11 years of Rayleigh Lidar Observations of Gravity Wave Activity above the Southern Tip of South America
International audience Gravity wave (GW) activity is analyzed using temperature (T) data retrieved from a Rayleigh lidar at Río Gallegos, Argentina (51.6°S, 69.3°W). GW characteristics are derived from 302 nights of observations providing more than 1018 h of high‐resolution lidar data between 20 km...
Published in: | Journal of Geophysical Research: Atmospheres |
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Main Authors: | , , , , , , , , |
Other Authors: | , , , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
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HAL CCSD
2019
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Online Access: | https://insu.hal.science/insu-01960146 https://insu.hal.science/insu-01960146v1/document https://insu.hal.science/insu-01960146v1/file/2018JD028673.pdf https://doi.org/10.1029/2018JD028673 |
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Open Polar |
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Archives ouvertes de Paris-Saclay |
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ftuniparissaclay |
language |
English |
topic |
[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph] |
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[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph] Llamedo, P. Salvador, J. de La Torre, A. Quiroga, J. Alexander, P. Hierro, R. Schmidt, T. Pazmino, Andrea Quel, E. 11 years of Rayleigh Lidar Observations of Gravity Wave Activity above the Southern Tip of South America |
topic_facet |
[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph] |
description |
International audience Gravity wave (GW) activity is analyzed using temperature (T) data retrieved from a Rayleigh lidar at Río Gallegos, Argentina (51.6°S, 69.3°W). GW characteristics are derived from 302 nights of observations providing more than 1018 h of high‐resolution lidar data between 20 km and 56 km height from August 2005 to December 2015. T measurements are performed by a Differential Absorption lidar (DIAL) instrument. This lidar was the southernmost outside Antarctica until the end of 2017. Río Gallegos is an exceptional place to observe large amplitude GW. Every lidar measurement is classified according to its relative position to the polar vortex. The lidar measurements are compared with collocated Sounding of the Atmosphere using Broadband Emission Radiometry (SABER) and Global Positioning System‐Radio Occultation (GPS‐RO) data. The different instruments show different windows of the GW spectrum, providing complementary observations. In general, the geometric mean of the specific GW potential energy (PE) is larger during winter and spring than during summer and autumn. The largest geometric mean of PE is found inside the vortex and decreases monotonically at its edge, outside it and when there is no vortex. The same behavior is observed with satellite data. On average, it can be seen that lidar observations provide larger PE values than limb sounding measurements. From a Morlet continuous wavelet transform analysis, 3 distinct modes are captured from SABER and from GPS RO data at the upper and lower stratosphere, respectively. In particular, a systematic 3.5‐4 years oscillation, possibly related to El Niño–Southern Oscillation is observed. |
author2 |
Laboratorio de Investigación, Desarrollo y Transferencia de la Universidad Austral (LIDTUA) Consejo Nacional de Investigaciones Científicas y Técnicas Buenos Aires (CONICET)-Universidad Austral Centro de Investigaciones en Láseres y Aplicaciones Buenos Aires (CEILAP) Consejo Nacional de Investigaciones Científicas y Técnicas Buenos Aires (CONICET)-Instituto de Investigaciones Científicas y Técnicas para la Defensa (CITEDEF) Facultad Regional Buenos Aires (UTN-FRBA) Universidad Tecnológica Nacional Sarmiento (UTN) Universidad Nacional de la Patagonia Austral (UNPA) Instituto de Física de Buenos Aires (IFIBA) Consejo Nacional de Investigaciones Científicas y Técnicas Buenos Aires (CONICET)-Facultad de Ciencias Exactas y Naturales Buenos Aires (FCEyN) Universidad de Buenos Aires Buenos Aires (UBA)-Universidad de Buenos Aires Buenos Aires (UBA) German Research Centre for Geosciences - Helmholtz-Centre Potsdam (GFZ) STRATO - LATMOS Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS) |
format |
Article in Journal/Newspaper |
author |
Llamedo, P. Salvador, J. de La Torre, A. Quiroga, J. Alexander, P. Hierro, R. Schmidt, T. Pazmino, Andrea Quel, E. |
author_facet |
Llamedo, P. Salvador, J. de La Torre, A. Quiroga, J. Alexander, P. Hierro, R. Schmidt, T. Pazmino, Andrea Quel, E. |
author_sort |
Llamedo, P. |
title |
11 years of Rayleigh Lidar Observations of Gravity Wave Activity above the Southern Tip of South America |
title_short |
11 years of Rayleigh Lidar Observations of Gravity Wave Activity above the Southern Tip of South America |
title_full |
11 years of Rayleigh Lidar Observations of Gravity Wave Activity above the Southern Tip of South America |
title_fullStr |
11 years of Rayleigh Lidar Observations of Gravity Wave Activity above the Southern Tip of South America |
title_full_unstemmed |
