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1. Substantial contribution of iodine to Arctic ozone destruction

Author

Benavent, Nuria, Mahajan, Anoop S., Li, Qinyi, Cuevas, Carlos A., Schmale, Julia, Angot, Hélène, Jokinen, Tuija, Quéléver, Lauriane L. J., Blechschmidt, Anne-Marlene, Zilker, Bianca, Richter, Andreas, Serna, Jesús A., Garcia-Nieto, David, Fernandez, Rafael P., Skov, Henrik, Dumitrascu, Adela, Simões Pereira, Patric, Abrahamsson, Katarina, Bucci, Silvia, Duetsch, Marina, Stohl, Andreas, Beck, Ivo, Laurila, Tiia, Blomquist, Byron, Howard, Dean, Archer, Stephen D., Bariteau, Ludovic, Helmig, Detlev, Hueber, Jacques, Jacobi, Hans-Werner, Posman, Kevin, Dada, Lubna, Daellenbach, Kaspar R., and Saiz-Lopez, Alfonso

Published
2022
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3. The annual cycle and sources of relevant aerosol precursor vapors in the central Arctic.

Author

Boyer, Matthew, Aliaga, Diego, Quéléver, Lauriane L. J., Bucci, Silvia, Angot, Hélène, Dada, Lubna, Heutte, Benjamin, Beck, Lisa, Duetsch, Marina, Stohl, Andreas, Beck, Ivo, Laurila, Tiia, Sarnela, Nina, Thakur, Roseline C., Miljevic, Branka, Kulmala, Markku, Petäjä, Tuukka, Sipilä, Mikko, Schmale, Julia, and Jokinen, Tuija

Subjects
VAPORS, AEROSOLS, ARCTIC climate, SEA ice, SPRING
Abstract

In this study, we present and analyze the first continuous timeseries of relevant aerosol precursor vapors from the central Arctic during the Multidisciplinary drifting Observatory for the Study of Arctic Climate (MOSAiC) expedition. These precursor vapors include sulfuric acid (SA), methanesulfonic acid (MSA), and iodic acid (IA). We use FLEXPART simulations, inverse modeling, sulfur dioxide (SO2) mixing ratios, and chlorophyll-a (chl-a) observations to interpret the 20 seasonal variability of the vapor concentrations and identify dominant sources. Our results show that both natural and anthropogenic sources are relevant for the concentrations of SA in the Arctic, but anthropogenic sources associated with Arctic haze are the most prevalent. MSA concentrations are an order of magnitude higher during polar day than during polar night due to seasonal changes in biological activity. Peak MSA concentrations were observed in May, which corresponds with the timing of the annual peak in chl-a concentrations north of 75° N. IA concentrations exhibit two distinct peaks during 25 the year: a dominant peak in spring and a secondary peak in autumn, suggesting that seasonal IA concentrations depend on both solar radiation and sea ice conditions. In general, the seasonal cycles of SA, MSA, and IA in the central Arctic Ocean are related to sea ice conditions, and we expect that changes in the Arctic environment will affect the concentrations of these vapors in the future. The magnitude of these changes and the subsequent influence on aerosol processes remains uncertain, highlighting the need for continued observations of these precursor vapors in the Arctic. [ABSTRACT FROM AUTHOR]

Published
2024
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4. Substantial contribution of iodine to Arctic ozone destruction

