Total ozone trends at three northern high-latitude stations
International audience Afterthedecreaseofozone-depletingsubstances(ODSs)asaconsequenceoftheMontrealProtocol, it is still challenging to detect a recovery in the total column amount of ozone (total ozone) at northern high latitudes. To assess regional total ozone changes in the “ozone-recovery” perio...
Published in: | Atmospheric Chemistry and Physics |
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Main Authors: | , , , , , , , , |
Other Authors: | , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
HAL CCSD
2023
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Subjects: | |
Online Access: | https://insu.hal.science/insu-04060799 https://insu.hal.science/insu-04060799/document https://insu.hal.science/insu-04060799/file/acp-23-4165-2023.pdf https://doi.org/10.5194/acp-23-4165-2023 |
Summary: | International audience Afterthedecreaseofozone-depletingsubstances(ODSs)asaconsequenceoftheMontrealProtocol, it is still challenging to detect a recovery in the total column amount of ozone (total ozone) at northern high latitudes. To assess regional total ozone changes in the “ozone-recovery” period (2000–2020) at northern high latitudes, this study investigates trends from ground-based total ozone measurements at three stations in Norway (Oslo, Andøya, and Ny-Ålesund). For this purpose, we combine measurements from Brewer spectrophotome- ters, ground-based UV filter radiometers (GUVs), and a SAOZ (Système d’Analyse par Observation Zénithale) instrument. The Brewer measurements have been extended to work under cloudy conditions using the global ir- radiance (GI) technique, which is also presented in this study. We derive trends from the combined ground-based time series with the multiple linear regression model from the Long-term Ozone Trends and Uncertainties in the Stratosphere (LOTUS) project. We evaluate various predictors in the regression model and found that tropopause pressure and lower-stratospheric temperature contribute most to ozone variability at the three stations. We report significantly positive annual trends at Andøya (0.9 ± 0.7 % per decade) and Ny-Ålesund (1.5 ± 0.1 % per decade) and no significant annual trend at Oslo (0.1 ± 0.5 % per decade) but significantly positive trends in autumn at all stations. Finally we found positive but insignificant trends of around 3 % per decade in March at all three stations, which may be an indication of Arctic springtime ozone recovery. Our results contribute to a better understanding of regional total ozone trends at northern high latitudes, which is essential to assess how Arctic ozone responds to changes in ODSs and to climate change. |
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