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POTOKI ENERGII, TEPLA, IMPUL'SA I MASSY, SOZDAVAEMYE GRAVITATSIONNYMI VOLNAMI V METEORNOJ ZONE. / Gavrilov, N. M.; Kalov, E. D.

In: Izvestia Akademii nauk SSSR. Fizika atmosfery i okeana, Vol. 22, No. 3, 03.1986, p. 227-235.

Research output: Contribution to journal › Article › peer-review

Harvard

Gavrilov, NM & Kalov, ED 1986, 'POTOKI ENERGII, TEPLA, IMPUL'SA I MASSY, SOZDAVAEMYE GRAVITATSIONNYMI VOLNAMI V METEORNOJ ZONE.', Izvestia Akademii nauk SSSR. Fizika atmosfery i okeana, vol. 22, no. 3, pp. 227-235.

APA

Gavrilov, N. M., & Kalov, E. D. (1986). POTOKI ENERGII, TEPLA, IMPUL'SA I MASSY, SOZDAVAEMYE GRAVITATSIONNYMI VOLNAMI V METEORNOJ ZONE. Izvestia Akademii nauk SSSR. Fizika atmosfery i okeana, 22(3), 227-235.

Vancouver

Gavrilov NM, Kalov ED. POTOKI ENERGII, TEPLA, IMPUL'SA I MASSY, SOZDAVAEMYE GRAVITATSIONNYMI VOLNAMI V METEORNOJ ZONE. Izvestia Akademii nauk SSSR. Fizika atmosfery i okeana. 1986 Mar;22(3):227-235.

Author

Gavrilov, N. M. ; Kalov, E. D. / POTOKI ENERGII, TEPLA, IMPUL'SA I MASSY, SOZDAVAEMYE GRAVITATSIONNYMI VOLNAMI V METEORNOJ ZONE. In: Izvestia Akademii nauk SSSR. Fizika atmosfery i okeana. 1986 ; Vol. 22, No. 3. pp. 227-235.

BibTeX

@article{3d78b3125e9c40b0bae6acbfadc87c23,
title = "POTOKI ENERGII, TEPLA, IMPUL'SA I MASSY, SOZDAVAEMYE GRAVITATSIONNYMI VOLNAMI V METEORNOJ ZONE.",
abstract = "The results of calculations wave fluxes from radio meteor observations at Obninsk in 1979-1980 are presented. The vertical wave energy flux varies from 6 multiplied by 10** minus **3 W multiplied by m** minus **2 in winter to 1 multiplied by 10** minus **3 W multiplied by m** minus **2 in summer. The vertical mass flux corresponds to a rise at rates of 1 to 4 cm multiplied by (times) sec** minus **1. The heat flux is always directed upwards. The values of the zonal wave acceleration in the winter amount to minus (80-100) m multiplied by sec** minus **1/day in a wasterly direction and in the summer - to plus (10-20) m multiplied by sec** minus **1/day in an easterly direction. The meridional wave acceleration amounts to plus (10-50) m multiplied by sec** minus **1/day in spring and minus (10-50) m multiplied by sec** minus **1/day in winter and summer. This experimentally confirms the existing assumptions that internal gravity waves in the upper atmosphere promote deceleration of the zonal flux and the formation of a meridional circulation.",
author = "Gavrilov, {N. M.} and Kalov, {E. D.}",
year = "1986",
month = mar,
language = "русский",
volume = "22",
pages = "227--235",
journal = "Izvestiya, Atmospheric and Oceanic Physics",
issn = "0001-4338",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "3",

}

RIS

TY - JOUR

T1 - POTOKI ENERGII, TEPLA, IMPUL'SA I MASSY, SOZDAVAEMYE GRAVITATSIONNYMI VOLNAMI V METEORNOJ ZONE.

AU - Gavrilov, N. M.

AU - Kalov, E. D.

PY - 1986/3

Y1 - 1986/3

N2 - The results of calculations wave fluxes from radio meteor observations at Obninsk in 1979-1980 are presented. The vertical wave energy flux varies from 6 multiplied by 10** minus **3 W multiplied by m** minus **2 in winter to 1 multiplied by 10** minus **3 W multiplied by m** minus **2 in summer. The vertical mass flux corresponds to a rise at rates of 1 to 4 cm multiplied by (times) sec** minus **1. The heat flux is always directed upwards. The values of the zonal wave acceleration in the winter amount to minus (80-100) m multiplied by sec** minus **1/day in a wasterly direction and in the summer - to plus (10-20) m multiplied by sec** minus **1/day in an easterly direction. The meridional wave acceleration amounts to plus (10-50) m multiplied by sec** minus **1/day in spring and minus (10-50) m multiplied by sec** minus **1/day in winter and summer. This experimentally confirms the existing assumptions that internal gravity waves in the upper atmosphere promote deceleration of the zonal flux and the formation of a meridional circulation.

AB - The results of calculations wave fluxes from radio meteor observations at Obninsk in 1979-1980 are presented. The vertical wave energy flux varies from 6 multiplied by 10** minus **3 W multiplied by m** minus **2 in winter to 1 multiplied by 10** minus **3 W multiplied by m** minus **2 in summer. The vertical mass flux corresponds to a rise at rates of 1 to 4 cm multiplied by (times) sec** minus **1. The heat flux is always directed upwards. The values of the zonal wave acceleration in the winter amount to minus (80-100) m multiplied by sec** minus **1/day in a wasterly direction and in the summer - to plus (10-20) m multiplied by sec** minus **1/day in an easterly direction. The meridional wave acceleration amounts to plus (10-50) m multiplied by sec** minus **1/day in spring and minus (10-50) m multiplied by sec** minus **1/day in winter and summer. This experimentally confirms the existing assumptions that internal gravity waves in the upper atmosphere promote deceleration of the zonal flux and the formation of a meridional circulation.

UR - http://www.scopus.com/inward/record.url?scp=0022678230&partnerID=8YFLogxK

M3 - статья

AN - SCOPUS:0022678230

VL - 22

SP - 227

EP - 235

JO - Izvestiya, Atmospheric and Oceanic Physics

JF - Izvestiya, Atmospheric and Oceanic Physics

SN - 0001-4338

IS - 3

ER -

ID: 87735269