Author

European Commission, Consejo Superior de Investigaciones Científicas (España), Academy of Finland, Ministry of Earth Sciences (India), Swiss National Science Foundation, Swiss Polar Institute, National Science Foundation (US), Ferring Pharmaceuticals, German Research Foundation, Mahajan, Anoop S. [0000-0002-2909-5432], Li, Qinyi [0000-0002-5146-5831], Cuevas, Carlos A. [0000-0002-9251-5460], Schmale, Julia [0000-0002-1048-7962], Angot, Hélène [0000-0003-4673-8249], Richter, Andreas [0000-0003-3339-212X], Fernandez, Rafael P. [0000-0002-4114-5500], Skov, Henrik [0000-0003-1167-8696], Bucci, Silvia [0000-0002-6251-9444], Duetsch, Marina [0000-0002-1128-4198], Stohl, Andreas [0000-0002-2524-5755], Archer, Stephen D. [0000-0001-6054-2424], Dada, Lubna [0000-0003-1105-9043], Daellenbach, Kaspar R. [0000-0003-1246-6396], Saiz-Lopez, A. [0000-0002-0060-1581], Benavent, Nuria, Mahajan, Anoop S., Li, Qinyi, Cuevas, Carlos A., Schmale, Julia, Angot, Hélène, Jokinen, Tuija, Quéléver, Lauriane L.J., Blechschmidt, Anne Marlene, Zilker, Bianca, Richter, Andreas, Serna, Jesús A., García-Nieto, D., Fernández, Rafael P., Skov, Henrik, Dumitrascu, Adela, Simões Pereira, Patric, Abrahamsson, Katarina, Bucci, Silvia, Duetsch, Marina, Stohl, Andreas, Beck, Ivo, Laurila, Tiia, Blomquist, Byron, Howard, Dean, Archer, Stephen D., Bariteau, Ludovic, Helmig, Detlev, Hueber, Jacques, Jacobi, Hans Werner, Posman, Kevin, Dada, Lubna, Daellenbach, Kaspar R., Saiz-Lopez, A., European Commission, Consejo Superior de Investigaciones Científicas (España), Academy of Finland, Ministry of Earth Sciences (India), Swiss National Science Foundation, Swiss Polar Institute, National Science Foundation (US), Ferring Pharmaceuticals, German Research Foundation, Mahajan, Anoop S. [0000-0002-2909-5432], Li, Qinyi [0000-0002-5146-5831], Cuevas, Carlos A. [0000-0002-9251-5460], Schmale, Julia [0000-0002-1048-7962], Angot, Hélène [0000-0003-4673-8249], Richter, Andreas [0000-0003-3339-212X], Fernandez, Rafael P. [0000-0002-4114-5500], Skov, Henrik [0000-0003-1167-8696], Bucci, Silvia [0000-0002-6251-9444], Duetsch, Marina [0000-0002-1128-4198], Stohl, Andreas [0000-0002-2524-5755], Archer, Stephen D. [0000-0001-6054-2424], Dada, Lubna [0000-0003-1105-9043], Daellenbach, Kaspar R. [0000-0003-1246-6396], Saiz-Lopez, A. [0000-0002-0060-1581], Benavent, Nuria, Mahajan, Anoop S., Li, Qinyi, Cuevas, Carlos A., Schmale, Julia, Angot, Hélène, Jokinen, Tuija, Quéléver, Lauriane L.J., Blechschmidt, Anne Marlene, Zilker, Bianca, Richter, Andreas, Serna, Jesús A., García-Nieto, D., Fernández, Rafael P., Skov, Henrik, Dumitrascu, Adela, Simões Pereira, Patric, Abrahamsson, Katarina, Bucci, Silvia, Duetsch, Marina, Stohl, Andreas, Beck, Ivo, Laurila, Tiia, Blomquist, Byron, Howard, Dean, Archer, Stephen D., Bariteau, Ludovic, Helmig, Detlev, Hueber, Jacques, Jacobi, Hans Werner, Posman, Kevin, Dada, Lubna, Daellenbach, Kaspar R., and Saiz-Lopez, A.

Abstract

Unlike bromine, the effect of iodine chemistry on the Arctic surface ozone budget is poorly constrained. We present ship-based measurements of halogen oxides in the high Arctic boundary layer from the sunlit period of March to October 2020 and show that iodine enhances springtime tropospheric ozone depletion. We find that chemical reactions between iodine and ozone are the second highest contributor to ozone loss over the study period, after ozone photolysis-initiated loss and ahead of bromine.

