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GODAE Inter-comparisons in the south western Pacific Ocean

Peter R. Oke, Gary B. Brassington, James Cummings, Marie Drevillon, Fabrice Hernandez and Matthew Martin

 

Introduction ● Quantitative Assessment ●  Qualitative Assessment

 

Introduction

The goals of this study are to:

-         to understand when, where and why different systems perform well, or poorly, so that all systems can be improved in terms of their modelling and data assimilation techniques.

-         determine whether some ocean processes are consistently well/poorly reproduced by all systems and to understand why.

 

Data

Comparisons are made between model products provided under the GODAE Inter-comparison activity. The important elements of the four operational ocean forecast systems considered here are summarised in Table 1. Of these systems, Bluelink and HYCOM are eddy-resolving, and FOAM and Mercator are eddy permitting. Bluelink, FOAM and Mercator all use z-level models, while HYCOM is characterised by a hybrid, adaptive vertical grid. Both FOAM and Mercator use the same model code and grid. All systems use different NWP flux products. The NWP fluxes for Bluelink, FOAM and HYCOM represent diurnal variability, while Mercator uses daily averaged fluxes.

 

Table 1: Model characteristics (in progress).

 

OMAPS-hc

OMAPS-fc BRAN

UKMet

HYCOM

Mercator

Model code

MOM4

MOM4

MOM4

NEMO

HYCOM

NEMO

Horizontal grid

1/10o

1/10o

1/10o

1/4o

1/12o

1/4o

Vertical grid

47 levels

47 levels

47 levels

50 levels

32 hybrid

50 levels

NWP fluxes

GASP 3-hr

GASP 3-hr

ECMWF 3-hr

UKMO 6-hr

NOGAPS 3-hr

ECMWF 1-d

Forecast range

7-d

7-d

7-d

5-d

7-d

7-d (14-d)

updating

twice weekly

twice weekly

weekly

daily

daily

daily (weekly)

Hindcast

11-d

11-d

n/a

1-d

5-d

14-d

SST data des AMSR-E des AMSR-E a/d AMSR-E tba tba tba
SLA data GTS atSLA GTS atSLA DM atSLA tba tba tba
T/S data GTS Argo/XBT GTS Argo/XBT DM Argo tba tba tba

 

All systems, except Bluelink, produce daily forecasts of at least 5-days. Each system uses a hindcast period to spin the model up prior to a forecast. FOAM uses a short hindcast period of 1-day, while all other systems use a hindcast period of at least 5-days.

 

Comparisons presented here are based on:

Bluelink ReANalysis – delayed mode quality controlled along-track altimeter data; NRT AMSR-E data, NRT Argo data (no XBT data), NRT ECMWF surface fluxes, 7-d update cycle.

OMAPS-hc – 6-9 days behind real-time hindcasts using OceanMAPS, the operational Bluelink forecast system.

OMAPS-fc – 3-4 days real-time forecasts using OceanMAPS, the operational Bluelink forecast system.

UKMetNowcasts from the operational system … correct?

HYCOM – 5-day behind real-time analyses … correct?

Mercator – 7-14-day behind real-time hindcasts using Mercator PSY3 system.

 

Quantitative Assessment

Comparisons are presented for four regions in the south western Pacific Ocean:

-         EAC region (149-165E, 38S-22S)

-         Coral Sea and PNG region (142.5-165E, 22S-EQ)

-         ACC region (140-180E, 60S-38S)

-         Central south Pacific region (165-180E, 38S-EQ).

These regions are chosen as a subset of the South-Pacific GODAE Inter-comparison region to isolate the different dynamical regimes of the South-Western Pacific Ocean circulation.

Click here for image (~80K)

 

Surface Drifting Buoys

Comparison of drifter-derived and modelled near-surface zonal and meridional velocities.

Model velocities are near the surface (Bluelink = 15 m; HYCOM = 10 m; Mercator = 10 m; UKMet = 1 m).

Data points where the observed speed is less than 10 cm/s are excluded from these calculations to eliminate errors in data processing (all comparisons degrade when these data points are included).

Click here for image (~80K)

 

Taylor diagram (see Taylor 2001; JGR-Atmos) showing comparisons between drifter-derived and modelled near-surface zonal (top) and meridional (bottom) velocities.

