Seasonal atmospheric transitions in the Caribbean basin and Central America
International audience The dates of the transition between winter (S2W) regional-scale atmospheric regimes have been defined using daily weather types above and around the Caribbean basin from 1979 to 2017. The uncertainties due to either the use of two different reanalyses (i.e., NCEP-DOE and ERA-I...
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ftcollegfrance:oai:HAL:hal-02962648v1 2024-06-23T07:55:21+00:00 Seasonal atmospheric transitions in the Caribbean basin and Central America Gouirand, Isabelle Moron, Vincent Sing, Bernd Centre Européen de Recherche et d'Enseignement des Géosciences de l'Environnement (CEREGE) Institut de Recherche pour le Développement (IRD)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE) 2020-10 https://hal.science/hal-02962648 https://hal.science/hal-02962648/document https://hal.science/hal-02962648/file/gouirand%26al_cd2020.pdf https://doi.org/10.1007/s00382-020-05356-6 en eng HAL CCSD Springer Verlag info:eu-repo/semantics/altIdentifier/doi/10.1007/s00382-020-05356-6 hal-02962648 https://hal.science/hal-02962648 https://hal.science/hal-02962648/document https://hal.science/hal-02962648/file/gouirand%26al_cd2020.pdf doi:10.1007/s00382-020-05356-6 WOS: 000548495300002 info:eu-repo/semantics/OpenAccess ISSN: 0930-7575 EISSN: 1432-0894 Climate Dynamics https://hal.science/hal-02962648 Climate Dynamics, 2020, 55 (7-8), pp.1809-1828. ⟨10.1007/s00382-020-05356-6⟩ [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere info:eu-repo/semantics/article Journal articles 2020 ftcollegfrance https://doi.org/10.1007/s00382-020-05356-6 2024-06-13T23:38:27Z International audience The dates of the transition between winter (S2W) regional-scale atmospheric regimes have been defined using daily weather types above and around the Caribbean basin from 1979 to 2017. The uncertainties due to either the use of two different reanalyses (i.e., NCEP-DOE and ERA-Interim) or the parametrization used for the definition of the transition dates have typi- cally a small impact on the interannual variability of the seasonal transitions. When both reanalyses are considered together, the average W2S transition date occurs, on average, on May (with a standard deviation of 9 days) while the S2W transition date occurs, on average, on October 26 (with a standard deviation of 12 days). 1The atmospheric characteristics associated with both transitions reveal asymmetries in the annual cycle. The W2S transition is rather abrupt and near-synchronous and a weakening of the Caribbean Low Level Jet. The W2S transition is also not preceded by any significant sea surface temperature (SST) anomalies either in the tropical North Atlantic or the Eastern Pacific. On the other hand, the S2W transition is overall smoother, and anomalously warm (cold) SST over the Caribbean Sea and Gulf of Mexico (Eastern Pacific) during the bo- real summer are usually related to a delayed transition (and vice versa). The interannual variations of S2W and W2S transitions are mostly independent to each other. The potential and real-time predictability of the W2S transition is explored using a subseasonal-to-seasonal prediction ensemble (11 runs from 1998 to 2017) from the ECMWF model. Its skill is close to zero with a lead time longer than 15-20 days, confirming the weak im-pact of the antecedent SST upon the W2S transition. The skill suddenly increases from late April, 2-3 weeks only before the mean W2S transition date. It suggests that some atmospheric forcing, operating from synopticto intra-seasonal time scale, plays a role, but it seems barely related to any occurrence, or sequence, of specific weather types. Article in Journal/Newspaper North Atlantic Collège de France: HAL Pacific Climate Dynamics 55 7-8 1809 1828 |
institution |
Open Polar |
collection |
Collège de France: HAL |
op_collection_id |
ftcollegfrance |
language |
English |
topic |
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere |
spellingShingle |
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere Gouirand, Isabelle Moron, Vincent Sing, Bernd Seasonal atmospheric transitions in the Caribbean basin and Central America |