Published
2022

5. A full year of aerosol size distribution data from the central Arctic under an extreme positive Arctic Oscillation : insights from the Multidisciplinarydrifting Observatory for the Study of Arctic Climate (MOSAiC) expedition

Author

Boyer, Matthew, Aliaga, Diego, Pernov, Jakob Boyd, Angot, Hélène, Quéléver, Lauriane L. J., Dada, Lubna, Heutte, Benjamin, Dall'Osto, Manuel, Beddows, David C. S., Brasseur, Zoé, Beck, Ivo, Bucci, Silvia, Duetsch, Marina, Stohl, Andreas, Laurila, Tiia, Asmi, Eija, Massling, Andreas, Thomas, Daniel Charles, Klenø Nøjgaard, Jakob, Chan, Tak, Sharma, Sangeeta, Tunved, Peter, Krejci, Radovan, Hansson, Hans-Christen, Bianchi, Federico, Lehtipalo, Katrianne, Wiedensohler, Alfred, Weinhold, Kay, Kulmala, Markku, Petäjä, Tuukka, Sipilä, Mikko, Schmale, Julia, Jokinen, Tuija, Boyer, Matthew, Aliaga, Diego, Pernov, Jakob Boyd, Angot, Hélène, Quéléver, Lauriane L. J., Dada, Lubna, Heutte, Benjamin, Dall'Osto, Manuel, Beddows, David C. S., Brasseur, Zoé, Beck, Ivo, Bucci, Silvia, Duetsch, Marina, Stohl, Andreas, Laurila, Tiia, Asmi, Eija, Massling, Andreas, Thomas, Daniel Charles, Klenø Nøjgaard, Jakob, Chan, Tak, Sharma, Sangeeta, Tunved, Peter, Krejci, Radovan, Hansson, Hans-Christen, Bianchi, Federico, Lehtipalo, Katrianne, Wiedensohler, Alfred, Weinhold, Kay, Kulmala, Markku, Petäjä, Tuukka, Sipilä, Mikko, Schmale, Julia, and Jokinen, Tuija

Abstract

The Arctic environment is rapidly changing due to accelerated warming in the region. The warming trend is driving a decline in sea ice extent, which thereby enhances feedback loops in the surface energy budget in the Arctic. Arctic aerosols play an important role in the radiative balance and hence the climate response in the region, yet direct observations of aerosols over the Arctic Ocean are limited. In this study, we investigate the annual cycle in the aerosol particle number size distribution (PNSD), particle number concentration (PNC), and black carbon (BC) mass concentration in the central Arctic during the Multidisciplinary drifting Observatory for the Study of Arctic Climate (MOSAiC) expedition. This is the first continuous, year-long data set of aerosol PNSD ever collected over the sea ice in the central Arctic Ocean. We use a k-means cluster analysis, FLEXPART simulations, and inverse modeling to evaluate seasonal patterns and the influence of different source regions on the Arctic aerosol population. Furthermore, we compare the aerosol observations to land-based sites across the Arctic, using both long-term measurements and observations during the year of the MOSAiC expedition (2019–2020), to investigate interannual variability and to give context to the aerosol characteristics from within the central Arctic. Our analysis identifies that, overall, the central Arctic exhibits typical seasonal patterns of aerosols, including anthropogenic influence from Arctic haze in winter and secondary aerosol processes in summer. The seasonal pattern corresponds to the global radiation, surface air temperature, and timing of sea ice melting/freezing, which drive changes in transport patterns and secondary aerosol processes. In winter, the Norilsk region in Russia/Siberia was the dominant source of Arctic haze signals in the PNSD and BC observations, which contributed to higher accumulation-mode PNC and BC mass concentrations in the central Arctic than at land-based obse

Published
2023
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6. Isotopic measurements in water vapor, precipitation, and seawater during EUREC(4)A

Author

Bailey, Adriana, Aemisegger, Franziska, Villiger, Leonie, Los, Sebastian A., Reverdin, Gilles, Melendez, Estefania Quinones, Acquistapace, Claudia, Baranowski, Dariusz B., Bock, Tobias, Bony, Sandrine, Bordsdorff, Tobias, Coffman, Derek, De Szoeke, Simon P., Diekmann, Christopher J., Duetsch, Marina, Ertl, Benjamin, Galewsky, Joseph, Henze, Dean, Makuch, Przemyslaw, Noone, David, Quinn, Patricia K., Roesch, Michael, Schneider, Andreas, Schneider, Matthias, Speich, Sabrina, Stevens, Bjorn, Thompson, Elizabeth J., Bailey, Adriana, Aemisegger, Franziska, Villiger, Leonie, Los, Sebastian A., Reverdin, Gilles, Melendez, Estefania Quinones, Acquistapace, Claudia, Baranowski, Dariusz B., Bock, Tobias, Bony, Sandrine, Bordsdorff, Tobias, Coffman, Derek, De Szoeke, Simon P., Diekmann, Christopher J., Duetsch, Marina, Ertl, Benjamin, Galewsky, Joseph, Henze, Dean, Makuch, Przemyslaw, Noone, David, Quinn, Patricia K., Roesch, Michael, Schneider, Andreas, Schneider, Matthias, Speich, Sabrina, Stevens, Bjorn, and Thompson, Elizabeth J.

