Comparison of a coupled ocean-atmosphere model with and without oceanic eddy-induced advection. Part I: Ocean spinup and control integrations

By A. Hirst, S. O’Farrell, H. Gordon. 2000

136 citations recorded by the source corpus.

How researchers see this paper

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

Potential Enthalpy: A Conservative Oceanic Variable for Evaluating Heat Content and Heat Fluxes (2003, methodology): “For the same model data of Hirst et al. (2000) the difference between the meridional flux of « and of h0 is shown as the solid line with dots in Fig.”
Effects of climate‐driven primary production change on marine food webs: implications for fisheries and conservation (2010, methodology): “GCMs provide global coverage of physical changes in environmental variables driven by projected greenhouse gas emissions.”
Developments in ocean climate modelling (2000, background): “Additionally, the common choice of equal isopycnal diusion and GM90 thickness diusivities (e.g., Danabasoglu and McWilliams, 1995; England, 1995; Robitaille and Weaver, 1995; Duy et al., 1995, 1997; Hirst and McDougall, 1996, 1998; Hirst et al., 2000) renders the following ̄ux for isopycnal diu”
A Probability and Decision-Model Analysis of a Multimodel Ensemble of Climate Change Simulations (2001, background): “1998); Commonwealth Scientific and Industrial Research Organisation (CSIRO; Hirst et al. 2000); Geophysical Fluid Dynamics Laboratory (GFDL; Manabe et al.”
The CSIRO Mk3 climate system model (2002, methodology): “When this CSIRO Atmospheric Research Technical Paper No. 60 5 GM enhanced ocean model was subsequently coupled to the Mk2 AGCM, the climate drift that was experienced before was almost entirely eliminated (Hirst et al. 1996, 2000).”