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A multi‑parametric perspective of the North Atlantic eddy‑driven jet

dc.contributor.authorBarriopedro Cepero, David
dc.contributor.authorAyarzagüena Porras, Blanca
dc.contributor.authorGarcía-Burgos, Marina
dc.contributor.authorGarcía Herrera, Ricardo Francisco
dc.date.accessioned2024-02-05T19:24:01Z
dc.date.available2024-02-05T19:24:01Z
dc.date.issued2022
dc.description.abstractThe North Atlantic eddy-driven jet (EDJ) is an essential component of the Euro-Atlantic atmospheric circulation. It has been typically described in terms of latitude and intensity but this is not enough to fully characterize its variability and complex EDJ configurations. Here, we present a set of daily parameters of the EDJ based on low-tropospheric zonal wind data for the 1948–2020 period. They describe the intensity, sharpness, location, edges, tilt and other zonal asymmetries of the EDJ, therefore dissecting its structure beyond the latitudinal regimes. This allows for assessments of specific EDJ aspects and a multi-parametric treatment of EDJ configurations in a manageable way. Overall, variations in EDJ parameters reflect distinctive patterns of eddy forcing and wave breaking, with anticyclonic eddies playing a major role in shaping the EDJ structure. A multimodal behavior of the EDJ is only detected in latitude, which largely influences the longitudinal position of the EDJ. Other aspects of the EDJ are less constrained by the latitude and display a variety of configurations. Four multi-parametric states (northern, central, tilted and split EDJs) provide a satisfactory description of recurrent patterns of the EDJ. They participate in meridional migrations of the EDJ, but yield less dramatic transitions than viewed from the latitudinal perspective. Finally, the EDJ parameters help to better understand the EDJ influence on European climate. In many regions, latitude and intensity contain limited information on near-surface anomalies, and their signals can be masked by the additional effect of other EDJ parameters.
dc.description.departmentDepto. de Física de la Tierra y Astrofísica
dc.description.facultyInstituto de Geociencias (IGEO)
dc.description.refereedTRUE
dc.description.sponsorshipConsejo Superior de Investigaciones Científicas
dc.description.sponsorshipMinisterio de Ciencia, Innovación y Universidades (España)
dc.description.statuspub
dc.identifier.citationBarriopedro, D., Ayarzagüena, B., García-Burgos, M. et al. A multi-parametric perspective of the North Atlantic eddy-driven jet. Clim Dyn 61, 375–397 (2023). https://doi.org/10.1007/s00382-022-06574-w
dc.identifier.doi10.1007/s00382-022-06574-w
dc.identifier.essn1432-0894
dc.identifier.issn0930-7575
dc.identifier.officialurlhttps://doi.org/10.1007/s00382-022-06574-w
dc.identifier.relatedurlhttps://link.springer.com/article/10.1007/s00382-022-06574-w
dc.identifier.urihttps://hdl.handle.net/20.500.14352/99206
dc.journal.titleClimate Dynamics
dc.language.isoeng
dc.page.final397
dc.page.initial375
dc.publisherSpringer
dc.relation.projectIDRTI2018-096402-B-I00
dc.relation.projectIDGrant PRE2019-090618
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 Internationalen
dc.rights.accessRightsopen access
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/
dc.subject.cdu551.58
dc.subject.keywordEddy-driven jet
dc.subject.keywordNorth Atlantic atmospheric circulation
dc.subject.keywordClimate dynamics
dc.subject.keywordClimate variability
dc.subject.keywordClimate change
dc.subject.keywordEuropean climate
dc.subject.ucmFísica (Física)
dc.subject.unesco25 Ciencias de la Tierra y del Espacio
dc.subject.unesco2501 Ciencias de la Atmósfera
dc.titleA multi‑parametric perspective of the North Atlantic eddy‑driven jet
dc.typejournal article
dc.type.hasVersionVoR
dc.volume.number61
dspace.entity.typePublication
relation.isAuthorOfPublication71d8f23d-ceaf-4f5f-8434-10a193bc3835
relation.isAuthorOfPublicationafac4741-04ec-4805-9476-53451704e8de
relation.isAuthorOfPublication194b877d-c391-483e-9b29-31a99dff0a29
relation.isAuthorOfPublication.latestForDiscovery71d8f23d-ceaf-4f5f-8434-10a193bc3835

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