Abstract

In early 2020, an international team set out to investigate trade-wind cumulus clouds and their coupling to the large-scale circulation through the field campaign EUREC(4)A: ElUcidating the RolE of Clouds-Circulation Coupling in ClimAte. Focused on the western tropical Atlantic near Barbados, EUREC(4)A deployed a number of innovative observational strategies, including a large network of water isotopic measurements collectively known as EUREC(4)A-iso, to study the tropical shallow convective environment. The goal of the isotopic measurements was to elucidate processes that regulate the hydroclimate state - for example, by identifying moisture sources, quantifying mixing between atmospheric layers, characterizing the microphysics that influence the formation and persistence of clouds and precipitation, and providing an extra constraint in the evaluation of numerical simulations. During the field experiment, researchers deployed seven water vapor isotopic analyzers on two aircraft, on three ships, and at the Barbados Cloud Observatory (BCO). Precipitation was collected for isotopic analysis at the BCO and from aboard four ships. In addition, three ships collected seawater for isotopic analysis. All told, the in situ data span the period 5 January-22 February 2020 and cover the approximate area 6 to 16 degrees N and 50 to 60 degrees W, with water vapor isotope ratios measured from a few meters above sea level to the mid-free troposphere and seawater samples spanning the ocean surface to several kilometers depth.This paper describes the full EUREC(4)A isotopic in situ data collection - providing extensive information about sampling strategies and data uncertainties - and also guides readers to complementary remotely sensed water vapor isotope ratios. All field data have been made publicly available even if they are affected by known biases, as is the case for high-altitude aircraft measurements, one of the two BCO ground-based water vapor time series, and select rain an

Published
2023
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7. A full year of aerosol size distribution data from the central Arctic under an extreme positive Arctic Oscillation: insights from the Multidisciplinary drifting Observatory for the Study of Arctic Climate (MOSAiC) expedition

Author

European Commission, Academy of Finland, Department of Energy (US), Swiss Polar Institute, Agencia Estatal de Investigación (España), Boyer, Matthew, Aliaga, Diego, Pernov, Jakob Boyd, Angot, Hélène, Quéléver, Lauriane L.J., Dada, Lubna, Heutte, Benjamin, Dall'Osto, Manuel, Beddows, David C. S., Brasseur, Zoé, Beck, Ivo, Bucci, Silvia, Duetsch, Marina, Stohl, Andreas, Laurila, Tiia, Asmi, Eija, Massling, Andreas, Thomas, Daniel Charles, Nøjgaard, Jacob Klenø, Chan, Tak, Sharma, Sangeeta, Tunved, Peter, Krejci, Radovan, Hansson, Hans-Christien, Bianchi, Federico, Lehtipalo, Katrianne, Wiedensohler, Alfred, Weinhold, Kay, Kulmala, Markku, Petäjä, Tuukka, Sipilä, Mikko, Schmale, Julia, Jokinen, Tuija, European Commission, Academy of Finland, Department of Energy (US), Swiss Polar Institute, Agencia Estatal de Investigación (España), Boyer, Matthew, Aliaga, Diego, Pernov, Jakob Boyd, Angot, Hélène, Quéléver, Lauriane L.J., Dada, Lubna, Heutte, Benjamin, Dall'Osto, Manuel, Beddows, David C. S., Brasseur, Zoé, Beck, Ivo, Bucci, Silvia, Duetsch, Marina, Stohl, Andreas, Laurila, Tiia, Asmi, Eija, Massling, Andreas, Thomas, Daniel Charles, Nøjgaard, Jacob Klenø, Chan, Tak, Sharma, Sangeeta, Tunved, Peter, