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dc.contributor.authorCheriton, Olivia M.
dc.contributor.authorMcPhee-Shaw, Erika E.
dc.contributor.authorShaw, William J.
dc.contributor.authorStanton, Timothy P.
dc.contributor.authorBellingham, James G.
dc.contributor.authorStorlazzi, Curt D.
dc.date.accessioned2015-08-19T23:08:15Z
dc.date.available2015-08-19T23:08:15Z
dc.date.issued2014
dc.identifier.citationCheriton, O. M., E. E. McPhee-Shaw, W. J. Shaw, T. P. Stanton, J. G. Bellingham, and C. D. Storlazzi (2014), Suspended particulate layers and internal waves over the southern Monterey Bay continental shelf: An important control on shelf mud belts ?, J. Geophys. Res. Oceans, 119, 428–444, doi:10.1002/2013JC009360.en_US
dc.identifier.urihttp://hdl.handle.net/10945/46126
dc.descriptionThe article of record as published may be located at http://dx.doi.org/10.1002/2013JC009360en_US
dc.description.abstractPhysical and optical measurements taken over the mud belt on the southern continental shelf of Monterey Bay, California documented the frequent occurrence of suspended particulate matter features, the majority of which were detached from the seafloor, centered 9–33 m above the bed. In fall 2011, an automated profiling mooring and fixed instrumentation, including a thermistor chain and upward-looking acoustic Doppler current profiler, were deployed at 70 m depth for 5 weeks, and from 12 to 16 October a long-range autonomous underwater vehicle performed across-shelf transects. Individual SPM events were uncorrelated with local bed shear stress caused by surface waves and bottom currents. Nearly half of all observed SPM layers occurred during 1 week of the study, 9–16 October 2011, and were advected past the fixed profiling mooring by the onshore phase of semidiurnal internal tide bottom currents. At the start of the 9–16 October period, we observed intense near-bed vertical velocities capable of lifting particulates into the middle of the water column. This ‘‘updraft’’ event appears to have been associated with nonlinear adjustment of high-amplitude internal tides over the mid and outer shelf. These findings suggest that nonlinear internal tidal motions can erode material over the outer shelf and that, once suspended, this SPM can then be transported shoreward to the middle and shallow sections of the mud belt. This represents a fundamental broadening of our understanding of how shelf mud belts may be built up and sustained.en_US
dc.description.sponsorshipThis project was funded by the National Science Foundation (grant OCE0961810 to McPhee-Shaw, Bellingham, Shaw, and Stanton), and by the U.S. Geological Survey.en_US
dc.rightsThis publication is a work of the U.S. Government as defined in Title 17, United States Code, Section 101. Copyright protection is not available for this work in the United States.en_US
dc.titleSuspended particulate layers and internal waves over the southern Monterey Bay continental shelf: An important control on shelf mud belts?en_US
dc.typeArticleen_US
dc.contributor.departmentOceanographyen_US


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