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(Reference retrieved automatically from Web of Science through information on FAPESP grant and its corresponding number as mentioned in the publication by the authors.)

Regional-scale ocean wave variability associated with El Nino-Southern Oscillation-Madden-Julian Oscillation combined activity

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Author(s):
Godoi, Victor A. [1] ; de Andrade, Felipe M. [2] ; Bryan, Karin R. [1] ; Gorman, Richard M. [3]
Total Authors: 4
Affiliation:
[1] Univ Waikato, Sch Sci, Hillcrest Rd, Hamilton 3216, Waikato - New Zealand
[2] Inst Nacl Pesquisas Espaciais, Ctr Previsao Tempo & Estudos Climat, Rodovia Presidente Dutra, Cachoeira Paulista - Brazil
[3] Natl Inst Water & Atmospher Res Ltd, Hamilton - New Zealand
Total Affiliations: 3
Document type: Journal article
Source: INTERNATIONAL JOURNAL OF CLIMATOLOGY; v. 39, n. 1, p. 483-494, JAN 2019.
Web of Science Citations: 2
Abstract

The significant wave height variability caused by wind anomalies associated with the co-occurrence of the Madden-Julian Oscillation (MJO) and El Nino-Southern Oscillation (ENSO) was investigated in the New Zealand region. For this purpose, and wind anomalies composites were created using 23years (1979-2002) of modelled data during November-March periods, when simultaneous ENSO-MJO phase pairs are potentially most active. The results show striking features: El Nino-related wave conditions (which consist of increased along the west and south coasts of New Zealand) are reinforced during MJO phase 8, whereas the wave conditions associated with La Nina (which consist of larger along the north coast) are enhanced during MJO phase 6; Similar wave anomalies are generated during opposing ENSO phases (La Nina and El Nino) when these are combined with MJO phases 3 and 5, respectively; The majority of statistically significant anomalies disappear from the study area during El Nino-MJO phase 6, El Nino-MJO phase 2, and La Nina-MJO phase 4, showing the neutralizing nature of some phase combinations; Finally, negative anomalies are experienced off the country's west coast during El Nino-MJO phase 4, in contrast to the positive anomalies expected during El Nino events. These results clearly show the importance of remote forcing to wave anomalies in the New Zealand region, and highlight the need to assess atmospheric and oceanic conditions considering multiple climate oscillations. (AU)