Petersburg, 199053
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