A Spectral Rotary Analysis of Gravity Waves: An Application During One of the SOUTHTRAC Flights

Autores
de la Torre, Alejandro; Alexander, Pedro Manfredo; Marcos, Tomas; Hierro, Rodrigo Federico; Llamedo Soria, Pablo Martin; Hormaechea, José Luis; Preusse, P.; Geldenhuys, M.; Krasauskas, L.; Giez, A.; Kaifler, B.; Kaifler, N.; Rapp, M.
Año de publicación
2023
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
To understand the main orographic and non-orographic sources of gravity waves (GWs) over South America during an Experiment (Rapp et al., 2021, https://doi.org/10.1175/BAMS-D-20-0034.1), we propose the application of a rotational spectral analysis based on methods originally developed for oceanographic studies. This approach is deployed in a complex scenario of large-amplitude GWs by applying it to reanalysis data. We divide the atmospheric region of interest into two height intervals. The simulations are compared with lidar measurements during one of the flights. From the degree of polarization and the total energy of the GWs, the contribution of the upward and downward wave packets is described as a function of their vertical wavenumbers. At low levels, a larger downward energy flux is observed in a few significant harmonics, suggesting inertial GWs radiated at polar night jet levels, and below, near to a cold front. In contrast, the upward GW energy flux, per unit area, is larger than the downward flux, as expected over mountainous areas. The main sub-regions of upward GW energy flux are located above Patagonia, the Antarctic Peninsula and only some oceanic sectors. Above the sea, there are alternating sub-regions dominated by linearly polarized GWs and sectors of downward GWs. At the upper levels, the total available GW energy per unit mass is higher than at the lower levels. Regions with different degrees of polarization are distributed in elongated bands. A satisfactory comparison is made with an analysis based on the phase difference between temperature and vertical wind disturbances.
Fil: de la Torre, Alejandro. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Austral; Argentina
Fil: Alexander, Pedro Manfredo. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Física de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Física de Buenos Aires; Argentina
Fil: Marcos, Tomas. Universidad Austral; Argentina
Fil: Hierro, Rodrigo Federico. Universidad Austral; Argentina
Fil: Llamedo Soria, Pablo Martin. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Austral; Argentina
Fil: Hormaechea, José Luis. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de La Plata. Facultad de Ciencias Astronómicas y Geofísicas; Argentina
Fil: Preusse, P.. Helmholtz Gemeinschaft. Forschungszentrum Jülich; Alemania
Fil: Geldenhuys, M.. Helmholtz Gemeinschaft. Forschungszentrum Jülich; Alemania. South African Weather Service; Sudáfrica
Fil: Krasauskas, L.. Helmholtz Gemeinschaft. Forschungszentrum Jülich; Alemania
Fil: Giez, A.. Deutsches Zentrum für Luft- und Raumfahrt; Alemania
Fil: Kaifler, B.. Deutsches Zentrum für Luft- und Raumfahrt; Alemania
Fil: Kaifler, N.. Deutsches Zentrum für Luft- und Raumfahrt; Alemania
Fil: Rapp, M.. Deutsches Zentrum für Luft- und Raumfahrt; Alemania. Ludwig Maximilians Universitat; Alemania
Materia
ANTARCTIC PENINSULA
ENERGY FLUX
GRAVITY WAVES
PATAGONIA
ROTARY SPECTRUM
SOUTHTRAC
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-nd/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/219823
Acceder
id CONICETDig_aa2bd61ee01f67acce37af131384e70c
oai_identifier_str oai:ri.conicet.gov.ar:11336/219823
network_acronym_str CONICETDig
repository_id_str 3498
network_name_str CONICET Digital (CONICET)
spelling A Spectral Rotary Analysis of Gravity Waves: An Application During One of the SOUTHTRAC Flightsde la Torre, AlejandroAlexander, Pedro ManfredoMarcos, TomasHierro, Rodrigo FedericoLlamedo Soria, Pablo MartinHormaechea, José LuisPreusse, P.Geldenhuys, M.Krasauskas, L.Giez, A.Kaifler, B.Kaifler, N.Rapp, M.ANTARCTIC PENINSULAENERGY FLUXGRAVITY WAVESPATAGONIAROTARY SPECTRUMSOUTHTRAChttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1To understand the main orographic and non-orographic sources of gravity waves (GWs) over South America during an Experiment (Rapp et al., 2021, https://doi.org/10.1175/BAMS-D-20-0034.1), we propose the application of a rotational spectral analysis based on methods originally developed for oceanographic studies. This approach is deployed in