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dc.contributor.authorRichardson, Philip L.  Concept link
dc.date.accessioned2011-05-04T12:37:49Z
dc.date.available2011-05-04T12:37:49Z
dc.date.issued2010-08-26
dc.identifier.urihttps://hdl.handle.net/1912/4535
dc.descriptionAuthor Posting. © The Author(s), 2010. This is the author's version of the work. It is posted here by permission of Elsevier B.V. for personal use, not for redistribution. The definitive version was published in Progress In Oceanography 88 (2011): 46-58, doi:10.1016/j.pocean.2010.08.001.en_US
dc.description.abstractAlbatrosses fly long distances over the Southern Ocean, even around the world (almost) without flapping their wings, which has raised interest in how they perform such a feat. On a cruise to the South Atlantic I observed albatrosses soaring in a characteristic swooping zigzag flight that appears to combine two soaring techniques to gain energy— wind-shear soaring (dynamic soaring) using the vertical gradient of wind velocity and wave-slope soaring using updrafts over waves. The observed characteristic swooping flight is shown in a new illustration and interpreted in terms of the two soaring techniques. The energy gain estimated for “typical conditions” in the Southern Ocean suggests that wind-shear soaring provides around 80-90% of the total energy required for sustained soaring. A much smaller percentage is provided by wind shear in light winds and significant swell when wave-slope soaring dominates. A simple dynamical model of wind-shear soaring is proposed based on the concept of a bird flying across a sharp windshear layer as first described by Lord Rayleigh in 1883 and later developed with Pennycuick’s (2002) description of albatrosses “gust soaring.” In gust soaring a bird exploits structures in the wind field, such as separated boundary layers and eddies in the lee of wave crests, to obtain energy by climbing headed upwind and descending headed downwind across a thin wind-shear layer. Benefits of the model are that it is simple to understand, it captures the essential dynamics of wind-shear soaring, and it provides reasonable estimates of the minimum wind shear required for travel velocity in different directions with respect to the wind. Travel velocities, given in a travel velocity polar diagram, can be combined with tacking to fly in an upwind direction faster than the wind speed located at the top of the wind-shear layer.en_US
dc.description.sponsorshipFunds for the R/V Seward Johnson cruise were provided by National Science Foundation Grant OCE95-28574.en_US
dc.format.mimetypeapplication/pdf
dc.language.isoen_USen_US
dc.relation.urihttps://doi.org/10.1016/j.pocean.2010.08.001
dc.titleHow do albatrosses fly around the world (almost) without flapping their wings?en_US
dc.title.alternativeHow do albatrosses fly around the world without flapping their wings?en_US
dc.typePreprinten_US


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