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AO 160 – OZVAL

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AO 160 – OZVAL V alidation of ENVISAT ozone products through assimilation in the MSDOL model: First results obtained with GOMOS. Authors: B. Théodore and the OZVAL team. Objectives. Data assimilation for ENVISAT stratospheric ozone measurements using the MSDOL model - PowerPoint PPT Presentation
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Page 1 Validation by Model Assimilation and/or satellite intercomparison - ESRIN 9-13 December 2002 AO 160 – OZVAL Validation of ENVISAT ozone products through assimilation in the MSDOL model: First results obtained with GOMOS Authors: B. Théodore and the OZVAL team
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Page 1: AO 160 – OZVAL

Page 1Validation by Model Assimilation and/or satellite intercomparison - ESRIN 9-13 December 2002

AO 160 – OZVAL

Validation of ENVISAT ozone products through assimilation in the MSDOL model: First results obtained

with GOMOS

Authors: B. Théodore and the OZVAL team

Page 2: AO 160 – OZVAL

Page 2Validation by Model Assimilation and/or satellite intercomparison - ESRIN 9-13 December 2002

Objectives

Data assimilation for ENVISAT stratospheric ozone measurements using the MSDOL model

Daily delivery of ozone profiles over selected stations at synoptic hours

Daily maps of assimilated ozone field at synoptic hours

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Page 3Validation by Model Assimilation and/or satellite intercomparison - ESRIN 9-13 December 2002

Comparison of GOMOS profiles with assimilated SMR data

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Page 4Validation by Model Assimilation and/or satellite intercomparison - ESRIN 9-13 December 2002

MSDOL

CTM driven by analysed ECMWF wind fields

Resolution: 2.5°x2.5°, 36 pressure levels between 240 to 0.3 hPa (10 to 62 km)

33 chemical species computed, semi-lagrangian transport

Sequential assimilation of O3 profiles

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Page 5Validation by Model Assimilation and/or satellite intercomparison - ESRIN 9-13 December 2002

Read Level2 products from their native format; Select useable data ; Convert concentrations to mixing ratios using

ECMWF temperature ; Compute matrix H : each selected point is located

on the model grid and the interplation coefficients are computed ;

Save these informations in a file (one file per profile).

Data pre-processing

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Page 6Validation by Model Assimilation and/or satellite intercomparison - ESRIN 9-13 December 2002

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Page 7Validation by Model Assimilation and/or satellite intercomparison - ESRIN 9-13 December 2002

Data selection: the good…

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Page 8Validation by Model Assimilation and/or satellite intercomparison - ESRIN 9-13 December 2002

Data selection: the bad…

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Page 9Validation by Model Assimilation and/or satellite intercomparison - ESRIN 9-13 December 2002

Data selection: the ugly !

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Page 10Validation by Model Assimilation and/or satellite intercomparison - ESRIN 9-13 December 2002

A first glance at the Southern hemisphere in September

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Page 11Validation by Model Assimilation and/or satellite intercomparison - ESRIN 9-13 December 2002

Ozone field at 31.4 hPa on Sep. 24th

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Page 12Validation by Model Assimilation and/or satellite intercomparison - ESRIN 9-13 December 2002

Difference between an analyse and the free running model

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Page 13Validation by Model Assimilation and/or satellite intercomparison - ESRIN 9-13 December 2002

Sequence of ozone fields at 31.4 hPa

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Page 14Validation by Model Assimilation and/or satellite intercomparison - ESRIN 9-13 December 2002

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Page 15Validation by Model Assimilation and/or satellite intercomparison - ESRIN 9-13 December 2002

Comparison with an ozone sounding at Marambio (64.23°S, 56.72°W)

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Page 16Validation by Model Assimilation and/or satellite intercomparison - ESRIN 9-13 December 2002

Comparison with Lidar profiles at Lauder (45.05°S, 169.68°E)

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Page 17Validation by Model Assimilation and/or satellite intercomparison - ESRIN 9-13 December 2002

An assimilation diagnostic: the quantity .

T -1v S v

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Page 18Validation by Model Assimilation and/or satellite intercomparison - ESRIN 9-13 December 2002

OmF vs.OmA

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Page 19Validation by Model Assimilation and/or satellite intercomparison - ESRIN 9-13 December 2002

Time evolution of the OmF

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Page 20Validation by Model Assimilation and/or satellite intercomparison - ESRIN 9-13 December 2002

Time evolution of the OmF/OmA

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Page 21Validation by Model Assimilation and/or satellite intercomparison - ESRIN 9-13 December 2002

Assimilation with (better) data selection

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Page 22Validation by Model Assimilation and/or satellite intercomparison - ESRIN 9-13 December 2002

Diagnostics

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Page 23Validation by Model Assimilation and/or satellite intercomparison - ESRIN 9-13 December 2002

Time evolution of the OmF/OmA

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Page 24Validation by Model Assimilation and/or satellite intercomparison - ESRIN 9-13 December 2002

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Page 25Validation by Model Assimilation and/or satellite intercomparison - ESRIN 9-13 December 2002

Conclusions

GOMOS profiles exhibit large oscillations

Error bars in GOMOS products are unreliable

Careful data selection allows good assimilation results for ozone

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Page 26Validation by Model Assimilation and/or satellite intercomparison - ESRIN 9-13 December 2002

Perspectives

assimilation of GOMOS data over upcoming validation campaigns

Assimilation of GOMOS “line densities” could help dealing with the “strong oscillations” problem


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