topic_facet |
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere |
description |
International audience The dates of the transition between winter (S2W) regional-scale atmospheric regimes have been defined using daily weather types above and around the Caribbean basin from 1979 to 2017. The uncertainties due to either the use of two different reanalyses (i.e., NCEP-DOE and ERA-Interim) or the parametrization used for the definition of the transition dates have typi- cally a small impact on the interannual variability of the seasonal transitions. When both reanalyses are considered together, the average W2S transition date occurs, on average, on May (with a standard deviation of 9 days) while the S2W transition date occurs, on average, on October 26 (with a standard deviation of 12 days). 1The atmospheric characteristics associated with both transitions reveal asymmetries in the annual cycle. The W2S transition is rather abrupt and near-synchronous and a weakening of the Caribbean Low Level Jet. The W2S transition is also not preceded by any significant sea surface temperature (SST) anomalies either in the tropical North Atlantic or the Eastern Pacific. On the other hand, the S2W transition is overall smoother, and anomalously warm (cold) SST over the Caribbean Sea and Gulf of Mexico (Eastern Pacific) during the bo- real summer are usually related to a delayed transition (and vice versa). The interannual variations of S2W and W2S transitions are mostly independent to each other. The potential and real-time predictability of the W2S transition is explored using a subseasonal-to-seasonal prediction ensemble (11 runs from 1998 to 2017) from the ECMWF model. Its skill is close to zero with a lead time longer than 15-20 days, confirming the weak im-pact of the antecedent SST upon the W2S transition. The skill suddenly increases from late April, 2-3 weeks only before the mean W2S transition date. It suggests that some atmospheric forcing, operating from synopticto intra-seasonal time scale, plays a role, but it seems barely related to any occurrence, or sequence, of specific weather types. |
author2 |
Centre Européen de Recherche et d'Enseignement des Géosciences de l'Environnement (CEREGE) Institut de Recherche pour le Développement (IRD)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE) |
format |
Article in Journal/Newspaper |
author |
Gouirand, Isabelle Moron, Vincent Sing, Bernd |
author_facet |
Gouirand, Isabelle Moron, Vincent Sing, Bernd |
author_sort |
Gouirand, Isabelle |
title |
Seasonal atmospheric transitions in the Caribbean basin and Central America |
title_short |
Seasonal atmospheric transitions in the Caribbean basin and Central America |
title_full |
Seasonal atmospheric transitions in the Caribbean basin and Central America |
title_fullStr |
Seasonal atmospheric transitions in the Caribbean basin and Central America |
title_full_unstemmed |
Seasonal atmospheric transitions in the Caribbean basin and Central America |
title_sort |
seasonal atmospheric transitions in the caribbean basin and central america |
publisher |
HAL CCSD |
publishDate |
2020 |
url |
https://hal.science/hal-02962648 https://hal.science/hal-02962648/document https://hal.science/hal-02962648/file/gouirand%26al_cd2020.pdf https://doi.org/10.1007/s00382-020-05356-6 |
geographic |
Pacific |
geographic_facet |
Pacific |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
ISSN: 0930-7575 EISSN: 1432-0894 Climate Dynamics https://hal.science/hal-02962648 Climate Dynamics, 2020, 55 (7-8), pp.1809-1828. ⟨10.1007/s00382-020-05356-6⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1007/s00382-020-05356-6 hal-02962648 https://hal.science/hal-02962648 https://hal.science/hal-02962648/document https://hal.science/hal-02962648/file/gouirand%26al_cd2020.pdf doi:10.1007/s00382-020-05356-6 WOS: 000548495300002 |
op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1007/s00382-020-05356-6 |
container_title |
Climate Dynamics |
container_volume |
55 |
container_issue |
7-8 |
container_start_page |
1809 |
op_container_end_page |
1828 |
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1802647912760475648 |