a complex scenario of large-amplitude GWs by applying it to reanalysis data. We divide the atmospheric region of interest into two height intervals. The simulations are compared with lidar measurements during one of the flights. From the degree of polarization and the total energy of the GWs, the contribution of the upward and downward wave packets is described as a function of their vertical wavenumbers. At low levels, a larger downward energy flux is observed in a few significant harmonics, suggesting inertial GWs radiated at polar night jet levels, and below, near to a cold front. In contrast, the upward GW energy flux, per unit area, is larger than the downward flux, as expected over mountainous areas. The main sub-regions of upward GW energy flux are located above Patagonia, the Antarctic Peninsula and only some oceanic sectors. Above the sea, there are alternating sub-regions dominated by linearly polarized GWs and sectors of downward GWs. At the upper levels, the total available GW energy per unit mass is higher than at the lower levels. Regions with different degrees of polarization are distributed in elongated bands. A satisfactory comparison is made with an analysis based on the phase difference between temperature and vertical wind disturbances.Fil: de la Torre, Alejandro. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Austral; ArgentinaFil: Alexander, Pedro Manfredo. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Física de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Física de Buenos Aires; ArgentinaFil: Marcos, Tomas. Universidad Austral; ArgentinaFil: Hierro, Rodrigo Federico. Universidad Austral; ArgentinaFil: Llamedo Soria, Pablo Martin. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Austral; ArgentinaFil: Hormaechea, José Luis. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de La Plata. Facultad de Ciencias Astronómicas y Geofísicas; ArgentinaFil: Preusse, P.. Helmholtz Gemeinschaft. Forschungszentrum Jülich; AlemaniaFil: Geldenhuys, M.. Helmholtz Gemeinschaft. Forschungszentrum Jülich; Alemania. South African Weather Service; SudáfricaFil: Krasauskas, L.. Helmholtz Gemeinschaft. Forschungszentrum Jülich; AlemaniaFil: Giez, A.. Deutsches Zentrum für Luft- und Raumfahrt; AlemaniaFil: Kaifler, B.. Deutsches Zentrum für Luft- und Raumfahrt; AlemaniaFil: Kaifler, N.. Deutsches Zentrum für Luft- und Raumfahrt; AlemaniaFil: Rapp, M.. Deutsches Zentrum für Luft- und Raumfahrt; Alemania. Ludwig Maximilians Universitat; AlemaniaJohn Wiley & Sons2023-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/219823de la Torre, Alejandro; Alexander, Pedro Manfredo; Marcos, Tomas; Hierro, Rodrigo Federico; Llamedo Soria, Pablo Martin; et al.; A Spectral Rotary Analysis of Gravity Waves: An Application During One of the SOUTHTRAC Flights; John Wiley & Sons; Journal of Geophysical Research: Atmospheres; 128; 1; 1-2023; 1-272169-897X2169-8996CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2022JD037139info:eu-repo/semantics/altIdentifier/doi/10.1029/2022JD037139info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-nd/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-10-15T14:44:06Zoai:ri.conicet.gov.ar:11336/219823instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-10-15 14:44:06.836CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv A Spectral Rotary Analysis of Gravity Waves: An Application During One of the SOUTHTRAC Flights
title A Spectral Rotary Analysis of Gravity Waves: An Application During One of the SOUTHTRAC Flights
spellingShingle A Spectral Rotary Analysis of Gravity Waves: An Application During One of the SOUTHTRAC Flights
de la Torre, Alejandro
ANTARCTIC PENINSULA
ENERGY FLUX
GRAVITY WAVES
PATAGONIA
ROTARY SPECTRUM
SOUTHTRAC
title_short A Spectral Rotary Analysis of Gravity Waves: An Application During One of the SOUTHTRAC Flights
title_full A Spectral Rotary Analysis of Gravity Waves: An Application During One of the SOUTHTRAC Flights
title_fullStr A Spectral Rotary Analysis of Gravity Waves: An Application During One of the SOUTHTRAC Flights
title_full_unstemmed A Spectral Rotary Analysis of Gravity Waves: An Application During One of the SOUTHTRAC Flights
title_sort A Spectral Rotary Analysis of Gravity Waves: An Application During One of the SOUTHTRAC Flights
dc.creator.none.fl_str_mv de la Torre, Alejandro
Alexander, Pedro Manfredo
Marcos, Tomas
Hierro, Rodrigo Federico
Llamedo Soria, Pablo Martin
Hormaechea, José Luis
Preusse, P.
