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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Online Access: | https://doi.org/10.1029/2018GL081475 https://repositorio.uchile.cl/handle/2250/171229 |
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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 |
_version_ |
1766153840566992896 |