Extratropical Cyclogenesis Changes in Connection with Tropospheric ENSO Teleconnections to the North Atlantic: Role of Stationary and Transient Waves
International audience This study investigates mechanisms for changes in wintertime extratropical cyclogenesis over North America and the North Atlantic during different phases of El Niño-Southern Oscillation (ENSO). Insights into the relationship between the ENSO-North Atlantic teleconnection and t...
Published in: | Journal of the Atmospheric Sciences |
---|---|
Main Authors: | , , , |
Other Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
HAL CCSD
2018
|
Subjects: | |
Online Access: | https://hal.archives-ouvertes.fr/hal-02324720 https://hal.archives-ouvertes.fr/hal-02324720/document https://hal.archives-ouvertes.fr/hal-02324720/file/Schemm_et_al18.pdf https://doi.org/10.1175/JAS-D-17-0340.1 |
id |
ftccsdartic:oai:HAL:hal-02324720v1 |
---|---|
record_format |
openpolar |
spelling |
ftccsdartic:oai:HAL:hal-02324720v1 2023-05-15T16:27:17+02:00 Extratropical Cyclogenesis Changes in Connection with Tropospheric ENSO Teleconnections to the North Atlantic: Role of Stationary and Transient Waves Schemm, Sebastian Rivière, Gwendal Ciasto, Laura, Li, Camille Laboratoire de Météorologie Dynamique (UMR 8539) (LMD) Département des Géosciences - ENS Paris École normale supérieure - Paris (ENS Paris) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-École normale supérieure - Paris (ENS Paris) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Centre National de la Recherche Scientifique (CNRS)-École des Ponts ParisTech (ENPC)-École polytechnique (X)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC) 2018-11 https://hal.archives-ouvertes.fr/hal-02324720 https://hal.archives-ouvertes.fr/hal-02324720/document https://hal.archives-ouvertes.fr/hal-02324720/file/Schemm_et_al18.pdf https://doi.org/10.1175/JAS-D-17-0340.1 en eng HAL CCSD American Meteorological Society info:eu-repo/semantics/altIdentifier/doi/10.1175/JAS-D-17-0340.1 hal-02324720 https://hal.archives-ouvertes.fr/hal-02324720 https://hal.archives-ouvertes.fr/hal-02324720/document https://hal.archives-ouvertes.fr/hal-02324720/file/Schemm_et_al18.pdf doi:10.1175/JAS-D-17-0340.1 http://creativecommons.org/licenses/by/ info:eu-repo/semantics/OpenAccess ISSN: 0022-4928 EISSN: 1520-0469 Journal of the Atmospheric Sciences https://hal.archives-ouvertes.fr/hal-02324720 Journal of the Atmospheric Sciences, American Meteorological Society, 2018, 75 (11), pp.3943-3964. ⟨10.1175/JAS-D-17-0340.1⟩ [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere info:eu-repo/semantics/article Journal articles 2018 ftccsdartic https://doi.org/10.1175/JAS-D-17-0340.1 2021-11-21T01:12:28Z International audience This study investigates mechanisms for changes in wintertime extratropical cyclogenesis over North America and the North Atlantic during different phases of El Niño-Southern Oscillation (ENSO). Insights into the relationship between the ENSO-North Atlantic teleconnection and the cyclogenesis changes are provided by diagnosing the relative roles of stationary wave propagation and transient eddies in setting cyclogenesis-conducive large-scale circulation anomalies. During La Niña winters, Rocky Mountain and Greenland cyclogenesis are enhanced, while Gulf Stream cyclogenesis is reduced. Diagnostics suggest that stationary waves of tropical origin work in tandem with transient eddies to amplify the ridge over the northeastern Pacific, establishing background flow anomalies that favor Rocky Mountain cyclogenesis; downstream, more transient eddies with an anticyclonic tilt push the North Atlantic jet poleward, favoring cyclogenesis near Greenland, while contributions from stationary waves are small. During central Pacific El Niño winters, the cyclogenesis situation is essentially the opposite: Rocky Mountain and Greenland cyclo-genesis are reduced, while Gulf Stream cyclogenesis is enhanced. The analyses are consistent with stationary waves and transient eddies acting to weaken the climatological ridge over the northeastern Pacific, creating a more zonal Pacific jet; downstream, transient eddies with a cyclonic tilt push the North Atlantic jet equa-torward, favoring Gulf Stream cyclogenesis. Anomalies in cyclogenesis frequencies, and the relative roles of transient and stationary waves, during eastern Pacific El Niño winters are associated with larger uncertainties. Article in Journal/Newspaper Greenland North Atlantic Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Greenland Pacific Journal of the Atmospheric Sciences 75 11 3943 3964 |
institution |
Open Polar |
collection |
Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) |
op_collection_id |
ftccsdartic |
language |
English |
topic |
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere |
spellingShingle |