Geldenhuys, M.
Krasauskas, L.
Giez, A.
Kaifler, B.
Kaifler, N.
Rapp, M.
author de la Torre, Alejandro
author_facet de la Torre, Alejandro
Alexander, Pedro Manfredo
Marcos, Tomas
Hierro, Rodrigo Federico
Llamedo Soria, Pablo Martin
Hormaechea, José Luis
Preusse, P.
Geldenhuys, M.
Krasauskas, L.
Giez, A.
Kaifler, B.
Kaifler, N.
Rapp, M.
author_role author
author2 Alexander, Pedro Manfredo
Marcos, Tomas
Hierro, Rodrigo Federico
Llamedo Soria, Pablo Martin
Hormaechea, José Luis
Preusse, P.
Geldenhuys, M.
Krasauskas, L.
Giez, A.
Kaifler, B.
Kaifler, N.
Rapp, M.
author2_role author
author
author
author
author
author
author
author
author
author
author
author
dc.subject.none.fl_str_mv ANTARCTIC PENINSULA
ENERGY FLUX
GRAVITY WAVES
PATAGONIA
ROTARY SPECTRUM
SOUTHTRAC
topic ANTARCTIC PENINSULA
ENERGY FLUX
GRAVITY WAVES
PATAGONIA
ROTARY SPECTRUM
SOUTHTRAC
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv To understand the main orographic and non-orographic sources of gravity waves (GWs) over South America during an Experiment (Rapp et al., 2021, https://doi.org/10.1175/BAMS-D-20-0034.1), we propose the application of a rotational spectral analysis based on methods originally developed for oceanographic studies. This approach is deployed in a complex scenario of large-amplitude GWs by applying it to reanalysis data. We divide the atmospheric region of interest into two height intervals. The simulations are compared with lidar measurements during one of the flights. From the degree of polarization and the total energy of the GWs, the contribution of the upward and downward wave packets is described as a function of their vertical wavenumbers. At low levels, a larger downward energy flux is observed in a few significant harmonics, suggesting inertial GWs radiated at polar night jet levels, and below, near to a cold front. In contrast, the upward GW energy flux, per unit area, is larger than the downward flux, as expected over mountainous areas. The main sub-regions of upward GW energy flux are located above Patagonia, the Antarctic Peninsula and only some oceanic sectors. Above the sea, there are alternating sub-regions dominated by linearly polarized GWs and sectors of downward GWs. At the upper levels, the total available GW energy per unit mass is higher than at the lower levels. Regions with different degrees of polarization are distributed in elongated bands. A satisfactory comparison is made with an analysis based on the phase difference between temperature and vertical wind disturbances.
