Zobrazeno 1 - 5
of 5
pro vyhledávání: '"E. D. Drozdov"'
Autor:
E. D. Drozdov, P. A. Toropov, V. K. Avilov, A. Yu. Artamonov, A. A. Polyukhov, I. V. Zheleznova, Yu. I. Yarinich
Publikováno v:
Лëд и снег, Vol 64, Iss 1, Pp 25-40 (2024)
Unique automated meteorological observations were carried out on the southern slope of Elbrus, near Pastukhov Rocks, at 4700 m a.s.l., during the 2021–2022 accumulation season. Data were obtained on air temperature, humidity, wind speed and directi
Externí odkaz:
https://doaj.org/article/9fd754fe959248018c0ad840a7e85c29
Autor:
I. I. Lavrentiev, A. M. Smirnov, P. A. Toropov, N. E. Elagina, T. D. Kiseleva, E. D. Drozdov, A. I. Degtyarev
Publikováno v:
Лëд и снег, Vol 63, Iss 4, Pp 553-557 (2024)
In June 2023, mass-balance and meteorological observations on Elbrus were expanded: monitoring of the Mikelchiran glacier on the northern slope of the volcano was added to the permanent observations on the southern slope (Garabashi glacier). Such syn
Externí odkaz:
https://doaj.org/article/c4e6a6cc18d044699f6c4e5b71fdb609
Publikováno v:
Лëд и снег, Vol 63, Iss 2, Pp 225-242 (2023)
Based on the analysis of the results of two measurement episodes in February 2021/22 and calculations using the LSM SPONSOR model, we obtained estimates of the variability of the snow surface thermal balance components and the thermal regime of the s
Externí odkaz:
https://doaj.org/article/965d8115aa194372855b0d2d539a1006
Autor:
V. Yu Bogomolov, E. D. Drozdov, E. A. Dyukarev, N. N. Voropay, A. A. Kokoreva, Victor Stepanenko, A. A. Cherkashina
Publikováno v:
IOP Conference Series: Earth and Environmental Science. 611:012022
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::193b4b7c66569aadb8fd3f82c1878491
https://doi.org/10.1088/1755-1315/611/1/012022
https://doi.org/10.1088/1755-1315/611/1/012022
Publikováno v:
IOP Conference Series: Earth and Environmental Science. 611:012012
The thermal regimes of peat and mineral soils differ significantly. Peat soils are characterized by the presence of a surface peat horizon, which is replaced by organogenic rock. The total thickness of the peat layer can reach several meters. The pea
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a269aa8bae04ea62e7051378eb11928d
https://doi.org/10.1088/1755-1315/611/1/012012
https://doi.org/10.1088/1755-1315/611/1/012012