Email this article Soil temperature in Gobi ecosystems and factors influencing its change
- Authors: Dedkov V.P.1, Kazantseva T.I.2, Gunin P.D.3, Drobyshev Y.I.3
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Affiliations:
- Immanuel Kant Baltic Federal University
- Komarov Botanical Institute
- Severtsov Institute of Ecology and Evolution
- Issue: Vol 6, No 3 (2016)
- Pages: 177-183
- Section: By the 45th Anniversary of the Russian–Mongolian Complex Biological Expedition
- URL: https://ogarev-online.ru/2079-0961/article/view/206459
- DOI: https://doi.org/10.1134/S2079096116030057
- ID: 206459
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Abstract
Data on the temperature of the underlying surface in the Gobi ecosystems (Mongolia) are presented. The role of the biotic factor in changes in the temperature of the underlying surface in the desert zone of Central Asia is shown to have grown.
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About the authors
V. P. Dedkov
Immanuel Kant Baltic Federal University
Author for correspondence.
Email: VDedkov@kantiana.ru
Russian Federation, ul. Nevskogo 14, Kaliningrad, 236041
T. I. Kazantseva
Komarov Botanical Institute
Email: VDedkov@kantiana.ru
Russian Federation, ul. Professora Popova 2, St. Petersburg, 197022
P. D. Gunin
Severtsov Institute of Ecology and Evolution
Email: VDedkov@kantiana.ru
Russian Federation, pr. Leninsky 33, Moscow, 119071
Yu. I. Drobyshev
Severtsov Institute of Ecology and Evolution
Email: VDedkov@kantiana.ru
Russian Federation, pr. Leninsky 33, Moscow, 119071
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