Temporal Filtering Enhances the Skewness of Sea Surface Winds

dc.contributor.authorMonahan, Adam H.
dc.date.accessioned2019-09-26T12:11:48Z
dc.date.available2019-09-26T12:11:48Z
dc.date.copyright2018en_US
dc.date.issued2018
dc.description.abstractThe component of the sea surface wind in the along-mean wind direction is known to display pronounced skewness at many locations over the ocean. A recent study by Proistosescu et al. found that the skewness of daily 850-hPa air temperature measured by radiosondes is typically reduced by bandpass filtering. This behavior was also shown to be characteristic of correlated additive–multiplicative (CAM) noise, which has been proposed as a generic model for non-Gaussian variability in the atmosphere and ocean. The present study shows that if the cutoff frequency is not too low, the skewness of the along-mean wind component is enhanced by low-pass filtering, particularly in the equatorial band and in the midlatitude storm tracks. The filter time scale beyond which skewness is systematically reduced by filtering is of the daily to synoptic scale, except in a narrow equatorial band where it is of subseasonal to seasonal time scales. This behavior is reproduced in an idealized stochastic model of the near-surface winds, in which key parameters are the characteristic time scales of the nonlinear dynamics and of the noise. These results point toward more general approaches for assessing the relative importance of multiplicative noise or dynamical nonlinearities in producing non-Gaussian structure in atmospheric and oceanic fields.en_US
dc.description.reviewstatusRevieweden_US
dc.description.scholarlevelFacultyen_US
dc.description.sponsorshipI gratefully acknowledge support from the Natural Sciences and Engineering Research Council of Canada (NSERC; Grant RGPIN-2014-06509). I would also like to thank Carsten Abraham, Christian Proistosescu, Tim DelSole, and one anonymous reviewer for their helpful comments on the manuscript. This research was carried out when I was a visitor at the Statistical and Applied Mathematical Sciences Institute (SAMSI), whose hospitality I gratefully acknowledge. Data were obtained from the Global Modeling and Assimilation Office (GMAO 2015; https://doi.org/10.5067/3Z173KIE2TPD).en_US
dc.identifier.citationMonahan, A.H. (2018). Temporal Filtering Enhances the Skewness of Sea Surface Winds. Journal of Climate, 31(14), 5695-5706. https://doi.org/10.1175/JCLI-D-17- 0814.1en_US
dc.identifier.urihttps://doi.org/10.1175/JCLI-D-17-0814.1
dc.identifier.urihttp://hdl.handle.net/1828/11187
dc.language.isoenen_US
dc.publisherJournal of Climateen_US
dc.subjectWinden_US
dc.subjectFiltering techniquesen_US
dc.subjectTime seriesen_US
dc.subjectNonlinear modelsen_US
dc.subjectStochastic modelsen_US
dc.titleTemporal Filtering Enhances the Skewness of Sea Surface Windsen_US
dc.typeArticleen_US

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