11 years of Rayleigh Lidar Observations of Gravity Wave Activity above the Southern Tip of South America |
title_sort |
11 years of rayleigh lidar observations of gravity wave activity above the southern tip of south america |
publisher |
HAL CCSD |
publishDate |
2019 |
url |
https://insu.hal.science/insu-01960146 https://insu.hal.science/insu-01960146v1/document https://insu.hal.science/insu-01960146v1/file/2018JD028673.pdf https://doi.org/10.1029/2018JD028673 |
long_lat |
ENVELOPE(-67.150,-67.150,-68.133,-68.133) |
geographic |
Argentina Gallegos |
geographic_facet |
Argentina Gallegos |
genre |
Antarc* Antarctica |
genre_facet |
Antarc* Antarctica |
op_source |
ISSN: 2169-897X EISSN: 2169-8996 Journal of Geophysical Research: Atmospheres https://insu.hal.science/insu-01960146 Journal of Geophysical Research: Atmospheres, 2019, 124 (2), pp.451-467. ⟨10.1029/2018JD028673⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1029/2018JD028673 doi:10.1029/2018JD028673 |
op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1029/2018JD028673 |
container_title |
Journal of Geophysical Research: Atmospheres |
container_volume |
124 |
container_issue |
2 |
container_start_page |
451 |
op_container_end_page |
467 |
_version_ |
1812819294256365568 |
spelling |
ftuniparissaclay:oai:HAL:insu-01960146v1 2024-10-13T14:02:50+00:00 11 years of Rayleigh Lidar Observations of Gravity Wave Activity above the Southern Tip of South America Llamedo, P. Salvador, J. de La Torre, A. Quiroga, J. Alexander, P. Hierro, R. Schmidt, T. Pazmino, Andrea Quel, E. Laboratorio de Investigación, Desarrollo y Transferencia de la Universidad Austral (LIDTUA) Consejo Nacional de Investigaciones Científicas y Técnicas Buenos Aires (CONICET)-Universidad Austral Centro de Investigaciones en Láseres y Aplicaciones Buenos Aires (CEILAP) Consejo Nacional de Investigaciones Científicas y Técnicas Buenos Aires (CONICET)-Instituto de Investigaciones Científicas y Técnicas para la Defensa (CITEDEF) Facultad Regional Buenos Aires (UTN-FRBA) Universidad Tecnológica Nacional Sarmiento (UTN) Universidad Nacional de la Patagonia Austral (UNPA) Instituto de Física de Buenos Aires (IFIBA) Consejo Nacional de Investigaciones Científicas y Técnicas Buenos Aires (CONICET)-Facultad de Ciencias Exactas y Naturales Buenos Aires (FCEyN) Universidad de Buenos Aires Buenos Aires (UBA)-Universidad de Buenos Aires Buenos Aires (UBA) German Research Centre for Geosciences - Helmholtz-Centre Potsdam (GFZ) STRATO - LATMOS Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS) 2019 https://insu.hal.science/insu-01960146 https://insu.hal.science/insu-01960146v1/document https://insu.hal.science/insu-01960146v1/file/2018JD028673.pdf https://doi.org/10.1029/2018JD028673 en eng HAL CCSD American Geophysical Union info:eu-repo/semantics/altIdentifier/doi/10.1029/2018JD028673 doi:10.1029/2018JD028673 info:eu-repo/semantics/OpenAccess ISSN: 2169-897X EISSN: 2169-8996 Journal of Geophysical Research: Atmospheres https://insu.hal.science/insu-01960146 Journal of Geophysical Research: Atmospheres, 2019, 124 (2), pp.451-467. ⟨10.1029/2018JD028673⟩ [PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph] info:eu-repo/semantics/article Journal articles 2019 ftuniparissaclay https://doi.org/10.1029/2018JD028673 2024-10-03T23:59:12Z International audience Gravity wave (GW) activity is analyzed using temperature (T) data retrieved from a Rayleigh lidar at Río Gallegos, Argentina (51.6°S, 69.3°W). GW characteristics are derived from 302 nights of observations providing more than 1018 h of high‐resolution lidar data between 20 km and 56 km height from August 2005 to December 2015. T measurements are performed by a Differential Absorption lidar (DIAL) instrument. This lidar was the southernmost outside Antarctica until the end of 2017. Río Gallegos is an exceptional place to observe large amplitude GW. Every lidar measurement is classified according to its relative position to the polar vortex. The lidar measurements are compared with collocated Sounding of the Atmosphere using Broadband Emission Radiometry (SABER) and Global Positioning System‐Radio Occultation (GPS‐RO) data. The different instruments show different windows of the GW spectrum, providing complementary observations. In general, the geometric mean of the specific GW potential energy (PE) is larger during winter and spring than during summer and autumn. The largest geometric mean of PE is found inside the vortex and decreases monotonically at its edge, outside it and when there is no vortex. The same behavior is observed with satellite data. On average, it can be seen that lidar observations provide larger PE values than limb sounding measurements. From a Morlet continuous wavelet transform analysis, 3 distinct modes are captured from SABER and from GPS RO data at the upper and lower stratosphere, respectively. In particular, a systematic 3.5‐4 years oscillation, possibly related to El Niño–Southern Oscillation is observed. Article in Journal/Newspaper Antarc* Antarctica Archives ouvertes de Paris-Saclay Argentina Gallegos ENVELOPE(-67.150,-67.150,-68.133,-68.133) Journal of Geophysical Research: Atmospheres 124 2 451 467 |