Abstract

Abstract. Measurements of total ozone column and effective cloud transmittance have been performed since 1995 at the three Norwegian sites Oslo/Kjeller, Andøya/Tromsø, and in Ny-Ålesund (Svalbard). These sites are a subset of nine stations included in the Norwegian UV monitoring network, which uses ground-based ultraviolet (GUV) multi-filter instruments and is operated by the Norwegian Radiation and Nuclear Safety Authority (DSA) and the Norwegian Institute for Air Research (NILU). The network includes unique data sets of high-time-resolution measurements that can be used for a broad range of atmospheric and biological exposure studies. Comparison of the 25-year records of GUV (global sky) total ozone measurements with Brewer direct sun (DS) measurements shows that the GUV instruments provide valuable supplements to the more standardized ground-based instruments. The GUV instruments can fill in missing data and extend the measuring season at sites with reduced staff and/or characterized by harsh environmental conditions, such as Ny-Ålesund. Also, a harmonized GUV can easily be moved to more remote/unmanned locations and provide independent total ozone column data sets. The GUV instrument in Ny-Ålesund captured well the exceptionally large Arctic ozone depletion in March/April 2020, whereas the GUV instrument in Oslo recorded a mini ozone hole in December 2019 with total ozone values below 200 DU. For all the three Norwegian stations there is a slight increase in total ozone from 1995 until today. Measurements of GUV effective cloud transmittance in Ny-Ålesund indicate that there has been a significant change in albedo during the past 25 years, most likely resulting from increased temperatures and Arctic ice melt in the area surrounding Svalbard.

Highlights

  • The amount of stratospheric ozone decreased significantly both globally and over Norway during the 1980s and 1990s (WMO, 2018; Svendby and Dahlback, 2004)

  • Corrected ground-based ultraviolet (GUV) total ozone column (TOC) have been compared to GOME-2A and OMI TM3DAM v4.1 (Eskes et al, 2003) data for Oslo, Andøya, and Ny-Ålesund

  • Système d’Analyse par Observation Zénithale (SAOZ)) data and that any offset between Brewer and satellite data most likely will be reflected by offset in GUV–GOME-2 and GUV–OMI ozone data

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Summary

Introduction

The amount of stratospheric ozone decreased significantly both globally and over Norway during the 1980s and 1990s (WMO, 2018; Svendby and Dahlback, 2004). This decrease was mainly caused by the release of ozone-depleting substances (ODSs). This network consists of nine ground-based ultraviolet (GUV) radiometers located at sites between 58 and 79◦ N (Fig. 1).

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