Strongest MJO on Record Triggers Extreme Atacama Rainfall and Warmth in Antarctica

© 2019. The Authors.Tropical perturbations have been shown theoretically and observationally to excite long-range atmospheric responses in the form of Rossby wave teleconnections that result from the equator to pole gradient of planetary vorticity. An extreme teleconnection event occurred during Mar...

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Published in:Geophysical Research Letters
Main Authors: Rondanelli, R., Hatchett, B., Rutllant Costa, José, Bozkurt, D., Garreaud Salazar, René
Format: Article in Journal/Newspaper
Language:English
Published: Blackwell Publishing Ltd 2019
Subjects:
Online Access:https://doi.org/10.1029/2018GL081475
https://repositorio.uchile.cl/handle/2250/171229
id ftunivchile:oai:repositorio.uchile.cl:2250/171229
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spelling ftunivchile:oai:repositorio.uchile.cl:2250/171229 2023-05-15T13:41:41+02:00 Strongest MJO on Record Triggers Extreme Atacama Rainfall and Warmth in Antarctica Rondanelli, R. Hatchett, B. Rutllant Costa, José Bozkurt, D. Garreaud Salazar, René 2019 application/pdf https://doi.org/10.1029/2018GL081475 https://repositorio.uchile.cl/handle/2250/171229 en eng Blackwell Publishing Ltd Geophysical Research Letters, Volumen 46, Issue 6, 2019, Pages 3482-3491 19448007 00948276 doi:10.1029/2018GL081475 https://repositorio.uchile.cl/handle/2250/171229 Attribution-NonCommercial-NoDerivs 3.0 Chile http://creativecommons.org/licenses/by-nc-nd/3.0/cl/ CC-BY-NC-ND Geophysical Research Letters Antarctica atmospheric rivers climate dynamics extremes flooding Rossby waves Artículo de revista 2019 ftunivchile https://doi.org/10.1029/2018GL081475 2023-01-22T01:08:02Z © 2019. The Authors.Tropical perturbations have been shown theoretically and observationally to excite long-range atmospheric responses in the form of Rossby wave teleconnections that result from the equator to pole gradient of planetary vorticity. An extreme teleconnection event occurred during March 2015 in the Southeastern Pacific. As a result, extreme high temperatures were observed in Southwestern South America and the Antarctic Peninsula simultaneously with an extreme rainfall and flood event in the hyperarid Atacama desert. We show that the origin of these seemingly disconnected extreme events can be traced to a Rossby wave response to the strongest Madden-Julian Oscillation (MJO) on record in the tropical central Pacific. A barotropic wave number 3 to 4 perturbation with group velocity between 15 and 30 m/s is consistent with the trajectory and timing followed by the upper-level anomalies radiating away from the tropics after the MJO episode. Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula Antarctica Universidad de Chile: Repositorio académico Antarctic Antarctic Peninsula Pacific The Antarctic Geophysical Research Letters 46 6 3482 3491
institution Open Polar
collection Universidad de Chile: Repositorio académico
op_collection_id ftunivchile
language English
topic Antarctica
atmospheric rivers
climate dynamics
extremes
flooding
Rossby waves
spellingShingle Antarctica
atmospheric rivers
climate dynamics
extremes
flooding
Rossby waves
Rondanelli, R.
Hatchett, B.
Rutllant Costa, José
Bozkurt, D.
Garreaud Salazar, René
Strongest MJO on Record Triggers Extreme Atacama Rainfall and Warmth in Antarctica
topic_facet Antarctica
atmospheric rivers
climate dynamics
extremes
flooding
Rossby waves
description © 2019. The Authors.Tropical perturbations have been shown theoretically and observationally to excite long-range atmospheric responses in the form of Rossby wave teleconnections that result from the equator to pole gradient of planetary vorticity. An extreme teleconnection event occurred during March 2015 in the Southeastern Pacific. As a result, extreme high temperatures were observed in Southwestern South America and the Antarctic Peninsula simultaneously with an extreme rainfall and flood event in the hyperarid Atacama desert. We show that the origin of these seemingly disconnected extreme events can be traced to a Rossby wave response to the strongest Madden-Julian Oscillation (MJO) on record in the tropical central Pacific. A barotropic wave number 3 to 4 perturbation with group velocity between 15 and 30 m/s is consistent with the trajectory and timing followed by the upper-level anomalies radiating away from the tropics after the MJO episode.
format Article in Journal/Newspaper
author Rondanelli, R.
Hatchett, B.
Rutllant Costa, José
Bozkurt, D.
Garreaud Salazar, René
author_facet Rondanelli, R.
Hatchett, B.
Rutllant Costa, José
Bozkurt, D.
Garreaud Salazar, René
author_sort Rondanelli, R.
title Strongest MJO on Record Triggers Extreme Atacama Rainfall and Warmth in Antarctica
title_short Strongest MJO on Record Triggers Extreme Atacama Rainfall and Warmth in Antarctica
title_full Strongest MJO on Record Triggers Extreme Atacama Rainfall and Warmth in Antarctica
title_fullStr Strongest MJO on Record Triggers Extreme Atacama Rainfall and Warmth in Antarctica
title_full_unstemmed Strongest MJO on Record Triggers Extreme Atacama Rainfall and Warmth in Antarctica
title_sort strongest mjo on record triggers extreme atacama rainfall and warmth in antarctica
publisher Blackwell Publishing Ltd
publishDate 2019
url https://doi.org/10.1029/2018GL081475
https://repositorio.uchile.cl/handle/2250/171229
geographic Antarctic
Antarctic Peninsula
Pacific
The Antarctic
geographic_facet Antarctic
Antarctic Peninsula
Pacific
The Antarctic
genre Antarc*
Antarctic
Antarctic Peninsula
Antarctica
genre_facet Antarc*
Antarctic
Antarctic Peninsula
Antarctica
op_source Geophysical Research Letters
op_relation Geophysical Research Letters, Volumen 46, Issue 6, 2019, Pages 3482-3491
19448007
00948276
doi:10.1029/2018GL081475
https://repositorio.uchile.cl/handle/2250/171229
op_rights Attribution-NonCommercial-NoDerivs 3.0 Chile
http://creativecommons.org/licenses/by-nc-nd/3.0/cl/
op_rightsnorm CC-BY-NC-ND
op_doi https://doi.org/10.1029/2018GL081475
container_title Geophysical Research Letters
container_volume 46
container_issue 6
container_start_page 3482
op_container_end_page 3491
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