Page 1 Validation by Model Assimilation and/or Satellite Intercomparison - ESRIN 9–13 December 2002 Monitoring of SCIAMACHY Total Column Ozone Using the DAO Ozone DAS Authors: N. Winslow, I. Stajner, R. Rood
Page 2 Validation by Model Assimilation and/or Satellite Intercomparison - ESRIN 9–13 December 2002 Outline Overview of the DAO Ozone DAS Monitoring of SCIAMACHY total column ozone (TOZ) all data data that passed a simple quality control Summary
Page 3 Validation by Model Assimilation and/or Satellite Intercomparison - ESRIN 9–13 December Statistical Analysis 1. Tracer Transport Model Winds Assimilated O3 Data: TOMS SBUV MLS Forecast & Observation Error Models 4. HALOE Sondes Monitored Data: SCIAMACHY (MIPAS GOMOS) 3. Analysis Short term forecast 3a. Analysis Increments 3b. Observations-Forecast (O-F)
Page 4 Validation by Model Assimilation and/or Satellite Intercomparison - ESRIN 9–13 December 2002 Overview of the Ozone DAS Tracer transport model (2x2.5) uses near real time fv-DAS winds with parameterized chemistry SBUV profile and total column values are actively assimilated SCIAMACHY total column values are monitored Software to actively assimilate MIPAS, GOMOS and SCHIAMCHY is being developed
Page 5 Validation by Model Assimilation and/or Satellite Intercomparison - ESRIN 9–13 December 2002 Results with all SCIAMACHY TOZ data Pds2Ascii v converts RV_2 to DAS format Geolocation matched to observations using dsr time Data screened with provided quality flag Daily global RMS of O-F residuals are very large, typically over 200 D.U.
Page 6 Validation by Model Assimilation and/or Satellite Intercomparison - ESRIN 9–13 December 2002 Results with all SCIAMACHY TOZ data Time series of the zonal daily RMS of O-F residuals (D.U.) Large values concentrated in southern and northern high latitudes Large values appear to be near the terminator of high solar zenith angles
Page 7 Validation by Model Assimilation and/or Satellite Intercomparison - ESRIN 9–13 December 2002 Time series of the zonal daily mean of reported error of observations (%) Larger and smaller values of precision follow a distribution similar to that seen in zonal daily RMS of O-F residuals Results with all SCIAMACHY TOZ data
Page 8 Validation by Model Assimilation and/or Satellite Intercomparison - ESRIN 9–13 December 2002 Daily regional mean of reported error in observations (%) Large values are concentrated in space Most (>99%) large RMS values correspond to a reported error larger than 1.2% or equal to 0.0% Results with all SCIAMACHY TOZ data
Page 9 Validation by Model Assimilation and/or Satellite Intercomparison - ESRIN 9–13 December 2002 Results with quality controlled SCIAMACHY TOZ Times series of the daily global RMS of O-F residuals Quality control is a range check: 100DU <ozone< 1000DU Daily global RMS between SCIAMACHY TOZ and DAO forecast of TOZ is between 30 and 40 D.U.
Page 10 Validation by Model Assimilation and/or Satellite Intercomparison - ESRIN 9–13 December 2002 Time series of the zonal RMS of O-F residuals (D.U.) Larger RMS O-F residuals concentrated in the northern and southern high latitudes Pattern similar to data without quality control, but magnitudes are smaller Results with quality controlled SCIAMACHY TOZ
Page 11 Validation by Model Assimilation and/or Satellite Intercomparison - ESRIN 9–13 December 2002 Time series of the zonal mean of O-F residuals (D.U.) SCIAMACHY TOZ lower than DOA TOZ forecast by 25, 30, and 35 D.U in the northern mid latitudes, tropics, and southern mid latitudes respectively Some evidence of the zonal pattern seen in data without quality control Results with quality controlled SCIAMACHY TOZ
Page 12 Validation by Model Assimilation and/or Satellite Intercomparison - ESRIN 9–13 December 2002 Regional means of O-F residuals (D.U.) Large values are concentrated in space Most (>99%) large RMS values correspond to a reported error larger than 1.2% or equal to 0.0% Results with quality controlled SCIAMACHY TOZ
Page 13 Validation by Model Assimilation and/or Satellite Intercomparison - ESRIN 9–13 December 2002 Summary of SCIAMACHY TOZ Monitoring Data without external quality control generates RMS O-F residuals larger than 200 D.U. Simple quality control reduces the global RMS of O-F residuals to D.U. Large O-F residuals are tightly concentrated in northern and southern high latitudes at what appear to be high solar zenith angles, but this information is not yet provided in the data Reported errors show a similar spatial distribution Quality controlled data tends to be smaller than forecasted total column ozone by about 35 D.U.