| Document Date: 2005-11-17 16:58:47
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City Corvallis / Narragansett / / Company Over Georges Bank / THE NORTHERN FLANK OF GEORGES BANK / Sun / Georges Bank / Browns Bank / of Georges Bank / J. J. Bisagni / / Country United States / / Currency USD / / Event Environmental Issue / / Facility Oregon State University / University of Rhode Island / College of Oceanic / / IndustryTerm subsequent processing / cross-bank section / long-term mean cross-bank structures / along-bank gradients / ambient bank water / along-bank direction / bank edge / cross-bank position / ship cross-bank position / Internal wave energy / cool patch off-bank / patchy on-bank stratification / on-bank limit / off-bank stratification / bank / rapid cross-bank sections / off-bank-propagating / linear internal wave packets propagating off-bank / cross-bank velocities / Cross-bank sections / energy budget / outer bank / bank-edge processes / mixed and stratified groups / off-bank tidal flow / bank edge/slope region / energy / / NaturalFeature Northeast Channel / Gulf of Maine / / Organization American Geophysical Union / Graduate School / University of Rhode Island / Oregon State University / College of Oceanic and Atmospheric Sciences / / Person DALE ET AL / / Position Hunter / General / / Product M-16 / / ProgrammingLanguage R / / ProvinceOrState Maine / Rhode Island / Oregon / / PublishedMedium JOURNAL OF GEOPHYSICAL RESEARCH / /
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JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 108, NO. C11, 8009, doi:[removed]2002JC001327, 2003 The front on the Northern Flank of Georges Bank in spring: 1. Tidal and subtidal variability Andrew C. Dale,1 David S. Ullman,2 Jo