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere Schemm, Sebastian Rivière, Gwendal Ciasto, Laura, Li, Camille Extratropical Cyclogenesis Changes in Connection with Tropospheric ENSO Teleconnections to the North Atlantic: Role of Stationary and Transient Waves |
topic_facet |
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere |
description |
International audience This study investigates mechanisms for changes in wintertime extratropical cyclogenesis over North America and the North Atlantic during different phases of El Niño-Southern Oscillation (ENSO). Insights into the relationship between the ENSO-North Atlantic teleconnection and the cyclogenesis changes are provided by diagnosing the relative roles of stationary wave propagation and transient eddies in setting cyclogenesis-conducive large-scale circulation anomalies. During La Niña winters, Rocky Mountain and Greenland cyclogenesis are enhanced, while Gulf Stream cyclogenesis is reduced. Diagnostics suggest that stationary waves of tropical origin work in tandem with transient eddies to amplify the ridge over the northeastern Pacific, establishing background flow anomalies that favor Rocky Mountain cyclogenesis; downstream, more transient eddies with an anticyclonic tilt push the North Atlantic jet poleward, favoring cyclogenesis near Greenland, while contributions from stationary waves are small. During central Pacific El Niño winters, the cyclogenesis situation is essentially the opposite: Rocky Mountain and Greenland cyclo-genesis are reduced, while Gulf Stream cyclogenesis is enhanced. The analyses are consistent with stationary waves and transient eddies acting to weaken the climatological ridge over the northeastern Pacific, creating a more zonal Pacific jet; downstream, transient eddies with a cyclonic tilt push the North Atlantic jet equa-torward, favoring Gulf Stream cyclogenesis. Anomalies in cyclogenesis frequencies, and the relative roles of transient and stationary waves, during eastern Pacific El Niño winters are associated with larger uncertainties. |
author2 |
Laboratoire de Météorologie Dynamique (UMR 8539) (LMD) Département des Géosciences - ENS Paris École normale supérieure - Paris (ENS Paris) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-École normale supérieure - Paris (ENS Paris) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Centre National de la Recherche Scientifique (CNRS)-École des Ponts ParisTech (ENPC)-École polytechnique (X)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC) |
format |
Article in Journal/Newspaper |
author |
Schemm, Sebastian Rivière, Gwendal Ciasto, Laura, Li, Camille |
author_facet |
Schemm, Sebastian Rivière, Gwendal Ciasto, Laura, Li, Camille |
author_sort |
Schemm, Sebastian |
title |
Extratropical Cyclogenesis Changes in Connection with Tropospheric ENSO Teleconnections to the North Atlantic: Role of Stationary and Transient Waves |
title_short |
Extratropical Cyclogenesis Changes in Connection with Tropospheric ENSO Teleconnections to the North Atlantic: Role of Stationary and Transient Waves |
title_full |
Extratropical Cyclogenesis Changes in Connection with Tropospheric ENSO Teleconnections to the North Atlantic: Role of Stationary and Transient Waves |
title_fullStr |
Extratropical Cyclogenesis Changes in Connection with Tropospheric ENSO Teleconnections to the North Atlantic: Role of Stationary and Transient Waves |
title_full_unstemmed |
Extratropical Cyclogenesis Changes in Connection with Tropospheric ENSO Teleconnections to the North Atlantic: Role of Stationary and Transient Waves |
title_sort |
extratropical cyclogenesis changes in connection with tropospheric enso teleconnections to the north atlantic: role of stationary and transient waves |
publisher |
HAL CCSD |
publishDate |
2018 |
url |
https://hal.archives-ouvertes.fr/hal-02324720 https://hal.archives-ouvertes.fr/hal-02324720/document https://hal.archives-ouvertes.fr/hal-02324720/file/Schemm_et_al18.pdf https://doi.org/10.1175/JAS-D-17-0340.1 |
geographic |
Greenland Pacific |
geographic_facet |
Greenland Pacific |
genre |
Greenland North Atlantic |
genre_facet |
Greenland North Atlantic |
op_source |
ISSN: 0022-4928 EISSN: 1520-0469 Journal of the Atmospheric Sciences https://hal.archives-ouvertes.fr/hal-02324720 Journal of the Atmospheric Sciences, American Meteorological Society, 2018, 75 (11), pp.3943-3964. ⟨10.1175/JAS-D-17-0340.1⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1175/JAS-D-17-0340.1 hal-02324720 https://hal.archives-ouvertes.fr/hal-02324720 https://hal.archives-ouvertes.fr/hal-02324720/document https://hal.archives-ouvertes.fr/hal-02324720/file/Schemm_et_al18.pdf doi:10.1175/JAS-D-17-0340.1 |
op_rights |
http://creativecommons.org/licenses/by/ info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1175/JAS-D-17-0340.1 |
container_title |
Journal of the Atmospheric Sciences |
container_volume |
75 |
container_issue |
11 |
container_start_page |
3943 |
op_container_end_page |
3964 |
_version_ |
1766016404888223744 |