Articles | Volume 21, issue 10
https://doi.org/10.5194/acp-21-7881-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-21-7881-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
GUV long-term measurements of total ozone column and effective cloud transmittance at three Norwegian sites
NILU – Norwegian Institute for Air Research, Kjeller, Norway
Bjørn Johnsen
Norwegian Radiation and Nuclear Safety Authority, Østerås, Norway
Arve Kylling
NILU – Norwegian Institute for Air Research, Kjeller, Norway
Arne Dahlback
Department of Physics, University of Oslo, Oslo, Norway
Germar H. Bernhard
Biospherical Instruments Inc., San Diego, CA, USA
Georg H. Hansen
NILU – Norwegian Institute for Air Research, Kjeller, Norway
Boyan Petkov
Department of Psychological Sciences, Health and Territory, D'Annunzio University, Chieti, Italy
National Research Council, Institute of Polar Sciences (CNR-ISP),
Bologna, Italy
Vito Vitale
National Research Council, Institute of Polar Sciences (CNR-ISP),
Bologna, Italy
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David Tichopád, Kamil Láska, Tove Svendby, Klára Čížková, Andrea Pazmiño, Boyan Petkov, and Ladislav Metelka
EGUsphere, https://doi.org/10.5194/egusphere-2025-3963, https://doi.org/10.5194/egusphere-2025-3963, 2025
This preprint is open for discussion and under review for Atmospheric Chemistry and Physics (ACP).
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This study examined changes in the total ozone column above three Antarctic stations in 2007–2023 using ground and satellite observations. Ozone changes were mainly influenced by stratospheric temperature and atmospheric circulation. A significant increase occurred at Marambio, and unusually warm conditions in September 2019 caused ozone to rise strongly over East Antarctica, improving understanding of how the ozone layer responds to environmental changes.
Leonie Bernet, Tove Svendby, Georg Hansen, Yvan Orsolini, Arne Dahlback, Florence Goutail, Andrea Pazmiño, Boyan Petkov, and Arve Kylling
Atmos. Chem. Phys., 23, 4165–4184, https://doi.org/10.5194/acp-23-4165-2023, https://doi.org/10.5194/acp-23-4165-2023, 2023
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After the severe destruction of the ozone layer, the amount of ozone in the stratosphere is expected to increase again. At northern high latitudes, however, such a recovery has not been detected yet. To assess ozone changes in that region, we analyse the amount of ozone above specific locations (total ozone) measured at three stations in Norway. We found that total ozone increases significantly at two Arctic stations, which may be an indication of ozone recovery at northern high latitudes.
Alena Dekhtyareva, Mark Hermanson, Anna Nikulina, Ove Hermansen, Tove Svendby, Kim Holmén, and Rune Grand Graversen
Atmos. Chem. Phys., 22, 11631–11656, https://doi.org/10.5194/acp-22-11631-2022, https://doi.org/10.5194/acp-22-11631-2022, 2022
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Despite decades of industrial activity in Svalbard, there is no continuous air pollution monitoring in the region’s settlements except Ny-Ålesund. The NOx and O3 observations from the three-station network have been compared for the first time in this study. It has been shown how the large-scale weather regimes control the synoptic meteorological conditions and determine the atmospheric long-range transport pathways and efficiency of local air pollution dispersion.
Stephen M. Platt, Øystein Hov, Torunn Berg, Knut Breivik, Sabine Eckhardt, Konstantinos Eleftheriadis, Nikolaos Evangeliou, Markus Fiebig, Rebecca Fisher, Georg Hansen, Hans-Christen Hansson, Jost Heintzenberg, Ove Hermansen, Dominic Heslin-Rees, Kim Holmén, Stephen Hudson, Roland Kallenborn, Radovan Krejci, Terje Krognes, Steinar Larssen, David Lowry, Cathrine Lund Myhre, Chris Lunder, Euan Nisbet, Pernilla B. Nizzetto, Ki-Tae Park, Christina A. Pedersen, Katrine Aspmo Pfaffhuber, Thomas Röckmann, Norbert Schmidbauer, Sverre Solberg, Andreas Stohl, Johan Ström, Tove Svendby, Peter Tunved, Kjersti Tørnkvist, Carina van der Veen, Stergios Vratolis, Young Jun Yoon, Karl Espen Yttri, Paul Zieger, Wenche Aas, and Kjetil Tørseth
Atmos. Chem. Phys., 22, 3321–3369, https://doi.org/10.5194/acp-22-3321-2022, https://doi.org/10.5194/acp-22-3321-2022, 2022
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Here we detail the history of the Zeppelin Observatory, a unique global background site and one of only a few in the high Arctic. We present long-term time series of up to 30 years of atmospheric components and atmospheric transport phenomena. Many of these time series are important to our understanding of Arctic and global atmospheric composition change. Finally, we discuss the future of the Zeppelin Observatory and emerging areas of future research on the Arctic atmosphere.
Panagiotis G. Kosmopoulos, Stelios Kazadzis, Alois W. Schmalwieser, Panagiotis I. Raptis, Kyriakoula Papachristopoulou, Ilias Fountoulakis, Akriti Masoom, Alkiviadis F. Bais, Julia Bilbao, Mario Blumthaler, Axel Kreuter, Anna Maria Siani, Kostas Eleftheratos, Chrysanthi Topaloglou, Julian Gröbner, Bjørn Johnsen, Tove M. Svendby, Jose Manuel Vilaplana, Lionel Doppler, Ann R. Webb, Marina Khazova, Hugo De Backer, Anu Heikkilä, Kaisa Lakkala, Janusz Jaroslawski, Charikleia Meleti, Henri Diémoz, Gregor Hülsen, Barbara Klotz, John Rimmer, and Charalampos Kontoes
Atmos. Meas. Tech., 14, 5657–5699, https://doi.org/10.5194/amt-14-5657-2021, https://doi.org/10.5194/amt-14-5657-2021, 2021
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Large-scale retrievals of the ultraviolet index (UVI) in real time by exploiting the modern Earth observation data and techniques are capable of forming operational early warning systems that raise awareness among citizens of the health implications of high UVI doses. In this direction a novel UVI operating system, the so-called UVIOS, was introduced for massive outputs, while its performance was tested against ground-based measurements revealing a dependence on the input quality and resolution.
