%0 Journal Article
%@nexthigherunit 8JMKD3MGPCW/43SQKNE
%3 godoi_regional.pdf
%4 sid.inpe.br/mtc-m21c/2019/02.08.16.34
%8 Jan.
%9 journal article
%@issn 0899-8418
%A Godoi, Victor A.,
%A Andrade, Felipe Marques de,
%A Bryan, Karin R.,
%A Gorman, Richard M.,
%@secondarytype PRE PI
%B International Journal of Climatology
%D 2019
%K climate patterns, El Niño–Southern Oscillation, ENSO-MJO combined activity,Madden-Julian Oscillation, New Zealand, ocean wave variability, teleconnection,wave climate.
%@archivingpolicy denypublisher denyfinaldraft
%N 1
%P 483-494
%@secondarymark A1_GEOCIÊNCIAS A1_ENGENHARIAS_I A1_CIÊNCIAS_AMBIENTAIS A1_CIÊNCIAS_AGRÁRIAS_I A2_INTERDISCIPLINAR A2_BIODIVERSIDADE B1_CIÊNCIAS_BIOLÓGICAS_I
%T Regional‐scale ocean wave variability associated with El Niño–Southern Oscillation‐Madden‐Julian Oscillation combined activity
%V 39
%X The significant wave height (Hs) variability caused by wind anomalies associatedwith the co-occurrence of the Madden-Julian Oscillation (MJO) and El NiñoSouthern Oscillation (ENSO) was investigated in the New Zealand region. For thispurpose,Hsand wind anomalies composites were created using 23 years(19792002) of modelled data during NovemberMarch periods, when simulta-neous ENSO-MJO phase pairs are potentially most active. The results show strik-ing features: El Niño-related wave conditions (which consist of increasedHsalongthe west and south coasts of New Zealand) are reinforced during MJO phase8, whereas the wave conditions associated with La Niña (which consist of largerHsalong the north coast) are enhanced during MJO phase 6; Similar wave anomaliesare generated during opposing ENSO phases (La Niña and El Niño) when these arecombined with MJO phases 3 and 5, respectively; The majority of statistically sig-nificantHsanomalies disappear from the study area during El Niño-MJO phase6, El Niño-MJO phase 2, and La Niña-MJO phase 4, showing the neutralizingnature of some phase combinations; Finally, negativeHsanomalies are experiencedoff the country's west coast during El Niño-MJO phase 4, in contrast to the positiveanomalies expected during El Niño events. These results clearly show the impor-tance of remote forcing to wave anomalies in the New Zealand region, and high-light the need to assess atmospheric and oceanic conditions considering multipleclimate oscillations.
%@area MET
%@electronicmailaddress victorgodoirj@gmail.com
%@electronicmailaddress felipe.andrade@inpe.br
%@documentstage not transferred
%@group
%@group DIDOP-CGCPT-INPE-MCTIC-GOV-BR
%@dissemination WEBSCI; PORTALCAPES; COMPENDEX; SCOPUS.
%@orcid 0000-0001-7951-3017
%@usergroup simone
%@affiliation University of Waikato
%@affiliation Instituto Nacional de Pesquisas Espaciais (INPE)
%@affiliation University of Waikato
%@affiliation National Institute of Water and AtmosphericResearch Ltd
%@versiontype publisher
%@holdercode {isadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S}
%@doi 10.1002/joc.5823
%2 sid.inpe.br/mtc-m21c/2019/02.08.16.34.50