Observations of Gravity Wave Refraction and Its Causes and Consequences

Horizontal gravity wave (GW) refraction was observed around the Andes and Drake Passage during the SouthTRAC campaign. GWs interact with the background wind through refraction and dissipation. This interaction helps to drive midatmospheric circulations and slows down the polar vortex by taking GW mo...

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Published in:Journal of Geophysical Research: Atmospheres
Main Authors: Geldenhuys, Markus, Kaifler, Bernd, Preusse, Peter, Ungermann, Jurgen, Alexander, Pedro Manfredo, Krasauskas, Lukas, Rhode, Sebastian, Woiwode, Wolfgang, Ern, Manfred, Rapp, Markus, Riese, Martin
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union
Subjects:
Online Access:http://hdl.handle.net/11336/239423
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author Geldenhuys, Markus
Kaifler, Bernd
Preusse, Peter
Ungermann, Jurgen
Alexander, Pedro Manfredo
Krasauskas, Lukas
Rhode, Sebastian
Woiwode, Wolfgang
Ern, Manfred
Rapp, Markus
Riese, Martin
author_facet Geldenhuys, Markus
Kaifler, Bernd
Preusse, Peter
Ungermann, Jurgen
Alexander, Pedro Manfredo
Krasauskas, Lukas
Rhode, Sebastian
Woiwode, Wolfgang
Ern, Manfred
Rapp, Markus
Riese, Martin
author_sort Geldenhuys, Markus
collection CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas)
container_issue 3
container_title Journal of Geophysical Research: Atmospheres
container_volume 128
description Horizontal gravity wave (GW) refraction was observed around the Andes and Drake Passage during the SouthTRAC campaign. GWs interact with the background wind through refraction and dissipation. This interaction helps to drive midatmospheric circulations and slows down the polar vortex by taking GW momentum flux (GWMF) from one location to another. The SouthTRAC campaign was composed to gain improved understanding of the propagation and dissipation of GWs. This study uses observational data from this campaign collected by the German High Altitude Long Range research aircraft on 12 September 2019. During the campaign a minor sudden stratospheric warming in the southern hemisphere occurred, which heavily influenced GW propagation and refraction and thus also the location and amount of GWMF deposition. Observations include measurements from below the aircraft by Gimballed Limb Observer for Radiance Imaging of the Atmosphere and above the aircraft by Airborne Lidar for the Middle Atmosphere. Refraction is identified in two different GW packets as low as ≈4 km and as high as 58 km. One GW packet of orographic origin and one of nonorographic origin is used to investigate refraction. Observations are supplemented by the Gravity-wave Regional Or Global Ray Tracer, a simplified mountain wave model, ERA5 data and high-resolution (3 km) WRF data. Contrary to some previous studies we find that refraction makes a noteworthy contribution in the amount and the location of GWMF deposition. This case study highlights the importance of refraction and provides compelling arguments that models should account for this. Fil: Geldenhuys, Markus. Helmholtz Gemeinschaft. Forschungszentrum Jülich; Alemania. South African Weather Service; Sudáfrica Fil: Kaifler, Bernd. German Aerospace Center.; Alemania Fil: Preusse, Peter. Helmholtz Gemeinschaft. Forschungszentrum Jülich; Alemania Fil: Ungermann, Jurgen. Helmholtz Gemeinschaft. Forschungszentrum Jülich; Alemania Fil: Alexander, Pedro Manfredo. Consejo Nacional de Investigaciones ...