Kaisa Lakkala, Jukka Kujanpää, Colette Brogniez, Nicolas Henriot, Antti Arola, Margit Aun, Frédérique Auriol, Alkiviadis F. Bais, Germar Bernhard, Veerle De Bock, Maxime Catalfamo, Christine Deroo, Henri Diémoz, Luca Egli, Jean-Baptiste Forestier, Ilias Fountoulakis, Katerina Garane, Rosa Delia Garcia, Julian Gröbner, Seppo Hassinen, Anu Heikkilä, Stuart Henderson, Gregor Hülsen, Bjørn Johnsen, Niilo Kalakoski, Angelos Karanikolas, Tomi Karppinen, Kevin Lamy, Sergio F. León-Luis, Anders V. Lindfors, Jean-Marc Metzger, Fanny Minvielle, Harel B. Muskatel, Thierry Portafaix, Alberto Redondas, Ricardo Sanchez, Anna Maria Siani, Tove Svendby, and Johanna Tamminen
Atmos. Meas. Tech., 13, 6999–7024, https://doi.org/10.5194/amt-13-6999-2020, https://doi.org/10.5194/amt-13-6999-2020, 2020
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The TROPOspheric Monitoring Instrument (TROPOMI) onboard the Sentinel-5 Precursor (S5P) satellite was launched on 13 October 2017 to provide the atmospheric composition for atmosphere and climate research. Ground-based data from 25 sites located in Arctic, subarctic, temperate, equatorial and Antarctic
areas were used for the validation of the TROPOMI surface ultraviolet (UV) radiation product. For most sites 60 %–80 % of TROPOMI data was within ± 20 % of ground-based data.
David Tichopád, Kamil Láska, Tove Svendby, Klára Čížková, Andrea Pazmiño, Boyan Petkov, and Ladislav Metelka
EGUsphere, https://doi.org/10.5194/egusphere-2025-3963, https://doi.org/10.5194/egusphere-2025-3963, 2025
This preprint is open for discussion and under review for Atmospheric Chemistry and Physics (ACP).
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This study examined changes in the total ozone column above three Antarctic stations in 2007–2023 using ground and satellite observations. Ozone changes were mainly influenced by stratospheric temperature and atmospheric circulation. A significant increase occurred at Marambio, and unusually warm conditions in September 2019 caused ozone to rise strongly over East Antarctica, improving understanding of how the ozone layer responds to environmental changes.
Germar H. Bernhard, George T. Janson, Scott Simpson, Raúl R. Cordero, Edgardo I. Sepúlveda Araya, Jose Jorquera, Juan A. Rayas, and Randall N. Lind
Atmos. Chem. Phys., 25, 819–841, https://doi.org/10.5194/acp-25-819-2025, https://doi.org/10.5194/acp-25-819-2025, 2025
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Several publications have reported that total column ozone (TCO) may oscillate during solar eclipses, whereas other researchers have not seen evidence of such fluctuations. Here, we try to resolve these contradictions by measuring variations in TCO during three solar eclipses. In all instances, the variability in TCO was within natural variability. We conclude that solar eclipses do not lead to measurable variations in TCO, drawing into question reports of much larger changes found in the past.
André R. Brodtkorb, Anna Benedictow, Heiko Klein, Arve Kylling, Agnes Nyiri, Alvaro Valdebenito, Espen Sollum, and Nina Kristiansen
Geosci. Model Dev., 17, 1957–1974, https://doi.org/10.5194/gmd-17-1957-2024, https://doi.org/10.5194/gmd-17-1957-2024, 2024
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It is vital to know the extent and concentration of volcanic ash in the atmosphere during a volcanic eruption. Whilst satellite imagery may give an estimate of the ash right now (assuming no cloud coverage), we also need to know where it will be in the coming hours. This paper presents a method for estimating parameters for a volcanic eruption based on satellite observations of ash in the atmosphere. The software package is open source and applicable to similar inversion scenarios.
Andrea Pazmiño, Florence Goutail, Sophie Godin-Beekmann, Alain Hauchecorne, Jean-Pierre Pommereau, Martyn P. Chipperfield, Wuhu Feng, Franck Lefèvre, Audrey Lecouffe, Michel Van Roozendael, Nis Jepsen, Georg Hansen, Rigel Kivi, Kimberly Strong, and Kaley A. Walker
Atmos. Chem. Phys., 23, 15655–15670, https://doi.org/10.5194/acp-23-15655-2023, https://doi.org/10.5194/acp-23-15655-2023, 2023
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The vortex-averaged ozone loss over the last 3 decades is evaluated for both polar regions using the passive ozone tracer of the chemical transport model TOMCAT/SLIMCAT and total ozone observations from the SAOZ network and MSR2 reanalysis. Three metrics were developed to compute ozone trends since 2000. The study confirms the ozone recovery in the Antarctic and shows a potential sign of quantitative detection of ozone recovery in the Arctic that needs to be robustly confirmed in the future.
