Energy Dissipation Rates Project
Explanation of
Potential and Kinetic Energy
Model Results
CCSM (details)
Spectral Analysis
GFDL (details)
Spectral Analysis
Hadcm3 (details)
Spectral Analysis
Miroc (details)
Spectral Analysis
MOM4 (details)
Spectral Analysis
ORCA (details)
SODA (details)
Alpha calculation
References
Fedorov, A.V. Estimating net energy dissipation rates in the tropical ocean: diabatic effects on ENSO dynamics. Accepted by J. Climate with minor revisions.
Goddard L. and Philander S.G. (2000) The Energetics of El Niño and La Niña. Journal of Climate. P 1496
Model Details
Model Institution
CCSM3 NCAR
(
GFDL-CM2.0or2.1? GFDL (
MIROC3.2(hires) CCSR/NIES/FRCGC (
UKMO – HadCM3 Hadley Centre (
MOM4 GFDL
(
POP – ocean
only NCAR
(
Table 1.
Directory: alphacalculations/original_datafiles/IPCC/Hadcm3
IPCC Climate of the 20th Century Run.
Variables: rhopoto, tauu, ua, tos.
Resolution: monthly. Starts at 1900
Coupled model.
Ocean friction: In the mixed layer a K-theory scheme is used. (P&P 81) Below the upper layers the vertical diffusivity is an increasing function of depth only.
Horiz. Resolution: 1.25*1.25 in ocean, 2.5*3.75 in atmosphere.
Model details: www.metoffice.com/research/hadleycentre/models/HadCM3.html, Pope et al (2000), Gordon et al (2000)
IPCC run.
http://nomads.gfdl.noaa.gov/dods-data/gfdl_cm2_1/
pp/ocean/static/tripolar
CM2.1U-D4_1860-2000-AllForc_H1
Miroc3_2_hires from IPCC run
Directory: alphacalculations/original_datafiles/IPCC/miroc3_2_hires
Coupled Model
Horizontal resolution: Atmos - T106 spectral truncation, approximately equivalent to 1.125° long-lat grid. Ocean – 0.28125 zonally and 0.1875 meridionally.
Lateral mixing of momentum – Smagorinsky’s biharmonic viscosity.
Mom4ocean from GFDL
43 years from an ocean only model forced by observed wind-stress and surface fluxes.
Directory: alphacalculations/original_datafiles/mom4ocean
Large datafiles stored in /extra/jb842/store_full_mom4data as have to be <4Gig to be on external hard drive.
Region:
Pot_rho: x=119.5e:84.5w, y=15.19s:15.19n, k=1:30 or to 446.9m.
U & tau_x: x=120e:85w, y=15.56s:15.56n, k=1:30 or to 446.9m.

Density at the surface for t=1. Showing region for integration.
Resolution: Monthly.
Time: Jan 1, 1958 – Dec 31, 2000.
Source:
Downloaded from
John Dunne: jpd@gfdl.noaa.gov
Files – pot_rho.nc, temp.nc, tau_x.nc, u.nc tau_y.nc, v.nc
Find out: what windstress and surface fluxes were used? Have emailed John to find this out.
Calculations:

Rho_star
Data from IRI website: http://ingrid.ldeo.columbia.edu/SOURCES/.CARTON-GIESE/SODA/.v1p4p2/
Region x=119.25e:80.25W, y=30.25s:30.25n, k=1:19, time=Jan 58 to Dec 2001. Can get later data till 2004.
getdata.jnl – ferret file to save data sets from web.