2008
DOI: 10.1016/j.ocemod.2008.06.004
|View full text |Cite
|
Sign up to set email alerts
|

Inverse barotropic tidal estimation for regional ocean applications

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1
1

Citation Types

0
35
0

Year Published

2008
2008
2023
2023

Publication Types

Select...
6
2
2

Relationship

0
10

Authors

Journals

citations
Cited by 54 publications
(35 citation statements)
references
References 63 publications
0
35
0
Order By: Relevance
“…The physical model is coupled to multiple biological models (Besiktepe et al, 2003;Tian et al, 2004) and acoustic models (Lam et al, 2009;Lermusiaux et al, 2010). The ocean physics is forced with high-resolution barotropic tides, estimated using nested coastal inversions (Logutov and Lermusiaux, 2008). Due to the complex multiconnected sea domains, all ocean fields are initialized here with new objective mapping schemes developed specifically for PhilEx, using fast marching methods Agarwal and Lermusiaux, 2010).…”
Section: Simulation Estimation and Assimilationmentioning
confidence: 99%
“…The physical model is coupled to multiple biological models (Besiktepe et al, 2003;Tian et al, 2004) and acoustic models (Lam et al, 2009;Lermusiaux et al, 2010). The ocean physics is forced with high-resolution barotropic tides, estimated using nested coastal inversions (Logutov and Lermusiaux, 2008). Due to the complex multiconnected sea domains, all ocean fields are initialized here with new objective mapping schemes developed specifically for PhilEx, using fast marching methods Agarwal and Lermusiaux, 2010).…”
Section: Simulation Estimation and Assimilationmentioning
confidence: 99%
“…Its modeling capabilities include implicit two-way nesting for multiscale hydrostatic primitive equation (PE) dynamics with a nonlinear free-surface [97] and a high-order finite element code on unstructured grids for non-hydrostatic processes also with a nonlinear free-surface [98][99][100]. Other MSEAS subsystems include: initialization schemes [101], nested data-assimilative tidal prediction and inversion [102]; fast-marching coastal objective analysis [103]; stochastic subgrid-scale models (e.g., [104,105]); generalized adaptable biogeochemical modeling systems; Lagrangian Coherent Structures; non-Gaussian data assimilation and adaptive sampling [106][107][108]; dynamically-orthogonal equations for uncertainty predictions [109][110][111]; and machine learning of model formulations [112]. e MSEAS software is used for basic and fundamental research and for realistic simulations and predictions in varied regions of the world's ocean [113][114][115][116][117][118][119][120], including monitoring [121], naval exercises including real-time acoustic-ocean predictions [122] and environmental management [123].…”
Section: Mseas Modeling System E Multidisciplinary Simulation Estimmentioning
confidence: 99%
“…These were from SW06 forecasts and/or hindcasts made with the oceanographic modeling and assimilation schemes of the Massachusetts Institute of Technology (MIT, Cambridge) Multidisciplinary Simulation, Estimation, and Assimilation System (MSEAS) [16]. This system included oceanographic primitive-equation models [17] and tidal models [18] with data assimilation and uncertainty prediction [8], [19]. The primitive-equation model used here was a new free-surface version of the Harvard Ocean Prediction System (HOPS) [20] completed at MIT.…”
Section: A Incorporating Salinity Information and Data-assimilated Omentioning
confidence: 99%