Easterly wave contributions to seasonal rainfall over the tropical Americas in observations and a regional climate model

Easterly waves (EWs) are important moisture carriers and their variability can impact the total May-November rainfall, defined as seasonal precipitation, over the Tropical Americas. The contribution of EWs to the seasonal precipitation is explored over the tropical Americas using rain gauge stations...

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Published in:Climate Dynamics
Other Authors: Dominguez, Christian (author), Done, James M. (author), Bruyère, Cindy L. (author)
Format: Article in Journal/Newspaper
Language:English
Published: 2020
Subjects:
Online Access:https://doi.org/10.1007/s00382-019-04996-7
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spelling ftncar:oai:drupal-site.org:articles_23154 2024-04-28T08:31:01+00:00 Easterly wave contributions to seasonal rainfall over the tropical Americas in observations and a regional climate model Dominguez, Christian (author) Done, James M. (author) Bruyère, Cindy L. (author) 2020-01-08 https://doi.org/10.1007/s00382-019-04996-7 en eng Climate Dynamics--Clim Dyn--0930-7575--1432-0894 articles:23154 ark:/85065/d74x5c04 doi:10.1007/s00382-019-04996-7 Copyright author(s). This work is licensed under a Creative Commons Attribution-NonCommercial 4.0 International License. article Text 2020 ftncar https://doi.org/10.1007/s00382-019-04996-7 2024-04-04T17:32:42Z Easterly waves (EWs) are important moisture carriers and their variability can impact the total May-November rainfall, defined as seasonal precipitation, over the Tropical Americas. The contribution of EWs to the seasonal precipitation is explored over the tropical Americas using rain gauge stations, reanalysis data and a regional model ensemble during the 1980-2013 period. In the present study, EWs are found to produce up to 50% of seasonal rainfall mainly over the north of South America and contribute substantially to interannual regional rainfall variability. An observational analysis shows that the El Nino Southern Oscillation (ENSO) affects EW frequency and therefore, their contribution to seasonal rainfall. In recent years, tropical cyclone (TC) activity over the Main Development Region (MDR) of the tropical North Atlantic has a negative impact on regional seasonal precipitation over northern South America. High TC activity over MDR corresponds to below-normal precipitation because it reduces the EW activity reaching northern South America through the recurving of TC tracks. Recurving TC tracks redirect moisture away from the tropical belt and into the mid-latitudes. However, this relationship only holds under neutral ENSO conditions and the positive phase of the Atlantic Multidecadal Oscillation. A 10-member regional model multi-physics ensemble simulation for the period 1990-2000 was analyzed to show the relationships are robust to different representations of physical processes. This new understanding of seasonal rainfall over the tropical Americas may support improved regional seasonal and climate outlooks. Article in Journal/Newspaper North Atlantic OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research) Climate Dynamics 54 1-2 191 209
institution Open Polar
collection OpenSky (NCAR/UCAR - National Center for Atmospheric Research/University Corporation for Atmospheric Research)
op_collection_id ftncar
language English
description Easterly waves (EWs) are important moisture carriers and their variability can impact the total May-November rainfall, defined as seasonal precipitation, over the Tropical Americas. The contribution of EWs to the seasonal precipitation is explored over the tropical Americas using rain gauge stations, reanalysis data and a regional model ensemble during the 1980-2013 period. In the present study, EWs are found to produce up to 50% of seasonal rainfall mainly over the north of South America and contribute substantially to interannual regional rainfall variability. An observational analysis shows that the El Nino Southern Oscillation (ENSO) affects EW frequency and therefore, their contribution to seasonal rainfall. In recent years, tropical cyclone (TC) activity over the Main Development Region (MDR) of the tropical North Atlantic has a negative impact on regional seasonal precipitation over northern South America. High TC activity over MDR corresponds to below-normal precipitation because it reduces the EW activity reaching northern South America through the recurving of TC tracks. Recurving TC tracks redirect moisture away from the tropical belt and into the mid-latitudes. However, this relationship only holds under neutral ENSO conditions and the positive phase of the Atlantic Multidecadal Oscillation. A 10-member regional model multi-physics ensemble simulation for the period 1990-2000 was analyzed to show the relationships are robust to different representations of physical processes. This new understanding of seasonal rainfall over the tropical Americas may support improved regional seasonal and climate outlooks.
author2 Dominguez, Christian (author)
Done, James M. (author)
Bruyère, Cindy L. (author)
format Article in Journal/Newspaper
title Easterly wave contributions to seasonal rainfall over the tropical Americas in observations and a regional climate model
spellingShingle Easterly wave contributions to seasonal rainfall over the tropical Americas in observations and a regional climate model
title_short Easterly wave contributions to seasonal rainfall over the tropical Americas in observations and a regional climate model
title_full Easterly wave contributions to seasonal rainfall over the tropical Americas in observations and a regional climate model
title_fullStr Easterly wave contributions to seasonal rainfall over the tropical Americas in observations and a regional climate model
title_full_unstemmed Easterly wave contributions to seasonal rainfall over the tropical Americas in observations and a regional climate model
title_sort easterly wave contributions to seasonal rainfall over the tropical americas in observations and a regional climate model
publishDate 2020
url https://doi.org/10.1007/s00382-019-04996-7
genre North Atlantic
genre_facet North Atlantic
op_relation Climate Dynamics--Clim Dyn--0930-7575--1432-0894
articles:23154
ark:/85065/d74x5c04
doi:10.1007/s00382-019-04996-7
op_rights Copyright author(s). This work is licensed under a Creative Commons Attribution-NonCommercial 4.0 International License.
op_doi https://doi.org/10.1007/s00382-019-04996-7
container_title Climate Dynamics
container_volume 54
container_issue 1-2
container_start_page 191
op_container_end_page 209
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