Leonie Bernet, Tove Svendby, Georg Hansen, Yvan Orsolini, Arne Dahlback, Florence Goutail, Andrea Pazmiño, Boyan Petkov, and Arve Kylling
Atmos. Chem. Phys., 23, 4165–4184, https://doi.org/10.5194/acp-23-4165-2023, https://doi.org/10.5194/acp-23-4165-2023, 2023
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After the severe destruction of the ozone layer, the amount of ozone in the stratosphere is expected to increase again. At northern high latitudes, however, such a recovery has not been detected yet. To assess ozone changes in that region, we analyse the amount of ozone above specific locations (total ozone) measured at three stations in Norway. We found that total ozone increases significantly at two Arctic stations, which may be an indication of ozone recovery at northern high latitudes.
Huan Yu, Claudia Emde, Arve Kylling, Ben Veihelmann, Bernhard Mayer, Kerstin Stebel, and Michel Van Roozendael
Atmos. Meas. Tech., 15, 5743–5768, https://doi.org/10.5194/amt-15-5743-2022, https://doi.org/10.5194/amt-15-5743-2022, 2022
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In this study, we have investigated the impact of 3D clouds on the tropospheric NO2 retrieval from UV–visible sensors. We applied standard NO2 retrieval methods including cloud corrections to synthetic data generated by the 3D radiative transfer model. A sensitivity study was done for synthetic data, and dependencies on various parameters were investigated. Possible mitigation strategies were investigated and compared based on 3D simulations and observed data.
Kostas Eleftheratos, John Kapsomenakis, Ilias Fountoulakis, Christos S. Zerefos, Patrick Jöckel, Martin Dameris, Alkiviadis F. Bais, Germar Bernhard, Dimitra Kouklaki, Kleareti Tourpali, Scott Stierle, J. Ben Liley, Colette Brogniez, Frédérique Auriol, Henri Diémoz, Stana Simic, Irina Petropavlovskikh, Kaisa Lakkala, and Kostas Douvis
Atmos. Chem. Phys., 22, 12827–12855, https://doi.org/10.5194/acp-22-12827-2022, https://doi.org/10.5194/acp-22-12827-2022, 2022
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We present the future evolution of DNA-active ultraviolet (UV) radiation in view of increasing greenhouse gases (GHGs) and decreasing ozone depleting substances (ODSs). It is shown that DNA-active UV radiation might increase after 2050 between 50° N–50° S due to GHG-induced reductions in clouds and ozone, something that is likely not to happen at high latitudes, where DNA-active UV radiation will continue its downward trend mainly due to stratospheric ozone recovery from the reduction in ODSs.
Alena Dekhtyareva, Mark Hermanson, Anna Nikulina, Ove Hermansen, Tove Svendby, Kim Holmén, and Rune Grand Graversen
Atmos. Chem. Phys., 22, 11631–11656, https://doi.org/10.5194/acp-22-11631-2022, https://doi.org/10.5194/acp-22-11631-2022, 2022
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Despite decades of industrial activity in Svalbard, there is no continuous air pollution monitoring in the region’s settlements except Ny-Ålesund. The NOx and O3 observations from the three-station network have been compared for the first time in this study. It has been shown how the large-scale weather regimes control the synoptic meteorological conditions and determine the atmospheric long-range transport pathways and efficiency of local air pollution dispersion.
Arve Kylling, Claudia Emde, Huan Yu, Michel van Roozendael, Kerstin Stebel, Ben Veihelmann, and Bernhard Mayer
Atmos. Meas. Tech., 15, 3481–3495, https://doi.org/10.5194/amt-15-3481-2022, https://doi.org/10.5194/amt-15-3481-2022, 2022
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Atmospheric trace gases such as nitrogen dioxide (NO2) may be measured by satellite instruments sensitive to solar ultraviolet–visible radiation reflected from Earth and its atmosphere. For a single pixel, clouds in neighbouring pixels may affect the radiation and hence the retrieved trace gas amount. We found that for a solar zenith angle less than about 40° this cloud-related NO2 bias is typically below 10 %, while for larger solar zenith angles the NO2 bias is on the order of tens of percent.
Cynthia H. Whaley, Rashed Mahmood, Knut von Salzen, Barbara Winter, Sabine Eckhardt, Stephen Arnold, Stephen Beagley, Silvia Becagli, Rong-You Chien, Jesper Christensen, Sujay Manish Damani, Xinyi Dong, Konstantinos Eleftheriadis, Nikolaos Evangeliou, Gregory Faluvegi, Mark Flanner, Joshua S. Fu, Michael Gauss, Fabio Giardi, Wanmin Gong, Jens Liengaard Hjorth, Lin Huang, Ulas Im, Yugo Kanaya, Srinath Krishnan, Zbigniew Klimont, Thomas Kühn, Joakim Langner, Kathy S. Law, Louis Marelle, Andreas Massling, Dirk Olivié, Tatsuo Onishi, Naga Oshima, Yiran Peng, David A. Plummer, Olga Popovicheva, Luca Pozzoli, Jean-Christophe Raut, Maria Sand, Laura N. Saunders, Julia Schmale, Sangeeta Sharma, Ragnhild Bieltvedt Skeie, Henrik Skov, Fumikazu Taketani, Manu A. Thomas, Rita Traversi, Kostas Tsigaridis, Svetlana Tsyro, Steven Turnock, Vito Vitale, Kaley A. Walker, Minqi Wang, Duncan Watson-Parris, and Tahya Weiss-Gibbons
Atmos. Chem. Phys., 22, 5775–5828, https://doi.org/10.5194/acp-22-5775-2022, https://doi.org/10.5194/acp-22-5775-2022, 2022
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Air pollutants, like ozone and soot, play a role in both global warming and air quality. Atmospheric models are often used to provide information to policy makers about current and future conditions under different emissions scenarios. In order to have confidence in those simulations, in this study we compare simulated air pollution from 18 state-of-the-art atmospheric models to measured air pollution in order to assess how well the models perform.
