Zobrazeno 1 - 8
of 8
pro vyhledávání: '"O. I. Komarovskaya"'
Autor:
O. I. Komarovskaya, V. V. Efimov
Publikováno v:
Physical Oceanography, Vol 26, Iss 2, Pp 123-134 (2019)
Introduction. Influence of the Crimean Mountains on the wind regime in the Crimea region for different seasons and wind directions is considered. Data and methods. Data on the monthly average temperature values on the model levels of the ERA Interim
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::df00cb6c46c35aa3e8f47e26d84ed6c9
http://physical-oceanography.ru/repository/2019/2/en_201902_03.pdf
http://physical-oceanography.ru/repository/2019/2/en_201902_03.pdf
Autor:
V. V. Efimov, O. I. Komarovskaya
Publikováno v:
Izvestiya, Atmospheric and Oceanic Physics. 54:581-593
The features of bora formation in the region of Novaya Zemlya surrounded by the Barents and Kara seas, differing in hydrometeorological conditions, are considered. The annual course of average magnitude of buoyancy frequency estimation at the points
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::79f836d4d66a502eafc7ead058d2e1bc
https://doi.org/10.1134/s0001433818060051
https://doi.org/10.1134/s0001433818060051
Autor:
V. V. Efimov, O. I. Komarovskaya
Publikováno v:
Oceanology. 58:155-163
Composites of warm and cold temperature anomalies were constructed, and the distribution of the recurrence frequency of days with temperature anomalies in the four seasons of the year was evaluated based on satellite measurements data on sea surface
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c7bc73698f2a5a968a3adf8507098caa
https://doi.org/10.1134/s0001437018020030
https://doi.org/10.1134/s0001437018020030
Autor:
V. V. Efimov, O. I. Komarovskaya
Publikováno v:
Izvestiya, Atmospheric and Oceanic Physics. 54:73-85
We consider the data of an ASRI reanalysis to distinguish the properties of velocity and temperature fields in the region of Novaya Zemlya (NZ). A numerical simulation of the bora development is performed using the WRF-ARW regional model of atmospher
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::04389ed44d97d8285b5a0aa055e8b305
https://doi.org/10.1134/s000143381801005x
https://doi.org/10.1134/s000143381801005x
Autor:
O. I. Komarovskaya, V. V. Efimov
Publikováno v:
Russian Meteorology and Hydrology. 43:22-28
The development of the bora in case of strong southeastern wind in the area of Novaya Zemlya in the winter-spring of 2016 is simulated using the WRF-ARW numerical atmosphere circulation model with high spatial resolution. The features of wind speed a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::17fbffe341981afb1fbba27520e1cb1b
https://doi.org/10.3103/s106837391801003x
https://doi.org/10.3103/s106837391801003x
Publikováno v:
Physical Oceanography, Vol 26, Iss 5, Pp 361-373 (2019)
Purpose. Bora in Novorossiysk is the strong, cold, gusting northeast wind directed to the sea on a ridge slope. As the dangerous phenomenon of weather it happens in winter at the wind speed more than 30 m/s, therefore, bora cases with maximum speed a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::11c4e5783af1eb9f5a36b60dff1d0123
https://doi.org/10.22449/0233-7584-2019-5-409-422
https://doi.org/10.22449/0233-7584-2019-5-409-422
Publikováno v:
Russian Meteorology and Hydrology. 32:465-469
A method of the NCEP/NCAR reanalysis wind data recalculation using a regional atmospheric circulation model is described. A comparison of model results and satellite measurements is performed. The results of wind wave computation using the reanalysis
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::edfc7526815d99fb9e8d28a8fbc8f858
https://doi.org/10.3103/s1068373907070084
https://doi.org/10.3103/s1068373907070084
Autor:
V. G. Polnikov, O. I. Komarovskaya
Publikováno v:
Physical Oceanography. 9:383-390
On the basis of numerical solution of a kinetic equation governing non-linear wave energy redistribution over the spectrum from sourceG to sinkD, it has been found that spectra of constant flux occur in the case of anisotropic distribution of the sou
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3241fcc7ac7caeb4c84f87d54d25b504
https://doi.org/10.1007/bf02522734
https://doi.org/10.1007/bf02522734