Articles | Volume 2, issue 4
https://doi.org/10.5194/wcd-2-1149-2021
https://doi.org/10.5194/wcd-2-1149-2021
Research article
 | 
02 Dec 2021
Research article |  | 02 Dec 2021

Intraseasonal variability of ocean surface wind waves in the western South Atlantic: the role of cyclones and the Pacific South American pattern

Dalton K. Sasaki, Carolina B. Gramcianinov, Belmiro Castro, and Marcelo Dottori

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Cited articles

Alves, J.-H. G.: Numerical modeling of ocean swell contributions to the global wind-wave climate, Ocean Model., 11, 98–122, https://doi.org/10.1016/j.ocemod.2004.11.007, 2006. a
Ambrizzi, T. and Hoskins, B. J.: Stationary rossby-wave propagation in a baroclinic atmosphere, Q. J. Roy. Meteorol. Soc., 123, 919–928, https://doi.org/10.1002/qj.49712354007, 1997. a, b
Ambrizzi, T., Hoskins, B. J., and Hsu, H.-H.: Rossby wave propagation and teleconnection patterns in the austral winter, J. Atmos. Sci., 52, 3661–3672, 1995. a
Ardhuin, F. and Orfila, A.: Wind Waves, in: New Frontiers in Operational Oceanography, edited by: Chassignet, E., Pascual, A., Tintoré, J., and Verron, J., GODAE OceanView, Florida State University College of Medicine, chap. 14, 393–422, https://doi.org/10.17125/gov2018.ch14, 2018. a
Ardhuin, F., Chapron, B., and Collard, F.: Observation of swell dissipation across oceans, Geophys. Res. Lett., 36, L06607, https://doi.org/10.1029/2008gl037030, 2009. a
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Extratropical cyclones are relevant in the western South Atlantic and influence the climate of ocean surface wave. Propagating atmospheric features from the South Pacific to the South Atlantic are relevant to the cyclones and waves, and its intensified westerlies lead to more cyclones and, as a consequence, to higher wave heights. The opposite happens with its weakening. These features are similar to the so-called Pacific South American patterns and present periods between 30 and 180 d.
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