Aki Virkkula, Henrik Grythe, John Backman, Tuukka Petäjä, Maurizio Busetto, Christian Lanconelli, Angelo Lupi, Silvia Becagli, Rita Traversi, Mirko Severi, Vito Vitale, Patrick Sheridan, and Elisabeth Andrews
Atmos. Chem. Phys., 22, 5033–5069, https://doi.org/10.5194/acp-22-5033-2022, https://doi.org/10.5194/acp-22-5033-2022, 2022
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Optical properties of surface aerosols at Dome C, Antarctica, in 2007–2013 and their potential source areas are presented. The equivalent black carbon (eBC) mass concentrations were compared with eBC measured at three other Antarctic sites: the South Pole (SPO) and two coastal sites, Neumayer and Syowa. Transport analysis suggests that South American BC emissions are the largest contributor to eBC at Dome C.
Christine D. Groot Zwaaftink, Wenche Aas, Sabine Eckhardt, Nikolaos Evangeliou, Paul Hamer, Mona Johnsrud, Arve Kylling, Stephen M. Platt, Kerstin Stebel, Hilde Uggerud, and Karl Espen Yttri
Atmos. Chem. Phys., 22, 3789–3810, https://doi.org/10.5194/acp-22-3789-2022, https://doi.org/10.5194/acp-22-3789-2022, 2022
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We investigate causes of a poor-air-quality episode in northern Europe in October 2020 during which EU health limits for air quality were vastly exceeded. Such episodes may trigger measures to improve air quality. Analysis based on satellite observations, transport simulations, and surface observations revealed two sources of pollution. Emissions of mineral dust in Central Asia and biomass burning in Ukraine arrived almost simultaneously in Norway, and transport continued into the Arctic.
Claudia Emde, Huan Yu, Arve Kylling, Michel van Roozendael, Kerstin Stebel, Ben Veihelmann, and Bernhard Mayer
Atmos. Meas. Tech., 15, 1587–1608, https://doi.org/10.5194/amt-15-1587-2022, https://doi.org/10.5194/amt-15-1587-2022, 2022
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Retrievals of trace gas concentrations from satellite observations can be affected by clouds in the vicinity, either by shadowing or by scattering of radiation from clouds in the clear region. We used a Monte Carlo radiative transfer model to generate synthetic satellite observations, which we used to test retrieval algorithms and to quantify the error of retrieved NO2 vertical column density due to cloud scattering.
Stephen M. Platt, Øystein Hov, Torunn Berg, Knut Breivik, Sabine Eckhardt, Konstantinos Eleftheriadis, Nikolaos Evangeliou, Markus Fiebig, Rebecca Fisher, Georg Hansen, Hans-Christen Hansson, Jost Heintzenberg, Ove Hermansen, Dominic Heslin-Rees, Kim Holmén, Stephen Hudson, Roland Kallenborn, Radovan Krejci, Terje Krognes, Steinar Larssen, David Lowry, Cathrine Lund Myhre, Chris Lunder, Euan Nisbet, Pernilla B. Nizzetto, Ki-Tae Park, Christina A. Pedersen, Katrine Aspmo Pfaffhuber, Thomas Röckmann, Norbert Schmidbauer, Sverre Solberg, Andreas Stohl, Johan Ström, Tove Svendby, Peter Tunved, Kjersti Tørnkvist, Carina van der Veen, Stergios Vratolis, Young Jun Yoon, Karl Espen Yttri, Paul Zieger, Wenche Aas, and Kjetil Tørseth
Atmos. Chem. Phys., 22, 3321–3369, https://doi.org/10.5194/acp-22-3321-2022, https://doi.org/10.5194/acp-22-3321-2022, 2022
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Here we detail the history of the Zeppelin Observatory, a unique global background site and one of only a few in the high Arctic. We present long-term time series of up to 30 years of atmospheric components and atmospheric transport phenomena. Many of these time series are important to our understanding of Arctic and global atmospheric composition change. Finally, we discuss the future of the Zeppelin Observatory and emerging areas of future research on the Arctic atmosphere.
Panagiotis G. Kosmopoulos, Stelios Kazadzis, Alois W. Schmalwieser, Panagiotis I. Raptis, Kyriakoula Papachristopoulou, Ilias Fountoulakis, Akriti Masoom, Alkiviadis F. Bais, Julia Bilbao, Mario Blumthaler, Axel Kreuter, Anna Maria Siani, Kostas Eleftheratos, Chrysanthi Topaloglou, Julian Gröbner, Bjørn Johnsen, Tove M. Svendby, Jose Manuel Vilaplana, Lionel Doppler, Ann R. Webb, Marina Khazova, Hugo De Backer, Anu Heikkilä, Kaisa Lakkala, Janusz Jaroslawski, Charikleia Meleti, Henri Diémoz, Gregor Hülsen, Barbara Klotz, John Rimmer, and Charalampos Kontoes
Atmos. Meas. Tech., 14, 5657–5699, https://doi.org/10.5194/amt-14-5657-2021, https://doi.org/10.5194/amt-14-5657-2021, 2021
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Large-scale retrievals of the ultraviolet index (UVI) in real time by exploiting the modern Earth observation data and techniques are capable of forming operational early warning systems that raise awareness among citizens of the health implications of high UVI doses. In this direction a novel UVI operating system, the so-called UVIOS, was introduced for massive outputs, while its performance was tested against ground-based measurements revealing a dependence on the input quality and resolution.
