Modeling of very low frequency motions during RIPEX
dc.contributor.author | Reniers, A.J.H.M. | |
dc.contributor.author | MacMahan, J.H. | |
dc.contributor.author | Thornton, E.B. | |
dc.contributor.author | Stanton, Timothy P. | |
dc.date.accessioned | 2015-08-11T23:52:54Z | |
dc.date.available | 2015-08-11T23:52:54Z | |
dc.date.issued | 2007 | |
dc.identifier.uri | http://hdl.handle.net/10945/45997 | |
dc.description.abstract | Numerical computations are used to explain the presence of Very Low Frequency motions (VLF's), with frequencies less than 0:004 Hz, in the rip current velocity signals observed during the RIPEX ¯eld experiment. Observations show that the VLF-motions are most intense within the surfzone and then quickly taper o® in the o®shore direction. By comparing computed VLF-intensity (Urms;vlf ) distributions in both the cross-shore and alongshore direction with observations in a qualitative sense, the most important contributions to the VLF-dynamics are established. VLF-motions at neighboring rip-channels are seen to interact in the computations, with stronger surfzone intensity for increasing bathymetric variation. The intermittent forcing by spatially varying wave-groups is essential in obtaining the correct Urms;vlf distribution in the cross-shore direction suggesting this is the predominant mechanism responsible for the generation of the VLF-motions observed during RIPEX. Computations also suggest that VLF-motions can occasionally propagate o®shore but are mostly con¯ned to the surfzone corresponding to surfzone eddies. | en_US |
dc.rights | This 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.title | Modeling of very low frequency motions during RIPEX | en_US |
dc.type | Article | en_US |
dc.contributor.department | Oceanography | en_US |