Zobrazeno 1 - 10
of 44
pro vyhledávání: '"N. I. Osokin"'
Autor:
A. V. Sosnovsky, N. I. Osokin
Publikováno v:
Лëд и снег, Vol 63, Iss 4, Pp 558-568 (2024)
Average values of maximum snow depths (MaxSD) estimated separately under conditions of forests and fields on lowlands of Russia were compared during the past 29 years. It was found that MaxSD in the fields for the current climatic period 1991–2020
Externí odkaz:
https://doaj.org/article/b77865d7a7b94dc08faacb0c3ebd3500
Autor:
A. V. Sosnovsky, N. I. Osokin
Publikováno v:
Лëд и снег, Vol 60, Iss 3, Pp 471-480 (2020)
The purpose of the research is to evaluate the efficiency of winter sprinkling for desalination of seawater. The ice fraction in an individual drop and in a stream of drops in a free fall is estimated. At the air temperatures of −10 and −40 °C,
Externí odkaz:
https://doaj.org/article/8c82c6406f4d4652bece316e7c11b48e
Publikováno v:
Лëд и снег, Vol 60, Iss 2, Pp 201-212 (2020)
Results of modeling of the dynamics of the seasonally thawing layer in the twenty first century made for two polar points (the Svalbard Archipelago and the Antarctic Peninsula) are discussed in the paper. The loss of thermal stability of a permafrost
Externí odkaz:
https://doaj.org/article/9e01cfec8a114261a83d7ba6f17998ab
Autor:
A. V. Sosnovsky, N. I. Osokin
Publikováno v:
Лëд и снег, Vol 59, Iss 4, Pp 475-482 (2019)
Thaw and liquid precipitation retard cooling of snow cover and soil surface and so may be a factor of heating. This slows down the soil freezing due to more active freezing of the wet snow, and, thus, promotes cooling and re-cooling of the soil. Howe
Externí odkaz:
https://doaj.org/article/4cf64d3393f94d828ed00c358cc736a3
Publikováno v:
Лëд и снег, Vol 59, Iss 1, Pp 59-66 (2019)
Due to climatic changes in Spitsbergen the glaciation of the Nordenskjold Land (West Spitsbergen) has significantly degraded over the past 100 years. Changes in glaciers are undoubtedly associated with intensive melting caused by a rise of summer air
Externí odkaz:
https://doaj.org/article/2be3db233c2c4e59ba9f608ff9be3763
Publikováno v:
Лëд и снег, Vol 58, Iss 3, Pp 353-358 (2018)
The study was carried out to estimate the spatial variability of snow cover depths in avalanche centers of the mountain slopes of Svalbard. Accounting for the variability is necessary for monitoring the snow cover depths in the avalanche centers and
Externí odkaz:
https://doaj.org/article/924311acf3364d6a9f18a00a64678be8
Publikováno v:
Лëд и снег, Vol 58, Iss 3, Pp 343-352 (2018)
The results of experimental investigation of thermal conductivity of snow on the Svalbard archipelago in the conditions of natural occurrence are considered. The observations were carried out in the spring of 2013–2015 in the vicinity of the meteor
Externí odkaz:
https://doaj.org/article/cc6a5cc17940442bb2cfb35671363c01
Publikováno v:
Лëд и снег, Vol 58, Iss 2, Pp 183-190 (2018)
In 1966-2010, snow surveys were simultaneously performed in forests and fields on the Russian plain territory. This made it possible to analyze characteristics of snow storages on fields and in forests as well as a dynamics of them under the present-
Externí odkaz:
https://doaj.org/article/35276d2955204430ba067531b688ee8c
SNOW THICKNESS ON AUSTRE GRØNFJORDBREEN, SVALBARD, FROM RADAR MEASUREMENTS AND STANDARD SNOW SURVEYS
Autor:
I. I. Lavrentiev, S. S. Kutuzov, A. F. Glazovsky, Yu. Ya. Macheret, N. I. Osokin, A. V. Sosnovsky, R. А. Chernov, G. A. Cherniakov
Publikováno v:
Лëд и снег, Vol 58, Iss 1, Pp 5-20 (2018)
Summary Comparison of two methods of measurements of snow cover thickness on the glacier Austre Grønfjordbreen, Svalbard was performed in the spring of 2014. These methods were the radar (500 MHz) observations and standard snow surveys. Measurements
Externí odkaz:
https://doaj.org/article/311db9b11c8c4453ab49458f32e5dc20
Autor:
N. I. Osokin, A. V. Sosnovsky
Publikováno v:
Лëд и снег, Vol 56, Iss 2, Pp 189-198 (2016)
Climate variations result in changes of the snow cover characteristics which have a certain influence upon thermal state and stability of permafrost. Analysis of data of meteorological station Barentsburg (Svalbard) and our own observations has revea
Externí odkaz:
https://doaj.org/article/21c4897e6c0444ff823f33982d7f8574