Tijl Verhoelst, Steven Compernolle, Gaia Pinardi, Jean-Christopher Lambert, Henk J. Eskes, Kai-Uwe Eichmann, Ann Mari Fjæraa, José Granville, Sander Niemeijer, Alexander Cede, Martin Tiefengraber, François Hendrick, Andrea Pazmiño, Alkiviadis Bais, Ariane Bazureau, K. Folkert Boersma, Kristof Bognar, Angelika Dehn, Sebastian Donner, Aleksandr Elokhov, Manuel Gebetsberger, Florence Goutail, Michel Grutter de la Mora, Aleksandr Gruzdev, Myrto Gratsea, Georg H. Hansen, Hitoshi Irie, Nis Jepsen, Yugo Kanaya, Dimitris Karagkiozidis, Rigel Kivi, Karin Kreher, Pieternel F. Levelt, Cheng Liu, Moritz Müller, Monica Navarro Comas, Ankie J. M. Piters, Jean-Pierre Pommereau, Thierry Portafaix, Cristina Prados-Roman, Olga Puentedura, Richard Querel, Julia Remmers, Andreas Richter, John Rimmer, Claudia Rivera Cárdenas, Lidia Saavedra de Miguel, Valery P. Sinyakov, Wolfgang Stremme, Kimberly Strong, Michel Van Roozendael, J. Pepijn Veefkind, Thomas Wagner, Folkard Wittrock, Margarita Yela González, and Claus Zehner
Atmos. Meas. Tech., 14, 481–510, https://doi.org/10.5194/amt-14-481-2021, https://doi.org/10.5194/amt-14-481-2021, 2021
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This paper reports on the ground-based validation of the NO2 data produced operationally by the TROPOMI instrument on board the Sentinel-5 Precursor satellite. Tropospheric, stratospheric, and total NO2 columns are compared to measurements collected from MAX-DOAS, ZSL-DOAS, and PGN/Pandora instruments respectively. The products are found to satisfy mission requirements in general, though negative mean differences are found at sites with high pollution levels. Potential causes are discussed.
Kaisa Lakkala, Jukka Kujanpää, Colette Brogniez, Nicolas Henriot, Antti Arola, Margit Aun, Frédérique Auriol, Alkiviadis F. Bais, Germar Bernhard, Veerle De Bock, Maxime Catalfamo, Christine Deroo, Henri Diémoz, Luca Egli, Jean-Baptiste Forestier, Ilias Fountoulakis, Katerina Garane, Rosa Delia Garcia, Julian Gröbner, Seppo Hassinen, Anu Heikkilä, Stuart Henderson, Gregor Hülsen, Bjørn Johnsen, Niilo Kalakoski, Angelos Karanikolas, Tomi Karppinen, Kevin Lamy, Sergio F. León-Luis, Anders V. Lindfors, Jean-Marc Metzger, Fanny Minvielle, Harel B. Muskatel, Thierry Portafaix, Alberto Redondas, Ricardo Sanchez, Anna Maria Siani, Tove Svendby, and Johanna Tamminen
Atmos. Meas. Tech., 13, 6999–7024, https://doi.org/10.5194/amt-13-6999-2020, https://doi.org/10.5194/amt-13-6999-2020, 2020
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The TROPOspheric Monitoring Instrument (TROPOMI) onboard the Sentinel-5 Precursor (S5P) satellite was launched on 13 October 2017 to provide the atmospheric composition for atmosphere and climate research. Ground-based data from 25 sites located in Arctic, subarctic, temperate, equatorial and Antarctic
areas were used for the validation of the TROPOMI surface ultraviolet (UV) radiation product. For most sites 60 %–80 % of TROPOMI data was within ± 20 % of ground-based data.
Cited articles
Anderson, G. P., Clough, S. A., Kneizys, F. X., Chetwynd, J. H., and Shettle, E. P.: AFGL atmospheric constituent profiles (0–120 km), AFGL-TR-86-0110 Air Force Geophysics Laboratory, Hanscom Air Force Base, Massachusetts, 1987.
Antón, M. and Loyola, D.: Influence of cloud properties on satellite total ozone observations, J. Geophys. Res., 116, D03208, https://doi.org/10.1029/2010JD014780, 2011.
Bernhard, G.: Trends of solar ultraviolet irradiance at Barrow, Alaska, and
the effect of measurement uncertainties on trend detection, Atmos. Chem.
Phys., 11, 13029–13045, https://doi.org/10.5194/acp-11-13029-2011, 2011.
Bernhard, G., Booth, C. R., and Ehramjian, J. C.: Real-time ultraviolet and
column ozone from multichannel ultraviolet radiometers deployed in the National Science Foundation's ultraviolet monitoring network, Opt. Eng., 44, 041011-1–041011-12, 2005.
Bernhard, G., Dahlback, A., Fioletov, V., Heikkilä, A., Johnsen, B.,
Koskela, T., Lakkala, K., and Svendby, T.: High levels of ultraviolet radiation observed by ground-based instruments below the 2011 Arctic ozone hole, Atmos. Chem. Phys., 13, 10573–10590, https://doi.org/10.5194/acp-13-10573-2013, 2013.
Bernhard, G., Arola, A., Dahlback, A., Fioletov, V., Heikkilä, A.,
Johnsen, B., Koskela, T., Lakkala, K., Svendby, T., and Tamminen, J.: Comparison of OMI UV observations with ground-based measurements at high northern latitudes. Atmos. Chem. Phys., 15, 7391–7412, https://doi.org/10.5194/acp-15-7391-2015, 2015.
