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dc.contributor.authorLentz, Steven J.  Concept link
dc.contributor.authorDavis, Kristen A.  Concept link
dc.contributor.authorChurchill, James H.  Concept link
dc.contributor.authorDeCarlo, Thomas M.  Concept link
dc.date.accessioned2017-06-07T14:52:08Z
dc.date.available2017-06-07T14:52:08Z
dc.date.issued2017-05-04
dc.identifier.citationJournal of Physical Oceanography 47 (2017): 1061-1075en_US
dc.identifier.urihttps://hdl.handle.net/1912/9017
dc.descriptionAuthor Posting. © American Meteorological Society, 2017. This article is posted here by permission of American Meteorological Society for personal use, not for redistribution. The definitive version was published in Journal of Physical Oceanography 47 (2017): 1061-1075, doi:10.1175/JPO-D-16-0248.1.en_US
dc.description.abstractA major challenge in modeling the circulation over coral reefs is uncertainty in the drag coefficient because existing estimates span two orders of magnitude. Current and pressure measurements from five coral reefs are used to estimate drag coefficients based on depth-average flow, assuming a balance between the cross-reef pressure gradient and the bottom stress. At two sites wind stress is a significant term in the cross-reef momentum balance and is included in estimating the drag coefficient. For the five coral reef sites and a previous laboratory study, estimated drag coefficients increase as the water depth decreases consistent with open channel flow theory. For example, for a typical coral reef hydrodynamic roughness of 5 cm, observational estimates, and the theory indicate that the drag coefficient decreases from 0.4 in 20 cm of water to 0.005 in 10 m of water. Synthesis of results from the new field observations with estimates from previous field and laboratory studies indicate that coral reef drag coefficients range from 0.2 to 0.005 and hydrodynamic roughnesses generally range from 2 to 8 cm. While coral reef drag coefficients depend on factors such as physical roughness and surface waves, a substantial fraction of the scatter in estimates of coral reef drag coefficients is due to variations in water depth.en_US
dc.description.sponsorshipThe Red Sea field program was supported by Awards USA 00002 and KSA 00011 made by KAUST to S. Lentz and J. Churchill. The Palau field program was funded by NSF Award OCE-1220529.en_US
dc.language.isoen_USen_US
dc.publisherAmerican Meteorological Societyen_US
dc.relation.urihttps://doi.org/10.1175/JPO-D-16-0248.1
dc.subjectOceanen_US
dc.subjectCurrentsen_US
dc.subjectWind stressen_US
dc.subjectBoundary layeren_US
dc.subjectSea levelen_US
dc.subjectTidesen_US
dc.titleCoral reef drag coefficients – water depth dependenceen_US
dc.typeArticleen_US
dc.identifier.doi10.1175/JPO-D-16-0248.1


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