Standard

Spatial inhomogeneity in the wind-driven wave field as an indicator of flow velocity in ocean frontal zones. / Lavrenov, I. V.; Belonenko, T. V.; Sharikov, Y. D.

в: Izvestiya - USSR Academy of Sciences, Atmospheric and Oceanic Physics, Том 28, № 2, 01.01.1992, стр. 141-148.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Lavrenov, IV, Belonenko, TV & Sharikov, YD 1992, 'Spatial inhomogeneity in the wind-driven wave field as an indicator of flow velocity in ocean frontal zones', Izvestiya - USSR Academy of Sciences, Atmospheric and Oceanic Physics, Том. 28, № 2, стр. 141-148.

APA

Lavrenov, I. V., Belonenko, T. V., & Sharikov, Y. D. (1992). Spatial inhomogeneity in the wind-driven wave field as an indicator of flow velocity in ocean frontal zones. Izvestiya - USSR Academy of Sciences, Atmospheric and Oceanic Physics, 28(2), 141-148.

Vancouver

Lavrenov IV, Belonenko TV, Sharikov YD. Spatial inhomogeneity in the wind-driven wave field as an indicator of flow velocity in ocean frontal zones. Izvestiya - USSR Academy of Sciences, Atmospheric and Oceanic Physics. 1992 Янв. 1;28(2):141-148.

Author

Lavrenov, I. V. ; Belonenko, T. V. ; Sharikov, Y. D. / Spatial inhomogeneity in the wind-driven wave field as an indicator of flow velocity in ocean frontal zones. в: Izvestiya - USSR Academy of Sciences, Atmospheric and Oceanic Physics. 1992 ; Том 28, № 2. стр. 141-148.

BibTeX

@article{dfd53945ce2c4986a29baaff23b97fd4,
title = "Spatial inhomogeneity in the wind-driven wave field as an indicator of flow velocity in ocean frontal zones",
abstract = "Aerial survey data are used to reconstruct the flow velocities and slope spectra for an agitated surface in the region of a frontal zone characterized by large horizontal flow velocity gradients. By means of the spectral equation for wave action balance in the collision-free approximation, the spatial inhomogeneity in the wind-wave field is calculated at the boundary between the two flows simulating a frontal zone. In this case, quantitative agreement is obtained between the calculated and observed positions for the spectral maxima, and qualitative agreement is obtained between the shapes of the spectra. -from Authors",
author = "Lavrenov, {I. V.} and Belonenko, {T. V.} and Sharikov, {Y. D.}",
year = "1992",
month = jan,
day = "1",
language = "English",
volume = "28",
pages = "141--148",
journal = "Izvestiya - Atmospheric and Oceanic Physics",
issn = "0001-4338",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "2",

}

RIS

TY - JOUR

T1 - Spatial inhomogeneity in the wind-driven wave field as an indicator of flow velocity in ocean frontal zones

AU - Lavrenov, I. V.

AU - Belonenko, T. V.

AU - Sharikov, Y. D.

PY - 1992/1/1

Y1 - 1992/1/1

N2 - Aerial survey data are used to reconstruct the flow velocities and slope spectra for an agitated surface in the region of a frontal zone characterized by large horizontal flow velocity gradients. By means of the spectral equation for wave action balance in the collision-free approximation, the spatial inhomogeneity in the wind-wave field is calculated at the boundary between the two flows simulating a frontal zone. In this case, quantitative agreement is obtained between the calculated and observed positions for the spectral maxima, and qualitative agreement is obtained between the shapes of the spectra. -from Authors

AB - Aerial survey data are used to reconstruct the flow velocities and slope spectra for an agitated surface in the region of a frontal zone characterized by large horizontal flow velocity gradients. By means of the spectral equation for wave action balance in the collision-free approximation, the spatial inhomogeneity in the wind-wave field is calculated at the boundary between the two flows simulating a frontal zone. In this case, quantitative agreement is obtained between the calculated and observed positions for the spectral maxima, and qualitative agreement is obtained between the shapes of the spectra. -from Authors

UR - http://www.scopus.com/inward/record.url?scp=0027088860&partnerID=8YFLogxK

M3 - Article

AN - SCOPUS:0027088860

VL - 28

SP - 141

EP - 148

JO - Izvestiya - Atmospheric and Oceanic Physics

JF - Izvestiya - Atmospheric and Oceanic Physics

SN - 0001-4338

IS - 2

ER -

ID: 49609875