Bernhard, G., Fioletov, V. E., Grooß, J.-U., Ialongo, I., Johnsen, B.,
Lakkala, K., Manney, G. L., Müller, R., and Svendby, T. : Record-Breaking
Increases in Arctic Solar Ultraviolet Radiation Caused by Exceptionally
Large Ozone Depletion in 2020, Geophys. Res. Lett., 47, e2020GL090844, https://doi.org/10.1029/2020GL090844, 2020.
Dahlback, A.: Measurements of biologically effective UV doses, total ozone
abundances, and cloud effects with multichannel, moderate bandwidth filter
instruments, Appl. Optics, 35, 6514–6521, 1996.
Dahlback, A. and Stamnes, K.: A new spherical model for computing the radiation field available for photolysis and heating at twilight, Planet. Space Sci., 39, 671–683, 1991.
Dameris, M., Loyola, D. G., Nützel, M., Coldewey-Egbers, M., Lerot, C.,
Romahn, F., and van Roozendael, M.: Record low ozone values over the Arctic
in boreal spring 2020, Atmos. Chem. Phys., 21, 617–633,
https://doi.org/10.5194/acp-21-617-2021, 2021.
Degünther, M. and Meerkötter, R.: Influence of inhomogeneous surface
albedo on UV irradiance: effect of a stratus cloud, J. Geophys. Res., 105,
22755–22761, 2000.
Degünther, M., Meerkötter, R., Albold, A., and Seckmeyer, G.: Case study on the influence of inhomogeneous surface albedo on UV irradiance, Geophys. Res. Lett., 25, 3587–3590, 1998.
Eleftheratos, K., Kazadzis, S., Zerefos, C., Tourpali, K., Meleti, C., Balis, D., Zyrichidou, I., Lakkala, K., Feister, U., Koskela, T., Heikkilä, A., and Karhu, J. M.: Ozone and spectroradiometric UV changes in the past 20 years over high latitudes, Atmos.-Ocean, 53, 117–125,
https://doi.org/10.1080/07055900.2014.919897, 2015.
Eskes, H., van Velthoven, P., Valks, P., and Kelder, H.: Assimilation of GOME
total ozone satellite observations in a three-dimensional tracer transport
model, Q. J. Roy. Meteorol. Soc., 129, 1663–1681, https://doi.org/10.1256/qj.02.14, 2003.
Fioletov, V. E., Labow, G., Evans, R., Hare, E. W., Köhler, U, McElroy,
C. T., Miyagawa, K., Redondas, A., Savastiouk, V., Shalamyansky, A. M.,
Staehelin, J., Vanicek, K., and Weber, M.: Performance of the ground-based total ozone network assessed using satellite data, J. Geophys. Res., 113, D14313, https://doi.org/10.1029/2008JD009809, 2008.
Grooß, J.-U. and Müller, R.: Simulation of the record Arctic stratospheric ozone depletion in 2020, in: EGU General Assembly 2021, online, 19–30 April 2021, EGU21-2429, https://doi.org/10.5194/egusphere-egu21-2429, 2021.
Hendrick, F., Pommereau, J.-P., Goutail, F., Evans, R. D., Ionov, D.,
Pazmino, A. , Kyrö, E., Held, G., Eriksen, P., Dorokhov, V., Gil, M. , and Van Roozendael, M., NDACC/SAOZ UV-visible total ozone measurements: improved retrieval and comparison with correlative ground-based and satellite observations, Atmos. Chem. Phys., 11, 5975–5995,
https://doi.org/10.5194/acp-11-5975-2011, 2011.
Høiskar, B. A. K., Braathen, G. O., Dahlback, A., Bojkov, B. R., Edvardsen, K., Hansen, G.,and Svenøe, T. : Monitoring of the atmospheric ozone layer and natural ultraviolet radiation, Annual report 2000, Report 833/01, TA-1829/2001, NILU OR 35/2001, NILU, Kjeller, 2001.
Høiskar, B. A. K., Haugen, R., Danielsen, T., Kylling, A., Edvardsen, K.,
Dahlback, A., Johnsen, B., Blumthaler, M., and Schreder, J.: Multichannel
moderate-bandwidth filter instrument for measurement of the ozone-column
amount, cloud transmittance, and ultraviolet dose rates, Appl. Optics, 42,
3472–3479, https://doi.org/10.1364/ao.42.003472, 2003.
IPCC: Global warming of 1.5 ∘C, in: An IPCC Special Report on the impacts of global warming of 1.5 ∘C above pre-industrial levels and related global greenhouse gas emission pathways, in the context of strengthening the global response to the threat of climate change, sustainable development, and efforts to eradicate poverty, edited by:
Masson-Delmotte, V., Zhai, P., Pörtner, H. O., Roberts, D., Skea, J.,
Shukla, P. R., Pirani, A., Moufouma-Okia, W., Péan, C., Pidcock, R., Connors, S., Matthews, J. B. R., Chen, Y., Zhou, X., Gomis, M. I., Lonnoy, E., Maycock, T., Tignor, M., and Waterfield, T., available at: https://www.ipcc.ch/sr15/ (last acccess: 19 May 2021), 2018.
Johnsen, B., Kjeldstad, B., Aalerud, T. N., Nilsen, L. T., Schreder, J.,
Blumthaler, M., Bernhard, G., Topaloglou, C., Meinander, O., Bagheri, A.,
Slusser, J. R., and Davis, J.: Intercomparison and harmonization of UV index
measurements from multiband filter radiometers, J. Geophys. Res., 113, D15206, https://doi.org/10.1029/2007JD009731, 2008.
