Assessment of the Snow Cover Effect on Soil Surface Temperature from Observational Data
- Авторы: Sherstiukov A.B.1, Anisimov O.A.2
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Учреждения:
- All-Russian Research Institute of Hydrometeorological Information–World Data Center
- State Hydrological Institute
- Выпуск: Том 43, № 2 (2018)
- Страницы: 72-78
- Раздел: Article
- URL: https://journals.rcsi.science/1068-3739/article/view/230877
- DOI: https://doi.org/10.3103/S1068373918020024
- ID: 230877
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Аннотация
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.
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Об авторах
A. Sherstiukov
All-Russian Research Institute of Hydrometeorological Information–World Data Center
Автор, ответственный за переписку.
Email: artem@meteo.ru
Россия, ul. Koroleva 6, Obninsk, Kaluga oblast, 249035
O. Anisimov
State Hydrological Institute
Email: artem@meteo.ru
Россия, Vtoraya liniya 23, V.O., St. Petersburg, 199053
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