Open boundary conditions for long-term integration of regional oceanic models

By Patrick Marchesiello, James C. McWilliams, Alexander F. Shchepetkin. 2001

1,005 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/95964ec76f771ddb00e10d9a7198d10f1e496e6c

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Citations in the corpus

Modelling the transport success of anchovy Engraulis encrasicolus eggs and larvae in the southern Benguela: the effect of spatio-temporal spawning patterns (2003, background): “At the 3 lateral boundaries facing the open ocean, a specific scheme (Marchesiello et al. 2001) connects the model solution to cyclic seasonal, time-averaged outputs of the ‘Agulhas as primitive equations’ (AGAPE) basin scale ocean model (Biastoch & Krauß 1999).”
Tracking coherent structures in a regional ocean model with wavelet analysis: Application to Cape Basin eddies - art. no. C05043 (2007, background): “At the four lateral boundaries facing the open ocean, the model solution is connected to the surroundings by an active, implicit, and upstream-biased radiation condition [ Marchesiello et al., 2001 ].”
A numerical study of stochastic larval settlement in the California Current system (2008, background): “toward prescribed climatological values (Marchesiello et al., 2001).”
B‐preconditioned minimization algorithms for variational data assimilation with the dual formulation (2014, background): “Terrain-following vertical coordinates are employed allowing for greater vertical resolution in shallow water and regions with complex bathymetry (Marchesiello et al., 2001; Shchepetkin and McWilliams, 2003, 2005; Haidvogel et al., 2008).”
Results from a three-dimensional, nested biological-physical model of the California Current System and comparisons with statistics from satellite imagery (2006, methodology): “[18] For the 3-D variables (U, V, and tracers) we use the radiation boundary condition with adaptive nudging described by Marchesiello et al. [2001, 2003] .”
The Regional Ocean Modeling System (ROMS) 4-dimensional variational data assimilation systems Part I - System overview and formulation (2011, background): “…is beyond the scope of this paper, however thorough descriptions of the numerical schemes, physical parameterizations, and open boundary condition options can be found in Shchepetkin and McWilliams (2003), Shchepetkin and McWilliams (2005), Marchesiello et al. (2001), and Haidvogel et al. (2008).”
Computation of the Streamfunction and Velocity Potential for Limited and Irregular Domains (2006, methodology): “The dataset used for demonstrating the proposed algorithm is derived from a three-dimensional Regional Ocean Modeling System (ROMS) (Shchepetkin and McWilliams 1998, 2003; Marchesiello et al. 2001, 2003).”
Revisiting open boundary conditions from the point of view of characteristic variables (2005, methodology): “The Flather condition has been used in some comparative studies (e.g. Palma and Matano, 1998; Marchesiello et al., 2001; Nycander and Döös, 2003), and it always appears to be one of the most efficient conditions.”
Generation and unstable evolution of a density‐driven Eastern Poleward Current: The Iberian Poleward Current (2003, methodology): “Active/passive boundary conditions [Marchesiello et al., 2000] were also used at the boundaries together with the relaxation terms.”
A coupled physical-biological model of the Northern Gulf of Mexico shelf: model description, validation and analysis of phytoplankton variability (2011, methodology): “The temperature and salinity boundary conditions use an adaptive nudging technique (Marchesiello et al., 2001) where tracers are relaxed to the horizontally uniform monthly climatology throughout the integration with a timescale of 10 days for outgoing information and 1 day for incoming information.”
Evolutionary individual-based model for the recruitment of anchovy (Engraulis capensis) in the southern Benguela (2002, background): “A specific open-boundary scheme has been developed for long-term integration of the model on limited size regional domains (Marchesiello et al. 2001; Penven et al. 2001a).”
Two-way nesting in split-explicit ocean models: Algorithms, implementation and validation (2012, neutral): “25(a)) exhibits the 3 large meanders of the CCS described by Marchesiello et al. (2003). In this new simulation, they appear slightly less prominent but they are similarly located: off Cape Mendocino, Monterey Bay and Point Conception.”
A finite-element ocean model: principles and evaluation (2004, background): “The boundary conditions at open boundaries are extensively discussed in the literature (see, e.g., the recent paper by Marchesiello et al. (2001)).”