Johnsen, B., Svendby, T., and Dahlback, A.: Norwegian UV Network – minute data (Version v1.0.0), Zenodo, https://doi.org/10.5281/zenodo.4043039, 2020.
Karppinen, T., Redondas, A., García, R. D., Lakkala, K., McElroy, C. T.,
and Kyrö, E.: Compensating for the Effects of Stray Light in Single-Monochromator Brewer Spectrophotometer Ozone Retrieval,
Atmos.-Ocean, 53, 66–73, https://doi.org/10.1080/07055900.2013.871499, 2015.
Kylling, A. and Mayer, B.: Ultraviolet radiation in partly snow covered terrain: Observations and three-dimensional simulations, Geophys. Res. Lett., 28, 3665–3668, 2001.
Lakkala, K., Kujanpää, J., Brogniez, C., Henriot, N., Arola, A., Aun, M., Auriol, F., Bais, A. F., Bernhard, G., De Bock, V., Catalfamo, M., Deroo, C., Diémoz, H., Egli, L., Forestier, J.-B., Fountoulakis, I., Garcia, R. D., Gröbner, J., Hassinen, S., Heikkilä, A., Henderson, S., Hülsen, G., Johnsen, B., Kalakoski, N., Karanikolas, A., Karppinen,
T., Lamy, K., León-Luis, S. F., Lindfors, A. V., Metzger, J.-M., Minvielle, F., Muskatel, H. B., Portafaix, T., Redondas, A., Sanchez, R.,
Siani, A. M., Svendby, T., and Tamminen, J.: Validation of TROPOMI Surface UV Radiation Product, Atmos. Meas. Tech., 13, 6999–7024,
https://doi.org/10.5194/amt-13-6999-2020, 2020.
Lapeta, B., Engelsen, O., Litynska, Z., Kois, B., and Kylling, A.: Sensitivity of surface UV radiation and ozone column retrieval to ozone and temperature profiles, J. Geophys. Res., 105, 5001–5007, 2000.
Lawrence, Z. D., Perlwitz, J., Butler, A. H., Manney, G. L., Newman, P. A.,
Lee, S. H., and Nash, E. R.: The Remarkably Strong Arctic Stratospheric Polar
Vortex of Winter 2020: Links to Record-Breaking Arctic Oscillation and Ozone
Loss, J. Geophys. Res.-Atmos., 125, e2020JD033271, https://doi.org/10.1029/2020jd033271, 2020.
Lenoble, J.: Influence of the environment reflectance on the ultraviolet
zenith radiance for cloudless sky, Appl. Optics, 39, 4247–4254, 2000.
Manney, G. L., Livesey, N. J., Santee, M. L., Froidevaux, L., Lambert, A.,
Lawrence, Z. D., Millán, L. F., Neu, J. L., Read, W. G., Schwartz, M. J., and Fuller, R. A.: Record-low Arctic stratospheric ozone in 2020: MLS observations of chemical processes and comparisons with previous extreme winters, Geophys. Res. Lett., 47, e2020GL089063, https://doi.org/10.1029/2020gl089063, 2020.
Mayer, B., Kylling, A., Madronich, S., and Seckmeyer, G.: Enhanced Absorption of UV Radiation due to Multiple Scattering in Clouds: Experimental Evidence and Theoretical Explanation, J. Geophys. Res., 103, 31241–31254, 1998.
McPeters, R. D., Bhartia, P. K., Krueger, A. J., and Herman, J. R.: Nimbus-7
Total Ozone Mapping Spectrometer (TOMS) Data Products User's Guide, NASA
Reference Publication, NASA, available at: https://docserver.gesdisc.eosdis.nasa.gov/public/project/TOMS/NIMBUS7_USERGUIDE.PDF
(last access: 19 May 2021), 1996.
Möller, M. and Möller, R.: Modeling glacier-surface albedo across Svalbard for the 1979–2015 period: The HiRSvaC500-a data set, J. Adv. Model. Earth Syst., 9, 404–422, https://doi.org/10.1002/2016MS000752, 2017.
Norwegian Polar Institute: Sea ice extent in the Barents Sea in April, Environmental monitoring of Svalbard and Jan Mayen (MOSJ), available at:
http://www.mosj.no/en/climate/ocean/sea-ice-extent-barents-sea-fram-strait.html
(last access: 1 April 2021), 2020.
PMOD/WRC: Qasume site Audits, available at:
https://www.pmodwrc.ch/en/world-radiation-center-2/wcc-uv/qasume-site-audits/, last access: 19 May 2021, Protocol of the intercomparison at DSA, available at:
https://www.pmodwrc.ch/wcc_uv/qasume_audit/reports/2019_05_norway_olso.pdf (last access: 19 May 2021), 2019.
Pommereau, J. P. and Goutail, F.: O3 and NO2 ground-based measurements by visible spectrometry during Arctic winter and spring 1988, Geophys. Res. Lett., 15, 891–894, 1988.
Scarnato, B., Staehelin, J., Stübi, R., and Schill, H.: Long-term total
ozone observations at Arosa (Switzerland) with Dobson and Brewer instruments (1988–2007), J. Geophys. Res., 115, D13306, https://doi.org/10.1029/2009JD011908, 2010.
