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Statistical analysis of gravity waves observed with the middle and upper atmosphere radar in the middle atmosphere 2. Waves propagated in different directions. / Gavrilov, N. M.

в: Journal of Geophysical Research Atmospheres, Том 102, № D12, 97JD00736, 1997, стр. 13433-13440.

Результаты исследований: Научные публикации в периодических изданияхстатьяРецензирование

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@article{c2a276dd02dd49708028a87fc6c3b647,
title = "Statistical analysis of gravity waves observed with the middle and upper atmosphere radar in the middle atmosphere 2. Waves propagated in different directions",
abstract = "The statistical method developed in the first part of the paper is applied to obtain parameters of internal gravity wave (IGW) harmonics with periods from 5 min to 6 hours propagating upward and downward, and in the direction of the mean wind and opposite to it, from the observations of motions in the middle atmosphere with the middle and upper atmosphere radar. Usually, wave amplitudes and modulus of momentum fluxes are larger for IGWs having upward energy fluxes and propagated opposite to the mean wind (eastward propagation in summer and westward propagation in winter). Most of IGWs have momentum fluxes directed to the northeast in winter and to the east in summer.",
author = "Gavrilov, {N. M.}",
year = "1997",
doi = "10.1029/97JD00736",
language = "English",
volume = "102",
pages = "13433--13440",
journal = "Journal of Geophysical Research: Biogeosciences",
issn = "0148-0227",
publisher = "American Geophysical Union",
number = "D12",

}

RIS

TY - JOUR

T1 - Statistical analysis of gravity waves observed with the middle and upper atmosphere radar in the middle atmosphere 2. Waves propagated in different directions

AU - Gavrilov, N. M.

PY - 1997

Y1 - 1997

N2 - The statistical method developed in the first part of the paper is applied to obtain parameters of internal gravity wave (IGW) harmonics with periods from 5 min to 6 hours propagating upward and downward, and in the direction of the mean wind and opposite to it, from the observations of motions in the middle atmosphere with the middle and upper atmosphere radar. Usually, wave amplitudes and modulus of momentum fluxes are larger for IGWs having upward energy fluxes and propagated opposite to the mean wind (eastward propagation in summer and westward propagation in winter). Most of IGWs have momentum fluxes directed to the northeast in winter and to the east in summer.

AB - The statistical method developed in the first part of the paper is applied to obtain parameters of internal gravity wave (IGW) harmonics with periods from 5 min to 6 hours propagating upward and downward, and in the direction of the mean wind and opposite to it, from the observations of motions in the middle atmosphere with the middle and upper atmosphere radar. Usually, wave amplitudes and modulus of momentum fluxes are larger for IGWs having upward energy fluxes and propagated opposite to the mean wind (eastward propagation in summer and westward propagation in winter). Most of IGWs have momentum fluxes directed to the northeast in winter and to the east in summer.

UR - http://www.scopus.com/inward/record.url?scp=0031391475&partnerID=8YFLogxK

U2 - 10.1029/97JD00736

DO - 10.1029/97JD00736

M3 - Article

AN - SCOPUS:0031391475

VL - 102

SP - 13433

EP - 13440

JO - Journal of Geophysical Research: Biogeosciences

JF - Journal of Geophysical Research: Biogeosciences

SN - 0148-0227

IS - D12

M1 - 97JD00736

ER -

ID: 87718884