format Article in Journal/Newspaper
genre Drake Passage
genre_facet Drake Passage
geographic Drake Passage
geographic_facet Drake Passage
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op_doi https://doi.org/10.1029/2022JD036830
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spelling ftconicet:oai:ri.conicet.gov.ar:11336/239423 2025-01-16T21:39:47+00:00 Observations of Gravity Wave Refraction and Its Causes and Consequences Geldenhuys, Markus Kaifler, Bernd Preusse, Peter Ungermann, Jurgen Alexander, Pedro Manfredo Krasauskas, Lukas Rhode, Sebastian Woiwode, Wolfgang Ern, Manfred Rapp, Markus Riese, Martin application/pdf http://hdl.handle.net/11336/239423 eng eng American Geophysical Union info:eu-repo/semantics/altIdentifier/url/https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2022JD036830 info:eu-repo/semantics/altIdentifier/doi/10.1029/2022JD036830 http://hdl.handle.net/11336/239423 CONICET Digital CONICET info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by/2.5/ar/ GRAVITY WAVES MOMENTUM FLUX REFRACTION https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 info:eu-repo/semantics/article info:ar-repo/semantics/artículo info:eu-repo/semantics/publishedVersion ftconicet https://doi.org/10.1029/2022JD036830 2024-10-04T09:34:15Z Horizontal gravity wave (GW) refraction was observed around the Andes and Drake Passage during the SouthTRAC campaign. GWs interact with the background wind through refraction and dissipation. This interaction helps to drive midatmospheric circulations and slows down the polar vortex by taking GW momentum flux (GWMF) from one location to another. The SouthTRAC campaign was composed to gain improved understanding of the propagation and dissipation of GWs. This study uses observational data from this campaign collected by the German High Altitude Long Range research aircraft on 12 September 2019. During the campaign a minor sudden stratospheric warming in the southern hemisphere occurred, which heavily influenced GW propagation and refraction and thus also the location and amount of GWMF deposition. Observations include measurements from below the aircraft by Gimballed Limb Observer for Radiance Imaging of the Atmosphere and above the aircraft by Airborne Lidar for the Middle Atmosphere. Refraction is identified in two different GW packets as low as ≈4 km and as high as 58 km. One GW packet of orographic origin and one of nonorographic origin is used to investigate refraction. Observations are supplemented by the Gravity-wave Regional Or Global Ray Tracer, a simplified mountain wave model, ERA5 data and high-resolution (3 km) WRF data. Contrary to some previous studies we find that refraction makes a noteworthy contribution in the amount and the location of GWMF deposition. This case study highlights the importance of refraction and provides compelling arguments that models should account for this. Fil: Geldenhuys, Markus. Helmholtz Gemeinschaft. Forschungszentrum Jülich; Alemania. South African Weather Service; Sudáfrica Fil: Kaifler, Bernd. German Aerospace Center.; Alemania Fil: Preusse, Peter. Helmholtz Gemeinschaft. Forschungszentrum Jülich; Alemania Fil: Ungermann, Jurgen. Helmholtz Gemeinschaft. Forschungszentrum Jülich; Alemania Fil: Alexander, Pedro Manfredo. Consejo Nacional de Investigaciones ... Article in Journal/Newspaper Drake Passage CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) Drake Passage Journal of Geophysical Research: Atmospheres 128 3
spellingShingle GRAVITY WAVES
MOMENTUM FLUX
REFRACTION
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
Geldenhuys, Markus
Kaifler, Bernd
Preusse, Peter
Ungermann, Jurgen
Alexander, Pedro Manfredo
Krasauskas, Lukas
Rhode, Sebastian
Woiwode, Wolfgang
Ern, Manfred
Rapp, Markus
Riese, Martin
Observations of Gravity Wave Refraction and Its Causes and Consequences
title Observations of Gravity Wave Refraction and Its Causes and Consequences
title_full Observations of Gravity Wave Refraction and Its Causes and Consequences
title_fullStr Observations of Gravity Wave Refraction and Its Causes and Consequences
title_full_unstemmed Observations of Gravity Wave Refraction and Its Causes and Consequences
title_short Observations of Gravity Wave Refraction and Its Causes and Consequences
title_sort observations of gravity wave refraction and its causes and consequences
topic GRAVITY WAVES
MOMENTUM FLUX
REFRACTION
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
topic_facet GRAVITY WAVES
MOMENTUM FLUX
REFRACTION
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
url http://hdl.handle.net/11336/239423