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@Article{GodoiAndrBryaGorm:2019:ReOcWa,
               author = "Godoi, Victor A. and Andrade, Felipe Marques de and Bryan, Karin 
                         R. and Gorman, Richard M.",
          affiliation = "{University of Waikato} and {Instituto Nacional de Pesquisas 
                         Espaciais (INPE)} and {University of Waikato} and {National 
                         Institute of Water and AtmosphericResearch Ltd}",
                title = "Regional\‐scale ocean wave variability associated with El 
                         Niño–Southern Oscillation\‐Madden\‐Julian 
                         Oscillation combined activity",
              journal = "International Journal of Climatology",
                 year = "2019",
               volume = "39",
               number = "1",
                pages = "483--494",
                month = "Jan.",
             keywords = "climate patterns, El Niño–Southern Oscillation, ENSO-MJO combined 
                         activity,Madden-Julian Oscillation, New Zealand, ocean wave 
                         variability, teleconnection,wave climate.",
             abstract = "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.",
                  doi = "10.1002/joc.5823",
                  url = "http://dx.doi.org/10.1002/joc.5823",
                 issn = "0899-8418",
             language = "en",
           targetfile = "godoi_regional.pdf",
        urlaccessdate = "05 dez. 2020"
}


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