Diurnal to decadal global forcing for ocean and sea-ice models: The data sets and flux climatologies

By G. Large, S. Yeager. 2004

1,245 citations recorded by the source corpus.

Subfields: Atmospheric Science, Oceanography

View Paper: https://www.semanticscholar.org/paper/66bad7c65df808c404864c84f6e12052d73a6754

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

In Oceanography

Citations in the corpus

An ERA40-based atmospheric forcing for global ocean circulation models (2010, methodology): “These unrealistically high values do not seem to be consistent with the near-zero imbalance of heat and freshwater of LYDS reported by Large and Yeager (2004).”
The Norwegian Earth System Model, NorESM1-M – Part 1: Description and basic evaluation of the physical climate (2013, background): “…MODIS (Greenwald, 2009; Seethala and Horváth, 2010),g ERA40 (Uppala et al., 2005),h JRA25 (Onogi et al., 2007),i NCEP (Kanamitsu et al., 2002),j LARYA (Large and Yeager, 2004, 2008),k ECMWF (Trenberth et al., 2011),l WHOI (Yu and Weller, 2007; Yu et al., 2008). and sea ice model and the land…”
The Impact of Abyssal Mixing Parameterizations in an Ocean General Circulation Model (2009, methodology): “The model was forced using an annually repeating cycle driving the CCSM ﬂux coupler with the climatological corrected ‘‘normal year’’ forcing of Large and Yeager (2004, 2009).”
Mesoscale to submesoscale wavenumber spectra in Drake Passage (2016, positive): “These ﬁelds are converted to surface ﬂuxes using the bulk formulae of Large and Yeager (2004) and the dynamic/ thermodynamic sea ice model of Losch et al. (2010).”
Is the thermohaline circulation changing (2006, methodology): “The global model cases were computed using the forcing fields of Large and Yeager (2004).”
Causes of Interannual–Decadal Variability in the Meridional Overturning Circulation of the Midlatitude North Atlantic Ocean (2008, methodology): “The surface boundary conditions used for the present ORCA simulations are based on the atmospheric datasets and formulations developed by Large and Yeager (2004) for global ocean–ice models; these have been suggested as a basic choice for the design of “coordinated ocean-ice reference experiments…”
Parameterization of mixed layer eddies. III: Implementation and impact in global ocean climate simulations (2010, background): “Further details of these forcing data sets and forcing formulation, including treatment of under-ice forcing and river runoff are found elsewhere (Large and Yeager, 2004; Danabasoglu et al., 2009).”
A multi-resolution approach to global ocean modeling (2013, methodology): “For the surface momentum flux, monthly mean wind stress is computed offline using 6-hourly ‘‘Normal Year’’ forcing data from the Coordinated Ocean-ice Reference Experiment (CORE, Large and Yeager, 2004) and bulk formulae of Large and Pond (1982).”
Iron availability limits the ocean nitrogen inventory stabilizing feedbacks between marine denitrification and nitrogen fixation (2007, background): “climate forcings are from a late 20th century NCAR-NCEP climatology [Large and Yeager, 2004].”
Eddy-permitting ocean circulation hindcasts of past decades (2007, background): “Comparison of CORE and DFS3 driven hindcasts is presently under investigation and already indicates new directions for improvements for the next forcing set (DFS4) now under construction.”
JRA-55 based surface dataset for driving ocean–sea-ice models (JRA55-do) (2018, methodology): “Following Large and Yeager (2004; 2009), who produced the CORE data using ISCCP-FD radiation, we compared the CERES data with buoy observations and evaluated the necessity of adjusting them before their application to the reference fields.”