Evaluation of easterly wave disturbances over the tropical South Atlantic in CMIP6 models

dc.contributor.authorCavalcante, Lucas C. V.
dc.contributor.authorGomes, Helber B.
dc.contributor.authorHodges, Kevin
dc.contributor.authorRay, Pallav
dc.contributor.authorHerdies, Dirceu L.
dc.contributor.authorBarbosa, Henrique M. J.
dc.contributor.authorGoncalves, Weber A.
dc.date.accessioned2025-10-29T11:33:11Z
dc.date.issued2025
dc.departmentFakülteler, Havacılık ve Uzay Bilimleri Fakültesi, Havacılık Bölümü
dc.description.abstractThis study assesses the performance of the latest phase of Coupled Model Intercomparison Project (CMIP6) models in simulating easterly wave disturbances (EWD) over the tropical South Atlantic (TSA) impacting northeast Brazil (NEB). Initially, we evaluate simulated precipitation from 17 historical CMIP, 16 AMIP, 7 hist-1950, and 10 highresSST-present models against the Global Precipitation Climatology Project (GPCP) dataset to identify models that accurately reproduce the spatial and temporal precipitation patterns in the study region. The ensemble's spatial analysis demonstrates their capability in reproducing annual and seasonal precipitation climatology. However, models underestimate precipitation intensity along NEB's coast while overestimating it in TSA and NEB's north. Model uncertainties tend to be greater with higher latitudes. The models represented the annual cycle in all subareas within the study region, particularly from July to October, albeit with a greater spread in the first half of the year, especially over the Intertropical Convergence Zone (ITCZ). Based on it, three top-performing models from each ensemble were selected for EWD evaluation. The automatic tracking algorithm for EWDs showed the model's ability to represent mean values of EWD lifetime (similar to 6 days) and phase speed (similar to 7 m s(-1)) as found in ERA5 reanalysis. However, they failed to capture EWD's interannual variability or climatological mean frequency. Despite CMIP6 model weaknesses, they accurately identified two primary EWD genesis regions: one over the TSA and another near the West African coast. Overall, CMIP6 models, particularly atmospheric and high-resolution models (HighResMIP), effectively captured precipitation climatology and EWD characteristics over NEB and the adjacent TSA.
dc.description.sponsorshipConselho Nacional de Desenvolvimento Cientifico e Tecnologico, CNPq [870018/2004-3]
dc.description.sponsorshipThis study was supported by Conselho Nacional de Desenvolvimento Cientifico e Tecnologico, CNPq (Grant no. 870018/2004-3).
dc.identifier.doi10.1007/s00382-024-07507-5
dc.identifier.issn0930-7575
dc.identifier.issn1432-0894
dc.identifier.issue1
dc.identifier.orcid0000-0001-8924-1852
dc.identifier.orcid0000-0002-2872-8453
dc.identifier.orcid0000-0003-0890-762X
dc.identifier.scopus2-s2.0-85213053232
dc.identifier.scopusqualityQ1
dc.identifier.urihttps://doi.org/10.1007/s00382-024-07507-5
dc.identifier.urihttps://hdl.handle.net/20.500.14854/12300
dc.identifier.volume63
dc.identifier.wosWOS:001385255500002
dc.identifier.wosqualityN/A
dc.indekslendigikaynakWeb of Science
dc.indekslendigikaynakScopus
dc.language.isoen
dc.publisherSpringer
dc.relation.ispartofClimate Dynamics
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı
dc.rightsinfo:eu-repo/semantics/closedAccess
dc.snmzKA_WOS_20251020
dc.subjectClimatology
dc.subjectTracking
dc.titleEvaluation of easterly wave disturbances over the tropical South Atlantic in CMIP6 models
dc.typeArticle

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