Energy Dissipation Rates Project

 

Explanation of Potential and Kinetic Energy

 

 

Exploring the wind work term

 

 

 

Model Results

 

CCSM (details)

Alpha calculation

Spectral Analysis

 

GFDL (details)

Alpha calculation

Spectral Analysis

W data

E data

 

 

Hadcm3 (details)

Hadcm3

Spectral Analysis

 

Miroc (details)

Miroc Alpha

Spectral Analysis

 

MOM4 (details)

Alpha calculation

Spectral Analysis

 

ORCA (details)

Alpha calculation

 

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 (USA)

 

GFDL-CM2.0or2.1?  GFDL (USA)

 

MIROC3.2(hires)      CCSR/NIES/FRCGC (Japan)

 

UKMO – HadCM3    Hadley Centre (UK)

 

MOM4                       GFDL (USA)

 

POP – ocean only       NCAR (USA)

 

 

Table 1.

 

 

CCSM

 

Hadcm3

 

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)

 

 

 

GFDL

 

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.

 

Image generated by ESP Ghostscript (device=ppmraw)

Density at the surface for t=1. Showing region for integration.

 

Resolution: Monthly.

 

Time: Jan 1, 1958 – Dec 31, 2000.

 

Source: Downloaded from Princeton. Directory from John Dunne /archive/jpd/lima/mom4_om3_43yearloop_new_sw/pp/ocean/ts/monthly/43yr/

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:

 

Image generated by ESP Ghostscript (device=ppmraw)

 

Rho_star

 

 

SODA

 

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.