Zobrazeno 1 - 10
of 29
pro vyhledávání: '"V. S. Barabanov"'
Publikováno v:
Russian Meteorology and Hydrology. 45:701-711
The response of the Black Sea upper layer to the quasitropical cyclone on September 25–29, 2005 is studied using the coupled model consisting of the WRF atmosphere model, NEMO ocean model, and OASIS coupler. The circulation arising in the sea under
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0dcc0ca775c6e0659ea4d9cb701e1006
https://doi.org/10.3103/s1068373920100040
https://doi.org/10.3103/s1068373920100040
Autor:
V. S. Barabanov, V. V. Efimov
Publikováno v:
Izvestiya, Atmospheric and Oceanic Physics. 53:343-351
Seasonal average distribution of mesoscale anomalies of the Black Sea surface temperature (SST) and features of their localization for various seasons are considered. The area of cold SST anomalies is detected in open western and central parts of the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a52823708d81f5f8d4123b5b7dadd3ef
https://doi.org/10.1134/s0001433817030057
https://doi.org/10.1134/s0001433817030057
Publikováno v:
International Journal Of Remote Sensing (0143-1161) (Taylor & Francis Ltd), 2015, Vol. 36, N. 3, P. 863-881
Several algorithms have been proposed to retrieve near-surface wind fields from C-band synthetic aperture radar (SAR) images acquired over the ocean. They mainly differ in the way they retrieve the wind direction. Conventionally, the wind direction i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b0bd3af43f9cd51835eab4a4364ae147
https://doi.org/10.1080/01431161.2014.999169
https://doi.org/10.1080/01431161.2014.999169
Autor:
V. S. Barabanov, V. V. Efimov
Publikováno v:
Russian Meteorology and Hydrology. 38:840-845
The development of the Novorossiysk bora on February 5–6, 2010 is simulated with high spatial and temporal resolution using the regional model of atmospheric circulation. Considered are typical features of the wind speed and air temperature fields.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::032354b904ddca797c548df38ac99a30
https://doi.org/10.3103/s1068373913120054
https://doi.org/10.3103/s1068373913120054
Autor:
V. S. Barabanov, V. V. Efimov
Publikováno v:
Izvestiya, Atmospheric and Oceanic Physics. 49:632-641
The development of a severe bora during the winter period near the South Coast of Crimea has been reproduced using the regional atmospheric circulation numerical model. Characteristic features of the velocity and temperature fields responsible for th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::114c56bca0b143aac3f7da9f4a7c5dae
https://doi.org/10.1134/s0001433813060066
https://doi.org/10.1134/s0001433813060066
Autor:
V. V. Efimov, V. S. Barabanov
Publikováno v:
Russian Meteorology and Hydrology. 38:171-176
The bora event observed in Novorossiysk on February 6–8, 2012 was analyzed using the WRF numerical model of regional atmospheric circulation. The main meteorological parameters are reproduced. It is demonstrated that the maximum wind speed is reach
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::91bdd222e627e3af249be3e2bd8578d9
https://doi.org/10.3103/s1068373913030059
https://doi.org/10.3103/s1068373913030059
Publikováno v:
Russian Meteorology and Hydrology. 36:590-595
The development of the sea breeze in the Crimea during the day is studied on the basis of the mesoscale atmospheric circulation modeling. It is revealed that the formation of gravity currents directed from the banks to the center of the peninsula is
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::06e9bd7c29024fef3d919ac728adbe14
https://doi.org/10.3103/s1068373911090032
https://doi.org/10.3103/s1068373911090032
Publikováno v:
Physical Oceanography. 21:153-162
For the Black-Sea region, we perform the dynamic reanalysis of the data on atmospheric circulation for the period 1958–2001 by using the HadRM3P model with a space resolution of 25 km. We estimate the mean climatic atmospheric fields of vorticity a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::99ae7e8895a3200f7f8e074c7a070e48
https://doi.org/10.1007/s11110-011-9112-8
https://doi.org/10.1007/s11110-011-9112-8
Autor:
V. V. Efimov, V. S. Barabanov
Publikováno v:
Physical Oceanography. 20:335-346
On the basis of the results of regional reanalysis of the atmospheric circulation presented with a resolution of 9 km, the process of formation of breezes is studied for the case of weak synoptic background activity in the rectilinear part of the wes
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4916a855bfe7aa58ecdf76bcc5c6284d
https://doi.org/10.1007/s11110-011-9089-3
https://doi.org/10.1007/s11110-011-9089-3
Publikováno v:
Physical Oceanography. 18:154-167
A long-living mesoscale cyclone observed over the Black Sea in September 2005 was characterized by a high wind velocity (25 m/sec) and induced an abnormal lowering of the sea-surface temperature (by more than 10°C). We performed the numerical simula
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6629eba0d622429bc910ad458ba7587e
https://doi.org/10.1007/s11110-008-9018-2
https://doi.org/10.1007/s11110-008-9018-2