The Max-Planck-Institute global ocean/sea ice model with orthogonal curvilinear coordinates

By S. Marsland, Helmuth Haak, Johann Jungclaus, M. Latif, Frank Röske. 2003

1,041 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/29a92ab88134fcc7a905d026659bbdddbafea54c

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Citations in the corpus

Seasonal prediction and predictability of the Asian winter temperature variability (2013, neutral): “T42 L19 MPI-OM1 2.5 lat 9 0.5 –2.5 lon L23 9 Roeckner et al. (1996) Marsland et al. (2003) METFR (M12) Meteo- France ARPEGE T63 L31 OPA 8.0 182GP 9 152GP L31 9 Déqué (2001) Madec et al. (1997) UKMO (M13) UKMO HadAM3 2.5 9 3.75L19 GloSea OGCM 1.25 9 0.3 –1.25 L40 9 Roeckner et al. (1996), Marsland…”
Two tales of initializing decadal climate predictions experiments with the ECHAM5/MPI-OM model (2012, background): “A couple of recent studies (Chronis et al. 2011; Bladé et al. 2011; Marullo et al. 2011) have presented observational evidence for strong atmospheric teleconnection from the North Atlantic to the Mediterranean region during both the winter and summer seasons.”
Climate and carbon-cycle variability over the last millennium (2010, methodology): “MPIOM applies a conformal mapping grid with a horizontal resolution ranging from 22 km to 350 km.”
The influence of a weakening of the atlantic meridional overturning circulation on ENSO (2006, methodology): “As part of the Coupled Model Intercomparison Project (CMIP; Collins and the CMIP Modeling Groups 2005; Meehl et al. 2005), waterhosing experiments were conducted under preindustrial or presentday climate conditions (Stouffer et al. 2006).”
Bi-decadal variability excited in the coupled ocean–atmosphere system by strong tropical volcanic eruptions (2012, methodology): “Ocean subgridscale parameterizations include a formulation of bottom boundary layer slope convection, an isopycnal diffusion scheme, and a Gent and McWilliams style eddy-induced mixing parameterization ( Marsland et al. 2003 ).”
The Max Planck Institute Grand Ensemble: Enabling the Exploration of Climate System Variability (2019, background): “6.1p1; Marsland et al., 2003), run on the GR15L40 grid.”
Max Planck Institute Earth System Model (MPI-ESM1.2) for the High-Resolution Model Intercomparison Project (HighResMIP) (2018, methodology): “2 (Marsland et al., 2003), was replaced by the more sophisticated Kprofile parameterization (KPP) scheme of Large et al. (1994).”
Carbon dioxide and climate impulse response functions for the computation of greenhouse gas metrics:a multi-model analysis (2012, positive): “The physical ocean model is MPIOM, which further includes a sea-ice model (Marsland et al., 2003) on a nominal 1.5 grid with higher resolution in the North Atlantic.”
How are seasonal prediction skills related to models’ performance on mean state and annual cycle? (2010, background): “…8.0 182GP 9 152GP L31 9 Deque (2001), Madec et al. (1997) UKMO (M13) UKMO HadAM3 2.5 9 3.75L19 GloSea OGCM 1.25 9 0.3–1.25 L40 9 Roeckner et al. (1996), Marsland et al. (2003) Model index used in figures is also shown the Bay of Bengal), the equatorial western Pacific, and tropical Brazil, but…”
Initializing Decadal Climate Predictions with the GECCO Oceanic Synthesis: Effects on the North Atlantic (2009, methodology): “A slope convection scheme has been included that allows for a better representation of the flow of statically unstable dense water over sills (e.g., the Denmark Strait and the Strait of Gibraltar; for details, see Marsland et al. 2003) and off shelves (e.g., the Arctic and Antarctic shelves).”
Accuracy assessment of global barotropic ocean tide models (2014, methodology): “The ocean model includes an embedded thermodynamic sea ice model and is based on the Max-Planck Institute Ocean Model [Marsland et al., 2003] but formulated on a tripolar grid.”
Tropical Atmosphere-Ocean Interactions in a Conceptual Framework (2009, background): “…ocean observations are scarce outside of the equatorial Pacific and prior to the mid-1980s, 208C isotherm depths are from an NCEP–NCAR reanalysis–forced simulation from 1948 to 2001 of the Max Planck Institute Ocean Model (MPI-OM) ocean general circulation model (OGCM; Marsland et al. 2003).”