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CHISLENNOE ISSLEDOVANIE VERTLKAL'NOI STRUKTURY VNUTRENNIKH GRAVITATSIONNYKH VOLN OT TROPOSFERNYKH ISTOCHNIKOV. / Gavrilov, N. M.; Yudin, V. A.

In: Izvestia Akademii nauk SSSR. Fizika atmosfery i okeana, Vol. 22, No. 6, 06.1986, p. 563-572.

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

Harvard

Gavrilov, NM & Yudin, VA 1986, 'CHISLENNOE ISSLEDOVANIE VERTLKAL'NOI STRUKTURY VNUTRENNIKH GRAVITATSIONNYKH VOLN OT TROPOSFERNYKH ISTOCHNIKOV.', Izvestia Akademii nauk SSSR. Fizika atmosfery i okeana, vol. 22, no. 6, pp. 563-572.

APA

Gavrilov, N. M., & Yudin, V. A. (1986). CHISLENNOE ISSLEDOVANIE VERTLKAL'NOI STRUKTURY VNUTRENNIKH GRAVITATSIONNYKH VOLN OT TROPOSFERNYKH ISTOCHNIKOV. Izvestia Akademii nauk SSSR. Fizika atmosfery i okeana, 22(6), 563-572.

Vancouver

Gavrilov NM, Yudin VA. CHISLENNOE ISSLEDOVANIE VERTLKAL'NOI STRUKTURY VNUTRENNIKH GRAVITATSIONNYKH VOLN OT TROPOSFERNYKH ISTOCHNIKOV. Izvestia Akademii nauk SSSR. Fizika atmosfery i okeana. 1986 Jun;22(6):563-572.

Author

Gavrilov, N. M. ; Yudin, V. A. / CHISLENNOE ISSLEDOVANIE VERTLKAL'NOI STRUKTURY VNUTRENNIKH GRAVITATSIONNYKH VOLN OT TROPOSFERNYKH ISTOCHNIKOV. In: Izvestia Akademii nauk SSSR. Fizika atmosfery i okeana. 1986 ; Vol. 22, No. 6. pp. 563-572.

BibTeX

@article{c0066d7c84a444b2a93ab62663b5859e,
title = "CHISLENNOE ISSLEDOVANIE VERTLKAL'NOI STRUKTURY VNUTRENNIKH GRAVITATSIONNYKH VOLN OT TROPOSFERNYKH ISTOCHNIKOV.",
abstract = "The results of numerical calculations of the propagation of internal gravity waves (IGW) in a plane dissipative atmosphere with temperature and wind profiles are presented. The IGW are excited by a source at a height of 10 km in the troposphere. It is shown that a steady wave regime sets in within several tens of wave periods after the source in 'switched on. ' It is noted that when the jet stream is traveling at a moderate velocity in the stratosphere, it intensifies the IGW propagating counter to the jet (westward in winter and eastward in summer). When the jet stream is traveling at a high velocity a strong reflection of the oncoming IGW occurs; therefore the IGW propagating in the same direction as the stream dominate.",
author = "Gavrilov, {N. M.} and Yudin, {V. A.}",
year = "1986",
month = jun,
language = "русский",
volume = "22",
pages = "563--572",
journal = "Izvestiya, Atmospheric and Oceanic Physics",
issn = "0001-4338",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "6",

}

RIS

TY - JOUR

T1 - CHISLENNOE ISSLEDOVANIE VERTLKAL'NOI STRUKTURY VNUTRENNIKH GRAVITATSIONNYKH VOLN OT TROPOSFERNYKH ISTOCHNIKOV.

AU - Gavrilov, N. M.

AU - Yudin, V. A.

PY - 1986/6

Y1 - 1986/6

N2 - The results of numerical calculations of the propagation of internal gravity waves (IGW) in a plane dissipative atmosphere with temperature and wind profiles are presented. The IGW are excited by a source at a height of 10 km in the troposphere. It is shown that a steady wave regime sets in within several tens of wave periods after the source in 'switched on. ' It is noted that when the jet stream is traveling at a moderate velocity in the stratosphere, it intensifies the IGW propagating counter to the jet (westward in winter and eastward in summer). When the jet stream is traveling at a high velocity a strong reflection of the oncoming IGW occurs; therefore the IGW propagating in the same direction as the stream dominate.

AB - The results of numerical calculations of the propagation of internal gravity waves (IGW) in a plane dissipative atmosphere with temperature and wind profiles are presented. The IGW are excited by a source at a height of 10 km in the troposphere. It is shown that a steady wave regime sets in within several tens of wave periods after the source in 'switched on. ' It is noted that when the jet stream is traveling at a moderate velocity in the stratosphere, it intensifies the IGW propagating counter to the jet (westward in winter and eastward in summer). When the jet stream is traveling at a high velocity a strong reflection of the oncoming IGW occurs; therefore the IGW propagating in the same direction as the stream dominate.

UR - http://www.scopus.com/inward/record.url?scp=0022728409&partnerID=8YFLogxK

M3 - статья

AN - SCOPUS:0022728409

VL - 22

SP - 563

EP - 572

JO - Izvestiya, Atmospheric and Oceanic Physics

JF - Izvestiya, Atmospheric and Oceanic Physics

SN - 0001-4338

IS - 6

ER -

ID: 87735164