Mélanie JUZA Thierry PENDUFF Bernard BARNIER LEGI, Grenoble, FRANCE
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Transcript of Mélanie JUZA Thierry PENDUFF Bernard BARNIER LEGI, Grenoble, FRANCE
Regional accuracy of global ARGO-based Regional accuracy of global ARGO-based monthly mixed layer property estimates: monthly mixed layer property estimates:
depth, temperature, salinitydepth, temperature, salinity
Mélanie JUZAMélanie JUZAThierry PENDUFFThierry PENDUFFBernard BARNIER Bernard BARNIER
LEGI, Grenoble, FRANCELEGI, Grenoble, FRANCE
EGU, Vienna, Austria, April 18 th, 2008
Interest of ARGO array for climate
- Monitoring and research
Determination of the observable part of the ocean dynamics
- Accuracy of the ARGO array (OSSE approach)
Heat content within the mixed layer:
Regional accuracy of global ARGO-based Regional accuracy of global ARGO-based monthly mixed layer property estimates: monthly mixed layer property estimates:
depth, temperature, salinitydepth, temperature, salinity
0
0
MLDz
TdzCpMLHC
Datasets
Observations: ARGO floats
from ENACT-ENSEMBLES (Met Office Hadley Center observations datasets)
Datasets
1958-2004 numerical simulation : DRAKKAR ¼°
DRAKKAR Group 2007, Barnier et al 2006, Brodeau et al 2007, Penduff et al 2008
- NEMO code (ocean model OPA9 + sea-ice LIM2 + CFC11 + 14C)
- Global setup.
- Resolution: 1/4° . 46 vertical levels
- Interannual forcings 1958-2004: BULK formulae (COARE)
- Turbulent fluxes: atmospheric variables (from ERA40 reanalysis)
- Radiative fluxes: ISCCP satellite observations
- Precipitations (Xie and Arkin)
- Runoffs (Dai and Trenberth)
- Outputs: U , V, T, S, SSH … (5 day means)
Observations: ARGO floats
from ENACT-ENSEMBLES (Met Office Hadley Center observations datasets)
¼° Drakkar Model
Mixed Layer Depth
2004
Collocation of hydrographic data
ENACT/ENSEMBLEST,S(x,y,z,t) vertical profilesGlobal. ARGO. 1998-2004
MODELT,S(x,y,z,t)Global. 1998-2004
• Keep good data only• Quadrilinear collocation (obs. space)
COLLOCATEDOBSERVED and MODEL
T,S(x,y,z,t) profiles Dispersed in time and space
VALIDATION SAMPLING ERROR
Integrated quantities within the mixed layer
Statistical analysis
Simulated and observed MLD
ARGO
August 1998-2004 February 1998-2004
Mixed layer depths (MLD) (m)
1/4°
model
Realism of simulated and observed MLD quantities
Method for the analysis of mixed layer quantities
Distribution of Mixed Layer Depth / Temperature / Salinity / Heat and Salt Contents
Medians and percentiles 17% and 83%
Example: MLHC in North Atlantic
Median
17%
83%
0
0
MLDz
TdzCpMLHC
-- full model -- sub-sampled model (like ARGO)
SAMPLING ERROR
April
1998-2004
Sampling errors of MLHC in NATL
-- sub-sampled model
-- full model ¼°
Monthly cycles of MLHC (1998-2004): zone MNW-ATL
well observed seasonal cycle
small sampling error. JFM ~ 2 GJ/m2
jan mar may jul sep nov
16
14
12
10
8
6
4
2
0
ML
HC
(G
J/m
2 )
Sampling errors of MLHC at global scale
ARGO sampling error on monthly MLHC (1998-2004)
30° x 30° x 1 month bins (1998-2004)Error = <sub-sampled model> – <full model>
MLHC (J/m2)
too warm
too cold
Sampling errors of MLHC at global scale
ARGO sampling error on monthly MLHC (1998-2004)
30° x 30° x 1 month bins (1998-2004)Error = <sub-sampled model> – <full model>
MLHC (J/m2)
too warm
too cold
Sampling errors of MLHC at global scale
ARGO sampling error on monthly MLHC (1998-2004)
30° x 30° x 1 month bins (1998-2004)Error = <sub-sampled model> – <full model>
MLHC (J/m2)
too warm
too cold
Sampling errors of MLD and MLT
Regional sampling errors of MLHC, MLD, MLT
Sampling error of monthly MLHC/MLD/MLT (1998-2004)
Contribution of MLD / MLT to the ARGO sampling errors of MLHC
MLHC
North Atlantic
MLD
too warm
too cold
MLT
5°C too warm
5°C too cold
100m too shallow
100m too deep
0
0
MLDz
TdzCpMLHC
March
Regional sampling errors of MLHC, MLD, MLT
Sampling error of monthly MLHC/MLD/MLT (1998-2004)
Contribution of MLD / MLT to the ARGO sampling errors of MLHC
MLHC
North Atlantic
MLD
too warm
too cold
MLT
5°C too warm
5°C too cold
100m too shallow
100m too deep
Number of data per bin
March
Exact spatial distribution of ARGO floats
¼° model MLD & ARGO floats positions – mar 1998-2004
Regional sampling errors of MLHC, MLD, MLT
Sampling error of monthly MLHC/MLD/MLT (1998-2004)
Contribution of MLD / MLT to the ARGO sampling errors of MLHC
MLHC
North Atlantic
MLD
too warm
too cold
MLT
5°C too warm
5°C too cold
100m too shallow
100m too deep
¼° model MLD & ARGO floats positions – mar 1998-2004
- sub-sampled model
- full model ¼°
MLD
March
Preliminary estimates at global scale:
- ARGO sampling error in mixed layer
and Salinity and Salt Content …
- Dependence on spatial distribution of ARGO floats
Interest of numerical simulations to assess the accuracy of observation systems
Extend this assessment : to recent years (maximum ARGO coverage)
: toward the last 50 years (interannual cycles)
Conclusion-perspectives
Typical Max
Depth +/- 10 m +/- 100 m
Temperature +/- 1 °C +/- 5 °C
Heat content +/- 1 GJ/m2 +/- 5 GJ/m2