Schmalwieser, A. W., Gröbner, J., Blumthaler, M., Klotz, B., De Backer, H., Bolsée, D., Werner, R., Tomsic, D., Metelka, L., Eriksen, P., Jepsen, N., Aun, M., Heikkilä, A., Duprat, T., Sandmann, H., Weiss, T., Bais, A., Toth, Z., Siani, A. M., Vaccaro, L., Diémoz, H., Grifoni, D., Zipoli, G., Lorenzetto, G., Petkov, B. H., Giorgio di Sarra, A., Massen, F., Yousif, C., Aculinin, A. A., den Outer, P., Svendby, T., Dahlback, A., Johnsen, B., Biszczuk-Jakubowska, J., Krzyscin, J., Henriques, D., Chubarova, N., Kolarž, P., Mijatovic, Z., Groselj, D., Pribullova, A., Gonzales, J. R. M., Bilbao, J., Guerrero, J. M. V., Serrano, A., Andersson, S., Vuilleumier, L., Webbat, A., and O'Haganau, J.: UV Index monitoring in Europe, Photochem. Photobio. Sci., 16, 1349–1370, https://doi.org/10.1039/c7pp00178a, 2017.
Solomon, S.: Stratospheric ozone depletion: a review of concepts and history, Rev. Geophys., 37, 275–316, https://doi.org/10.1029/1999RG900008, 1999.
Stamnes, K., Tsay, S.-C., Wiscombe, W., and Jayaweera, K.: Numerically stable
algorithm for discrete-ordinate-method radiative transfer in multiple scattering and emitting layered media, Appl. Optics, 27, 2502–2509, https://doi.org/10.1364/AO.27.002502, 1988.
Stamnes, K., Pegau, S., and Frederick, J.: Uncertainties in total ozone amounts inferred from zenith sky observations: Implications for ozone trend
analyses, J. Geophys. Res., 95, 16523–16528, https://doi.org/10.1029/JD095iD10p16523, 1990.
Stamnes, K., Slusser, J., and Bowen, M.: Derivation of total ozone abundance and cloud effects from spectral irradiance measurements, Appl. Optics, 30,
4418–4426, 1991.
Stamnes, K., Thomas, G. E., and Stamnes, J. J.: Radiative Transfer in the
Atmosphere and Ocean, Cambridge University Press, Cambridge, 2017.
Svendby, T.: GUV total ozone column and effective cloud transmittance from three Norwegian sites 1995–2019 (Version v2.0) [Data set], Zenodo, https://doi.org/10.5281/zenodo.4773478, 2021.
Svendby, T. M. and Dahlback, A.: Twenty years of revised Dobson total ozone
measurements in Oslo, Norway, J. Geophys. Res., 107, 4369, https://doi.org/10.1029/2002JD002260, 2002.
Svendby, T. M. and Dahlback, A.: Statistical analysis of total ozone measurements in Oslo, Norway, 1978–1998, J. Geophys. Res., 109, D16107,
https://doi.org/10.1029/2004JD004679, 2004.
Svendby, T. M., Hansen, G. H., Bäcklund, A., and Nilsen, A.-C.: Monitoring of the atmospheric ozone layer and natural ultraviolet radiation, Annual report 2019, M-1768/2020, NILU, Kjeller, ISBN 978-82-425-3008-0, 2020.
Sztipanov, M., Tumeh, L., Li, W., Svendby, T., Kylling, A., Dahlback, A.,
Stamnes, J., Hansen, G. H., and Stamnes, K.: Ground-based measurements of total ozone column amount with a multichannel moderate-bandwidth filter instrument at the Troll research station, Antarctica, Appl. Optics, 59, 97–106, https://doi.org/10.1364/AO.59.000097, 2020.
WMO: Intercomparison of global UV index from multiband filter radiometers: Harmonization of global UVI and spectral irradiance, GAW report no. 179, WMO/TD-No. 1454, edited by: Johnsen, B., Kjeldstad, B., Aalerud, T. N., Nilsen, L. T., Schreder, J., Blumthaler, M., Bernhard, G., Topaloglou, C., Meinander, O., Bagheri, A., Slusser, J. R., and Davis, J., World
Meteorological Organization, Geneve, 2008.
WMO: Scientific assessment of ozone depletion: 2018, Global Ozone Research and Monitoring Project-Report No. 58, World Meteorological Organization, Geneva, available at: https://www.esrl.noaa.gov/csd/assessments/ozone/2018/ (last access: 19 May 2021), 2018.
Wohltmann, I., Gathen, P., Lehmann, R., Maturilli, M., Deckelmann, H.,
Manney, G. L., Davies, J., Tarasick, D., Jepsen, N., Kivi, R., Lyall, N., and Rex, M.: Near complete local reduction of Arctic stratospheric ozone by severe chemical loss in spring 2020, Geophys. Res. Lett., 47, e2020GL089547, https://doi.org/10.1029/2020gl089547, 2020.
WOUDC: WOUDC Contributor Guide (Version 2.1.3), available at:
https://guide.woudc.org/en/ (last access: 19 May 2021), 2019.
Wunderling, N., Willeit, M., Donges, J. F., and Winkelmann, R.: Global warming due to loss of large ice masses and Arctic summer sea ice, Nat.
Commun., 11, 5177, https://doi.org/10.1038/s41467-020-18934-3, 2020.
Short summary
Measurements of total ozone and effective cloud transmittance (eCLT) have been performed since 1995 at three Norwegian sites with GUV multi-filter instruments. The unique data sets of high-time-resolution measurements can be used for a broad range of studies. Data analyses reveal an increase in total ozone above Norway from 1995 to 2019. Measurements of GUV eCLT indicate changes in albedo in Ny-Ålesund (Svalbard) during the past 25 years, most likely resulting from increased Arctic ice melt.
Measurements of total ozone and effective cloud transmittance (eCLT) have been performed since...
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