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Slide 1 October 2011 Verification for polar regions Scores computed for polewards of 65° NB proposed for CBS is polewards of 60° Verification at ECMWF using available fields from other centres Done for Z500 only All verification against analysis (each centre against own analysis) ERA-Interim scores shown as reference (ERA is fixed model and assimilation system) Slide 1

Slide 1 October 2011 Verification for polar regions Scores computed for polewards of 65° NB proposed for CBS is polewards of 60° Verification at

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Page 1: Slide 1 October 2011 Verification for polar regions  Scores computed for polewards of 65°  NB proposed for CBS is polewards of 60°  Verification at

Slide 1

October 2011

Verification for polar regions Scores computed for polewards of 65°

NB proposed for CBS is polewards of 60°

Verification at ECMWF using available fields from other centres

Done for Z500 only

All verification against analysis (each centre against own analysis)

ERA-Interim scores shown as reference (ERA is fixed model and assimilation system)

Slide 1

Page 2: Slide 1 October 2011 Verification for polar regions  Scores computed for polewards of 65°  NB proposed for CBS is polewards of 60°  Verification at

Slide 2

ECMWF operational and ERA-Interim (1990-2011)

Z500 ACC=80%, 12-month moving average

N Pole: clear improvement in system around 2000, and consistently better than ERA beyond 2002. But the apparent change 2001-2002 and 2008-09 are matched in ERA

S Pole: clear sustained improvement in 1990s; still positive trend

ERA changes: either atmospheric variability or changes to observing system

October 2011 Slide 2

N Pole

S Pole

Page 3: Slide 1 October 2011 Verification for polar regions  Scores computed for polewards of 65°  NB proposed for CBS is polewards of 60°  Verification at

Slide 3

Comparison with other centres (2000-2011) N pole

Day 3 forecasts (T+72)

Z500, 12-month moving average

Each centre verified against own analysis

ERA-I shown for reference

October 2011 Slide 3

rms error

ACC

Page 4: Slide 1 October 2011 Verification for polar regions  Scores computed for polewards of 65°  NB proposed for CBS is polewards of 60°  Verification at

Slide 4

Comparison with other centres (2000-2011) S pole

Day 3 forecasts (T+72)

Z500, 12-month moving average

Each centre verified against own analysis

ERA-I shown for reference

October 2011 Slide 4

rms error

ACC

Page 5: Slide 1 October 2011 Verification for polar regions  Scores computed for polewards of 65°  NB proposed for CBS is polewards of 60°  Verification at

Slide 5

Comparison with other centres (2000-2011) N pole

Day 5 forecasts (T+120)

Z500, 12-month moving average

Each centre verified against own analysis

ERA-I shown for reference

October 2011 Slide 5

rms error

ACC

Page 6: Slide 1 October 2011 Verification for polar regions  Scores computed for polewards of 65°  NB proposed for CBS is polewards of 60°  Verification at

Slide 6

Comparison with other centres (2000-2011) S pole

Day 5 forecasts (T+120)

Z500, 12-month moving average

Each centre verified against own analysis

ERA-I shown for reference

NB some dates missing for CMC in 2009 – affects these scores for 2009 (other years OK)

October 2011 Slide 6

rms error

ACC

Page 7: Slide 1 October 2011 Verification for polar regions  Scores computed for polewards of 65°  NB proposed for CBS is polewards of 60°  Verification at

Slide 7

Comparison with other centres (2000-2011) N pole

Variability (activity) of forecast and analysis fields: standard deviation of anomalies

Day 5 forecasts (T+120)

Z500, 12-month moving average

ERA-I shown for reference

Compared to the analysis, Met Office forecast now rather underactive; CMC overactive (this can affect the rms errors)

NB some dates missing for CMC in 2009 – affects these scores for 2009 (other years OK)

October 2011 Slide 7

analysis

forecast

Page 8: Slide 1 October 2011 Verification for polar regions  Scores computed for polewards of 65°  NB proposed for CBS is polewards of 60°  Verification at

Slide 8

Comparison between analyses (N Pole)

Differences between the analyses of different centres

Z500 30 day moving average

Decrease over last decade in the difference between the analyses of different centres

October 2011 Slide 8

rms difference

mean difference

Page 9: Slide 1 October 2011 Verification for polar regions  Scores computed for polewards of 65°  NB proposed for CBS is polewards of 60°  Verification at

Slide 9

Comparison between analyses (S Pole)

Differences between the analyses of different centres

Z500 30 day moving average

Decrease over last decade in the difference between the analyses of different centres

October 2011 Slide 9

rms difference

mean difference

Page 10: Slide 1 October 2011 Verification for polar regions  Scores computed for polewards of 65°  NB proposed for CBS is polewards of 60°  Verification at

Slide 10

Comparison with other centres (JJA 2011) arctic

Mean scores over 3 months (June, July, August 2011)

Includes JMA

This for polewards of 60° (the new proposed CBS area)

All centres have slightly lower rmse and higher ACC for this larger area

In winter (DJF) it is opposite (error larger in the larger area, consistent with higher average activity towards mid-latitudes)

The definition of the area does not affect the relative performance of the different models

October 2011 Slide 10

Page 11: Slide 1 October 2011 Verification for polar regions  Scores computed for polewards of 65°  NB proposed for CBS is polewards of 60°  Verification at

Slide 11

Comparison with other centres (JJA 2011) N pole

Mean scores over 3 months (June, July, August 2011)

Includes JMA

This for polewards of 65° (for comparison with previous slide)

October 2011 Slide 11

Page 12: Slide 1 October 2011 Verification for polar regions  Scores computed for polewards of 65°  NB proposed for CBS is polewards of 60°  Verification at

Slide 12

Comparison with other centres (JJA 2011) antarctic

Mean scores over 3 months (June, July, August 2011)

Includes JMA

This for polewards of 60° (the new proposed CBS area)

October 2011 Slide 12