Ocean dynamics and numerical modeling of canyons and shelfbreaks

Multiscale ocean dynamics and multi-resolution numerical modeling of canyons and shelfbreaks are outlined. The dynamics focus is on fronts, currents, tides, and internal tides/waves that occur in these regions. Due to the topographic gradients and strong internal field gradients, nonlinear terms and...

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Bibliographic Details
Main Authors: Haley, Patrick (Contributor), Mirabito, Chris (Contributor), Duda, Timothy (Author), Gawarkiewicz, Glen (Author), Lermusiaux, Pierre F. J. (Contributor)
Other Authors: Massachusetts Institute of Technology. Department of Mechanical Engineering (Contributor)
Format: Article
Language:English
Published: Acoustical Society of America (ASA), 2015-09-01T14:10:45Z.
Subjects:
Online Access:Get fulltext
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042 |a dc 
100 1 0 |a Haley, Patrick  |e author 
100 1 0 |a Massachusetts Institute of Technology. Department of Mechanical Engineering  |e contributor 
100 1 0 |a Lermusiaux, Pierre F. J.  |e contributor 
100 1 0 |a Haley, Patrick  |e contributor 
100 1 0 |a Mirabito, Chris  |e contributor 
700 1 0 |a Mirabito, Chris  |e author 
700 1 0 |a Duda, Timothy  |e author 
700 1 0 |a Gawarkiewicz, Glen  |e author 
700 1 0 |a Lermusiaux, Pierre F. J.  |e author 
245 0 0 |a Ocean dynamics and numerical modeling of canyons and shelfbreaks 
260 |b Acoustical Society of America (ASA),   |c 2015-09-01T14:10:45Z. 
856 |z Get fulltext  |u http://hdl.handle.net/1721.1/98283 
520 |a Multiscale ocean dynamics and multi-resolution numerical modeling of canyons and shelfbreaks are outlined. The dynamics focus is on fronts, currents, tides, and internal tides/waves that occur in these regions. Due to the topographic gradients and strong internal field gradients, nonlinear terms and non-hydrostatic dynamics can be significant. Computationally, a challenge is to achieve accurate simulations that resolve strong gradients over dynamically significant space- and time-scales. To do so, one component are high-order schemes that are more accurate for the same efficiency than lower-order schemes. A second is multi-resolution grids that allow optimized refinements, such as reducing errors near steep topography. A third are methods that allow to solve for multiple dynamics, e.g., hydrostatic and non-hydrostatic, seamlessly. To address these components, new hybridizable discontinuous Galerkin (HDG) finite-element schemes for (non)-hydrostatic physics including a nonlinear free-surface are introduced. The results of data-assimilative multi-resolution simulations are then discussed, using the primitive-equation MSEAS system and telescoping implicitly two-way nested domains. They correspond to collaborative experiments: (i) Shallow Water 06 (SW06) and the Integrated Ocean Dynamics and Acoustics (IODA) research in the Middle Atlantic Bight region; (ii) Quantifying, Predicting and Exploiting Uncertainty (QPE) in the Taiwan-Kuroshio region; and (iii) Philippines Straits Dynamics Experiment (PhilEx). 
546 |a en_US 
655 7 |a Article 
773 |t The Journal of the Acoustical Society of America