2012
DOI: 10.1016/j.ocemod.2011.12.009
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Assimilation of glider and mooring data into a coastal ocean model

Abstract: This article appeared in a journal published by Elsevier. The attached copy is furnished to the author for internal non-commercial research and education use, including for instruction at the authors institution and sharing with colleagues.Other uses, including reproduction and distribution, or selling or licensing copies, or posting to personal, institutional or third party websites are prohibited. a b s t r a c tWe have applied an ensemble optimal interpolation (EnOI) data assimilation system to a high reso… Show more

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Cited by 38 publications
(28 citation statements)
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References 25 publications
(24 reference statements)
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“…The vertical coordinate system is a fixed staggered z coordinate grid, with a resolution of 1 m in the upper layers increasing to 10 m in the deeper layers. For model details on the modified physical grid see Jones et al (2012). This 3D BGC model is a modified version of that applied in the D'Entrecasteaux Channel, southeast Tasmania, Australia (Wild-Allen et al 2010).…”
Section: Resultsmentioning
confidence: 99%
“…The vertical coordinate system is a fixed staggered z coordinate grid, with a resolution of 1 m in the upper layers increasing to 10 m in the deeper layers. For model details on the modified physical grid see Jones et al (2012). This 3D BGC model is a modified version of that applied in the D'Entrecasteaux Channel, southeast Tasmania, Australia (Wild-Allen et al 2010).…”
Section: Resultsmentioning
confidence: 99%
“…These include: (1) physical and biogeochemical studies of offshore eddies (Baird et al, 2011), (2) characterization of internal tides and sediment resuspension (Boettger et al, 2015;Pattiaratchi and De Oliveira, 2016), and (3) examination of the influence of the East Australian Current on shelf dynamics (Schaeffer and Roughan, 2015). Schaeffer et al (2016) compiled a shelf climatology using Slocum glider data, and Jones et al (2012) 2016). Dense shelf water is formed when a decrease in temperature through cooling and/or an increase in salinity from evaporation increases the density of the inner shelf water (compared to that offshore).…”
Section: Science Highlightsmentioning
confidence: 99%
“…Information on the physical processes is typically obtained by applying hydrodynamic models. Once calibrated and verified against the observational data, the deterministic models then can be applied to explore a number of issues that can provide information for management practices [22,23].…”
Section: Introductionmentioning
confidence: 99%