Royal Netherlands Meteorological Institute

 
 
 
Ozone over NL
 
Research
Chemistry and Climate
30-year reanalysis of total ozone based on satellite and surface measurements
Added: November 2010

A single coherent total ozone dataset, called the Multi Sensor Reanalysis (MSR), has been created from all available ozone column data measured by polar orbiting satellites in the near-ultraviolet Huggins band in the last thirty years. Fourteen total ozone satellite retrieval datasets from the instruments TOMS (on the satellites Nimbus-7 and Earth Probe), SBUV (Nimbus-7, NOAA-9, NOAA-11 and NOAA-16), GOME (ERS-2), SCIAMACHY (Envisat), OMI (EOS-Aura), and GOME-2 (Metop-A) have been used in the MSR. As first step a bias correction scheme is applied to all satellite observations, based on independent ground-based total ozone data from the World Ozone and Ultraviolet Data Center. The correction is a function of solar zenith angle, viewing angle, time (trend), and effective ozone temperature. As second step data assimilation was applied to create a global dataset of total ozone analyses. The data assimilation method is a sub-optimal implementation of the Kalman filter technique, and is based on a chemical transport model driven by ECMWF meteorological fields. The chemical transport model provides a detailed description of (stratospheric) transport and uses parameterisations for gas-phase and ozone hole chemistry. The MSR dataset results from a 30-year data assimilation run with the 14 corrected satellite datasets as input, and is available on a grid of 1 by 1.5 degree with a sample frequency of 6 h for the complete time period (1978-2008). The Observation-minus-Analysis (OmA) statistics show that the bias of the MSR analyses is less than 1% with an RMS standard deviation of about 2% as compared to the corrected satellite observations used.

The results of this study were recently published in Atmospheric Physics and Chemistry.

Examples of the analysed MSR ozone field in DU. The left panel shows a low pressure system over Western Europe on 15 April 1992. The right panel shows the split ozone hole over Antarctica on 24 September 2002.

 
 
Nitrogen oxide distribution simulated with the TM model
Nitrogen oxide distribution simulated with the TM model