Uncertainties due to transport-parameter sensitivity in an efficient 3-D ocean-climate model

By N. Edwards, Robert Marsh. 2005

304 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/dca6995de8c8545aadc61ccc17f79143fc41ffb5

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

1. Stefan Rahmstorf
2. Gerrit Lohmann
3. J. Hargreaves
4. A. Ganopolski
5. Reto Knutti
6. A. Ridgwell
7. T. Lenton
8. Valerie N. Livina

In Global and Planetary Change

1. Reto Knutti
2. J. Hargreaves
3. A. Ridgwell
4. T. Lenton
5. Valerie N. Livina
6. A. Ganopolski
7. Robert Marsh
8. Stefan Rahmstorf

In Oceanography

1. A. Ridgwell
2. T. Lenton
3. J. Hargreaves
4. Valerie N. Livina
5. A. Ganopolski
6. Robert Marsh
7. Stefan Rahmstorf
8. Gerrit Lohmann

Citations in the corpus

• A modified method for detecting incipient bifurcations in a dynamical system (2007, methodology): “the C-GOLDSTEIN configuration [ Edwards and Marsh, 2005 ].”
• Thermohaline circulation hysteresis: A model intercomparison (2005, background): “Bern 2.5D zonally averaged, 3 basins zonally averaged energy moisture [Stocker et al., 1992] Bremen large-scale geostrophic energy balance [Prange et al., 2003] Climber-2 zonally averaged, 3 basins statistical-dynamical [Petoukhov et al., 2000] ECBilt-CLIO 3D primitive equations quasi-geostrophic [G”
• Carbon dioxide and climate impulse response functions for the computation of greenhouse gas metrics:a multi-model analysis (2012, unknown): “D energy moisture balance atmosphere and a thermodynamic-dynamic sea-ice model (Edwards and Marsh, 2005).”
• Regulation of atmospheric CO2 by deep‐sea sediments in an Earth system model (2007, methodology): “The GENIE-1 model is based on the fast climate model of Edwards and Marsh (2005), featuring a reduced physics (frictional geostrophic) 3-D ocean circulation model coupled to a 2-D energy-moisture balance model (EMBM) of the atmosphere and a dynamicthermodynamic sea-ice model and contains a represent”
• Assessing the potential long-term increase of oceanic fossil fuel CO 2 uptake due to CO 2 -calcification feedback (2007, unknown): “The inclusion of a climate component (Edwards and Marsh, 2005) in the GENIE-1 Earth system model allows us to assess the importance of changes in climate on the CO 2 -calcification feedback.”