Index of /ftp/oceans/NOAA_Workshop/Buitenhuisy_Data

Icon  Name                                              Last modified      Size  Description
[DIR] Parent Directory                                                       -   
[   ] PISCES_1948_2004_Cflx.nc.gz                       08-Jun-2005 13:25   42M  
[   ] PIT1.0_ET_PEAU_1948_2004_DelC.nc.gz               14-Jun-2005 08:58   41M  
[   ] PIT1.0_ET_PEAU_Alkalini_1948_2004.nc.gz           03-Jun-2005 13:32  356M  
[   ] PIT1.0_ET_PEAU_CO2flux_1949_2004_month.nc.gz      01-Jun-2005 11:24  3.8M  
[   ] PIT1.0_ET_PEAU_DIC_1948_2004.nc.gz                03-Jun-2005 13:50  367M  
[   ] PIT1.0_ET_PEAU_MLD_1948_2004.nc.gz                01-Jun-2005 11:24  3.0M  
[   ] PIT1.0_ET_PEAU_O2_1948_2004_155W.nc.gz            01-Jun-2005 11:25  4.1M  
[   ] PIT1.0_ET_PEAU_O2_1948_2004_165W.nc.gz            01-Jun-2005 11:25  4.3M  
[   ] PIT1.0_ET_PEAU_PCO2_1949_2004_month.nc.gz         01-Jun-2005 11:25  3.4M  
[   ] PIT1.0_ET_PEAU_PO4_1948_2004.nc.gz                01-Jun-2005 11:44  421M  
[   ] PIT1.0_ET_PEAU_SAL_1948_2004_155W.nc.gz           01-Jun-2005 11:44  3.3M  
[   ] PIT1.0_ET_PEAU_SAL_1948_2004_165W.nc.gz           01-Jun-2005 11:44  3.3M  
[   ] PIT1.0_ET_PEAU_SSS_1948_2004.nc.gz                01-Jun-2005 11:45  9.0M  
[   ] PIT1.0_ET_PEAU_SST_1948_2004.nc.gz                01-Jun-2005 11:46  9.9M  
[   ] PIT1.0_ET_PEAU_TEMP_1948_2004_155W.nc.gz          01-Jun-2005 11:46  3.9M  
[   ] PIT1.0_ET_PEAU_TEMP_1948_2004_165W.nc.gz          01-Jun-2005 11:46  4.0M  
[   ] PIT1.0_ET_PEAU_U_1948_2004_155W.nc.gz             01-Jun-2005 11:46  4.2M  
[   ] PIT1.0_ET_PEAU_U_1948_2004_165W.nc.gz             01-Jun-2005 11:47  4.2M  
[   ] PIT1.0_ET_PEAU_V_1948_2004_155W.nc.gz             01-Jun-2005 11:47  4.2M  
[   ] PIT1.0_ET_PEAU_V_1948_2004_165W.nc.gz             01-Jun-2005 11:47  4.2M  
[   ] PIT1.0_ET_PEAU_atmco2_mlo_spo1765_2100.LF8.dat.gz 14-Jun-2005 08:50   18K  

(1) pco2(x,y,t)       PIT1.0_ET_PAIR_pCO2_1949_2003.nc
(2) CO2 flux(x,y,t)   PIT1.0_ET_PAIR_CO2_flux_1949_2003.nc
(3) SST(x,y,t)        PIT1.0_ET_PAIR_SST_1948_2003.nc
(4) SSS(x,y,t)        PIT1.0_ET_PAIR_SSS_1948_2003.nc
(5) Mixed layer depth(x,y,t)  (calculated with a delta-sigma-theta
of 0.125)             PIT1.0_ET_PAIR_MLD_1948_2003.nc

And 12-month model climatologies from 0-1000m
Climatologies based on the last 30 years of model results, both
because this apparently is the definition of a climatology, and
because the initial drift of PO4 stabilises around the middle of the 
70s (T and S stabilise much sooner). 

(6) u,v(x,y,t) at 15m PIT1.0_ET_PAIR_UCLIM_1974_2003.nc
                      PIT1.0_ET_PAIR_VCLIM_1974_2003.nc
(7) T(x,y,z,t)        PIT1.0_ET_PAIR_TCLIM_1974_2003.nc
(8) S(x,y,z,t)        PIT1.0_ET_PAIR_SCLIM_1974_2003.nc
(9) phosphate(x,y,z,t)PIT1.0_ET_PAIR_PO4CLIM_1974_2003.nc

>Along 155W, 165E, and 30N across the Pacific, 1980 to 2000
>Temperature, Salinity (y,z,t)
>Phosphate (y,z,t)
>Oxygen(y,z,t)

I have done these files North of 15N from 0-1000m also from Jan 1980
to Jan 2001 inclusive
PIT1.0_ET_PAIR_O2_1980_2000_155W.nc
PIT1.0_ET_PAIR_O2_1980_2000_165E.nc
PIT1.0_ET_PAIR_O2_1980_2000_30N.nc
PIT1.0_ET_PAIR_PO4_1980_2000_155W.nc
PIT1.0_ET_PAIR_PO4_1980_2000_165E.nc
PIT1.0_ET_PAIR_PO4_1980_2000_30N.nc
PIT1.0_ET_PAIR_TS_1980_2000_155W.nc
PIT1.0_ET_PAIR_TS_1980_2000_165E.nc
PIT1.0_ET_PAIR_TS_1980_2000_30N.nc

>DIC and Alk (x,z,t) from 1980-2000 across 30N
I have done this file in the Pacific over the whole water column
PIT1.0_ET_PAIR_DICALK_1980_2000_30N.nc

Due to the interpolation from the model grid to the regular grid the PO4, DIC,
Alk, and O2 also have values where there is no ocean.

These are preliminary results from the PISCES T
model. This is based on the PISCES model (Aumont et al. 2003, Bopp et
al. 2003), with an improved representation of mesozooplankton, based
on observations and a POC degradation rate that is dependent on
temperature (Buitenhuis et al., in preparation). This biogeochemical
model is coupled online to the GCM OPA, which has a longitudinal
resolution of 2 degrees, an latitudinal resolution of between 0.5
degrees in the tropics and at the poles, and 2 degrees in the
temperate regions (average 1.1 degrees), 30 vertical levels, with 10
in the top 100 m. It is forced by daily average values of winds and
fluxes from NCEP reanalysis.

Buitenhuis, Erik, Corinne Le Quйrй, Olivier Aumont, Grйgory Beaugrand,
Adrian Bunker, Andrew Hirst, Tsutomu Ikeda, Todd O'Brien, Sergey
Piontkovski, Dietmar Straile (in preparation) Biogeochemical fluxes
through mesozooplankton. To be submitted to GBC

Bopp L., K. E. Kohfeld, C. Le Quйrй, O. Aumont  (2003)  Dust impact on
marine biota and atmospheric CO2 during glacial
periods. Paleoceanography 18 (2) #24, 16 p. doi:10.10129/2002/PA000810

Aumont et al.   (2003)  An ecosystem model of the global ocean
including Fe, Si, P co-limitations.      GBC 17 (2) #29,
15p. 2001GB001745