Using Green's Functions to Calibrate an Ocean General Circulation Model
By Dimitris Menemenlis, Ichiro Fukumori, Tong Lee. 2005
216 citations recorded by the source corpus.
Subfields: Global and Planetary Change, Oceanography
View Paper: https://www.semanticscholar.org/paper/0e804afd6034dd5bb3d936f1769ffa32fd267405
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Global and Planetary Change
- Patrick Heimbach
- Carl Wunsch
- Lee-Lueng Fu
- Tong Lee
- Denis L. Volkov
- R. Kwok
- An Thai Nguyen
- Dimitris Menemenlis
In Oceanography
- Patrick Heimbach
- Carl Wunsch
- Lee-Lueng Fu
- Tong Lee
- Denis L. Volkov
- An Thai Nguyen
- R. Kwok
- Dimitris Menemenlis
Citations in the corpus
- Arctic ice-ocean simulation with optimized model parameters: Approach and assessment (2011, methodology): “3.1. Green’s Function Approach [14] Green’s functions provide a simple yet effective method to adjust general circulation model (GCM) parameters [ Menemenlis et al., 2005a ].”
- Development of a four‐dimensional variational coupled data assimilation system for enhanced analysis and prediction of seasonal to interannual climate variations (2008, methodology): “[22] In addition, in order to reduce model drift before the 4D-VAR experiment, we have made a preliminary tuning by introducing the following 7 parameters through use of the Green’s function method proposed by Menemenlis et al. [2005] : (1) the wind sensitivity parameter in the ocean mixed layer sc”
- Dynamically and Kinematically Consistent Global Ocean Circulation and Ice State Estimates (2013, methodology): “Sea ice models have been developed within the state estimation framework as fully coupled sub-systems influenced by and influencing the ocean circulation (Menemenlis et al., 2005a,b; Losch et al., 2010).”
- Eddy‐induced meridional heat transport in the ocean (2008, methodology): “An ECCO2 data synthesis is obtained by least-squares fit of a global full-depth-ocean and sea-ice configuration of the Massachusetts Institute of Technology general circulation model [Marshall et al., 1997] to the available satellite and in-situ data using the Green’s function method [ Menemenlis et”