Click here for image for U (~300K)

Click here for image for V (~300K)

EAC Region:

Click here for image for U (~300K)

Click here for image for V (~300K)

Coral Sea and PNG region: as above

Click here for image for U (~300K)

Click here for image for V (~300K)

ACC region: as above

Click here for image for U (~300K)

Click here for image for V (~300K)
 

Central-west-south Pacific region: as above

Click here for image for U (~300K)

Click here for image for V (~300K)
 

 

SST

EAC Region: Time series of (a) anomaly correlation and (b) RMS difference between modelled SST and the Regional Australian Muliti-Sensor SST Analysis (RAMSSA) fields.

The statistics in the legend show the time-mean RMS difference and anomaly correlation.

We use the RAMSSA 1/12 degree resolution SST fields produced operationally at the BoM as described by Beggs (2007; BMRC Research Report; ~3.7M). RAMSSA is a GHRSST L4 product that produces a foundation SST estimate by combining AVHRR, AMSR-E, AATSR, and in situ buoy data using OI.

Click here for image (~200K)

Time series as above, except compared to AMSR-E SST observations (both ascending and descending).

Click here for image (~400K)

Taylor diagram (see Taylor 2001; JGR-Atmos) showing comparisons between AMSRE and modelled SST.

Click here for image (~280K)

Coral Sea and PNG region: as above

Click here for image (~200K)

Time series as above, except compared to AMSR-E SST observations (both ascending and descending).

Click here for image (~400K)

Taylor Diagram for comparison with AMSRE SST

Click here for image (~280K)

ACC region: as above

Click here for image (~200K)

Time series as above, except compared to AMSR-E SST observations (both ascending and descending).

Click here for image (~400K)

Taylor Diagram for comparison with AMSRE SST

Click here for image (~280K)

Central-west-south Pacific region: as above

Click here for image (~200K)

Time series as above, except compared to AMSR-E SST observations (both ascending and descending).

Click here for image (~400K)

Taylor Diagram for comparison with AMSRE SST

Click here for image (~280K)

 

SLA

EAC Region: Time series of (a) anomaly correlation and (b) RMS difference between modelled SLA and along-track SLA (from delayed-mode Jason, Envisat and GFO).

The statistics in the legend show the time-mean RMS difference and anomaly correlation.

Model sea-surface height is converted to SLA by removing the mean sea-level (mean dynamic topography) fields provided by each GODAE partner.

I spatial average for the region of interest has also been removed from each model field to eliminate any mean bias error.

Click here for image (~200K)

 

Taylor diagram (see Taylor 2001; JGR-Atmos) showing comparisons between along-track and modelled SLA.

Click here for image (~270K)

Coral Sea and PNG region: as above

 

Click here for image (~200K)

 

Taylor Diagram

Click here for image (~270K)

ACC region: as above

 

Click here for image (~200K)

 

Taylor Diagram

Click here for image (~270K)

Central-west-south Pacific region: as above

 

Click here for image (~200K)

 

Taylor Diagram

Click here for image (~270K)

 

Argo T/S

EAC Region: Profile of RMS difference between modelled and observed T and S.

Click here for image (~450K)

 

Taylor Diagram - generated after first converting T and S to anomalies from climatology.

Click here for image for T (~270K)

Click here for image for S (~270K)

Coral Sea and PNG region: as above

Click here for image (~450K)

 

Taylor Diagram

Click here for image for T (~270K)

Click here for image for S (~270K)

ACC region: as above

Click here for image (~450K)

 

Taylor Diagram

Click here for image for T (~270K)

Click here for image for S (~270K)

Central-west-south Pacific region: as above

Click here for image (~450K)

 

Taylor Diagram

Click here for image for T (~270K)

Click here for image for S (~270K)

 

Qualitative Assessment (in progress)

SST

An example of a series of side-by-side comparisons between modelled SST and observed SST in the EAC region.

Observed SST is a combination of 3-d averaged AMSR-E and 10-d composite AVHRR SST processed at CSIRO.

6-Feb-12-Mar -> Click here for image (~742KM)

19-Mar-23-Apr -> Click here for image (~742KM)

SLA

An example of a series of side-by-side comparisons between modelled SLA and observed SLA in the EAC region.

Observed SLA is a optimal interpolation map of all along-track altimeter data processed at CSIRO.

Click here for image (~1.2M)

XBT

Comparison between the observed and modelled potential temperature anomaly along the PX6 XBT line.

(a)            Region map showing XBT section.

(b)            Observed section

(c)             Observation-model comparisons at 1 m depth.

(d)            Observation-model comparisons at 50 m depth.

(e)            Observation-model comparisons at 200 m depth.

(f)              Observation-model comparisons at 400 m depth.

Model fields are plotted for selected depths that are common to all models.

Click here for image (~280K)

 

 

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