Abstract

Abstract. The total column water vapour product from the Global Ozone Monitoring Experiment-2 on board Metop-A and Metop-B satellites (GOME-2/Metop-A and GOME-2/Metop-B) produced by the Satellite Application Facility on Ozone and Atmospheric Chemistry Monitoring (O3M SAF) is compared with co-located radiosonde observations and global positioning system (GPS) retrievals. The validation is performed using recently reprocessed data by the GOME Data Processor (GDP) version 4.7. The time periods for the validation are January 2007–July 2013 (GOME-2A) and December 2012–July 2013 (GOME-2B). The radiosonde data are from the Integrated Global Radiosonde Archive (IGRA) maintained by the National Climatic Data Center (NCDC). The ground-based GPS observations from the COSMIC/SuomiNet network are used as the second independent data source. We find a good general agreement between the GOME-2 and the radiosonde/GPS data. The median relative difference of GOME-2 to the radiosonde observations is −2.7 % for GOME-2A and −0.3 % for GOME-2B. Against the GPS, the median relative differences are 4.9 % and 3.2 % for GOME-2A and B, respectively. For water vapour total columns below 10 kg m−2, large wet biases are observed, especially against the GPS retrievals. Conversely, at values above 50 kg m−2, GOME-2 generally underestimates both ground-based observations.

Highlights

  • Water vapour is the most important greenhouse gas accounting for about 60 % of the greenhouse effect for clear skies (e.g. Kiehl and Trenberth, 1997)

  • To illustrate the overall agreement between the data sets, we present the scatter plots of the GOME-2A and GOME-2B measurements vs. the co-located radiosonde and Global positioning system (GPS) measurements

  • We have performed the global validation of O3M SAF total column water vapour from GOME-2A (January 2007 to August 2013) and GOME-2B (December 2012 to August 2013) using radiosonde data from the Integrated Global Radiosonde Archive (IGRA) archive and the GPS data from the COSMIC/SuomiNet network

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Summary

Introduction

Water vapour is the most important greenhouse gas accounting for about 60 % of the greenhouse effect for clear skies (e.g. Kiehl and Trenberth, 1997). The water vapour products from the GOME/ERS-2 and SCIAMACHY instruments, using similar measurement principles and retrieval algorithms as those used for GOME-2, have been extensively compared against the SSM/I observations. They were found to generally slightly underestimate the water vapour column in comparison to the SSM/I observations. We report the geophysical validation of the GOME-2 water vapour total column against both radiosonde observations and ground-based GPS measurements. The IGRA database contains soundings from several different radiosonde types with different processing and is, as a result, a rather inhomogeneous data set (Wang and Zhang, 2008) It is, widely used in climate studies and provides the longest available record of upper air temperatures and humidity.

Overall agreement
Scan angle dependency
30 Radiosonde
Season and latitude
Conclusions
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