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  4. The impact of the ozone effective temperature on satellite validation using the Dobson spectrophotometer network
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The impact of the ozone effective temperature on satellite validation using the Dobson spectrophotometer network

Journal
Atmospheric Measurement Techniques
Date Issued
May 9, 2016
Author(s)
Koukouli, Maria Elissavet  
Zara, Marina  
Lerot, Christophe  
Fragkos, Konstantinos  
Balis, Dimitris S.  
van Roozendael, Michel  
Allart, Marcus Antonius Franciscus  
Van Der A, Ronald Johannes  
DOI
10.5194/amt-9-2055-2016
Abstract
The main aim of the paper is to demonstrate an approach for post-processing of the Dobson spectrophotometers' total ozone columns (TOCs) in order to compensate for their known stratospheric effective temperature (Teff) dependency and its resulting effect on the usage of the Dobson TOCs for satellite TOCs' validation. The Dobson observations employed are those routinely submitted to the World Ozone and Ultraviolet Data Centre (WOUDC) of the World Meteorological Organization, whereas the effective temperatures have been extracted from two sources: the European Space Agency, ESA, Ozone Climate Change Initiative, Ozone-CCI, GODFIT version 3 (GOME-type Direct FITting) algorithm applied to the GOME2/MetopA, GOME2A, observations as well as the one derived from the European Centre for Medium-Range Weather Forecasts (ECMWF) outputs. Both temperature sources are evaluated utilizing co-located ozonesonde measurements also retrieved from the WOUDC database. Both GODFIT-v3 and ECMWF Teffs are found to be unbiased against the ozonesonde observations and to agree with high correlation coefficients, especially for latitudes characterized by high seasonal variability in Teff. The validation analysis shows that, when applying the GODFIT-v3 effective temperatures in order to post-process the Dobson TOC, the mean difference between Dobson and GOME2A GODFIT-v3 TOCs moves from 0.63 ± 0.66 to 0.26 ± 0.46 % in the Northern Hemisphere and from 1.25 ± 1.20 to 0.80 ± 0.71 % in the Southern Hemisphere. The existing solar zenith angle dependency of the differences has been smoothed out, with near-zero dependency up to the 60-65° bin and the highest deviation decreasing from 2.38 ± 6.6 to 1.37 ± 6.4 % for the 80-85° bin. We conclude that the global-scale validation of satellite TOCs against collocated Dobson measurements benefits from a post-correction using suitably estimated Teffs.
Subjects

Europe

Eragrostis tef

air temperature

algorithm

GOME

model validation

Northern Hemisphere

ozone

ozonesonde

satellite data

seasonal variation

Southern Hemisphere

spectrophotometry

total ozone

zenith angle

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