Fil: de la Torre, Alejandro. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Austral; Argentina
Fil: Alexander, Pedro Manfredo. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Física de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Física de Buenos Aires; Argentina
Fil: Marcos, Tomas. Universidad Austral; Argentina
Fil: Hierro, Rodrigo Federico. Universidad Austral; Argentina
Fil: Llamedo Soria, Pablo Martin. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Austral; Argentina
Fil: Hormaechea, José Luis. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de La Plata. Facultad de Ciencias Astronómicas y Geofísicas; Argentina
Fil: Preusse, P.. Helmholtz Gemeinschaft. Forschungszentrum Jülich; Alemania
Fil: Geldenhuys, M.. Helmholtz Gemeinschaft. Forschungszentrum Jülich; Alemania. South African Weather Service; Sudáfrica
Fil: Krasauskas, L.. Helmholtz Gemeinschaft. Forschungszentrum Jülich; Alemania
Fil: Giez, A.. Deutsches Zentrum für Luft- und Raumfahrt; Alemania
Fil: Kaifler, B.. Deutsches Zentrum für Luft- und Raumfahrt; Alemania
Fil: Kaifler, N.. Deutsches Zentrum für Luft- und Raumfahrt; Alemania
Fil: Rapp, M.. Deutsches Zentrum für Luft- und Raumfahrt; Alemania. Ludwig Maximilians Universitat; Alemania
description To understand the main orographic and non-orographic sources of gravity waves (GWs) over South America during an Experiment (Rapp et al., 2021, https://doi.org/10.1175/BAMS-D-20-0034.1), we propose the application of a rotational spectral analysis based on methods originally developed for oceanographic studies. This approach is deployed in a complex scenario of large-amplitude GWs by applying it to reanalysis data. We divide the atmospheric region of interest into two height intervals. The simulations are compared with lidar measurements during one of the flights. From the degree of polarization and the total energy of the GWs, the contribution of the upward and downward wave packets is described as a function of their vertical wavenumbers. At low levels, a larger downward energy flux is observed in a few significant harmonics, suggesting inertial GWs radiated at polar night jet levels, and below, near to a cold front. In contrast, the upward GW energy flux, per unit area, is larger than the downward flux, as expected over mountainous areas. The main sub-regions of upward GW energy flux are located above Patagonia, the Antarctic Peninsula and only some oceanic sectors. Above the sea, there are alternating sub-regions dominated by linearly polarized GWs and sectors of downward GWs. At the upper levels, the total available GW energy per unit mass is higher than at the lower levels. Regions with different degrees of polarization are distributed in elongated bands. A satisfactory comparison is made with an analysis based on the phase difference between temperature and vertical wind disturbances.
publishDate 2023
dc.date.none.fl_str_mv 2023-01
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
http://purl.org/coar/resource_type/c_6501
info:ar-repo/semantics/articulo
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/219823
de la Torre, Alejandro; Alexander, Pedro Manfredo; Marcos, Tomas; Hierro, Rodrigo Federico; Llamedo Soria, Pablo Martin; et al.; A Spectral Rotary Analysis of Gravity Waves: An Application During One of the SOUTHTRAC Flights; John Wiley & Sons; Journal of Geophysical Research: Atmospheres; 128; 1; 1-2023; 1-27
2169-897X
2169-8996
CONICET Digital
CONICET
url http://hdl.handle.net/11336/219823
identifier_str_mv de la Torre, Alejandro; Alexander, Pedro Manfredo; Marcos, Tomas; Hierro, Rodrigo Federico; Llamedo Soria, Pablo Martin; et al.; A Spectral Rotary Analysis of Gravity Waves: An Application During One of the SOUTHTRAC Flights; John Wiley & Sons; Journal of Geophysical Research: Atmospheres; 128; 1; 1-2023; 1-27
2169-897X
2169-8996
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/url/https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2022JD037139
info:eu-repo/semantics/altIdentifier/doi/10.1029/2022JD037139
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-nd/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-nd/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
dc.publisher.none.fl_str_mv John Wiley & Sons
publisher.none.fl_str_mv John Wiley & Sons
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
collection CONICET Digital (CONICET)
instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
repository.name.fl_str_mv CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas
repository.mail.fl_str_mv dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar
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score 13.22299

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