Zobrazeno 1 - 7
of 7
pro vyhledávání: '"O. A. Razorenova"'
Publikováno v:
Springer Geology ISBN: 9783031165740
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7169c91eb425fec40e87788b3edcac6b
https://doi.org/10.1007/978-3-031-16575-7_37
https://doi.org/10.1007/978-3-031-16575-7_37
Publikováno v:
Springer Proceedings in Earth and Environmental Sciences ISBN: 9783030995034
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8bf13664b28ceaaece3c55ace8a38749
https://doi.org/10.1007/978-3-030-99504-1_21
https://doi.org/10.1007/978-3-030-99504-1_21
Autor:
O. A. Razorenova, P. A. Shabanov
Publikováno v:
Океанология. 59:521-528
Investigation of the interaction between oceanic heat fluxes and formation of the geopotential gradient fields in the middle troposphere during meridional and zonal processes has been carried out by applying linear correlation analysis. Analysis of t
Autor:
P. A. Shabanov, O. A. Razorenova
Publikováno v:
Доклады Академии наук. 487:684-690
An updated climatology of upper level frontal zones (UFZ) of the Northern Hemisphere is presented, based on a numerical analysis of geopotential gradients and the allocation of maximum gradient zones. Differences in the position of the UFZ during the
Autor:
O. A. Razorenova, P. A. Shabanov
Publikováno v:
Doklady Earth Sciences. 487:995-1001
Based on the use of an objective methodology that takes into account the local values of the geopotential gradients, the long-term average position of the upper-level frontal zones (UFZs) in the middle troposphere for the Northern Hemisphere over the
Autor:
O. A. Razorenova
Publikováno v:
Russian Meteorology and Hydrology. 41:1-9
Average long-term fields of geopotential gradients in the middle and upper troposphere and temperature gradients and geopotential Laplacian in the middle troposphere in the Northern Hemisphere in winter are analyzed. Based on the analysis of the dist
Autor:
O. A. Razorenova, P. A. Shabanov
Publikováno v:
Oceanology. 55:801-804
Interactions between oceanic heat transfer and the formation of the fields of spatial geopotential gradients in the middle troposphere has been studied using linear regressive analysis. The analysis of the spatial distribution of coefficients of corr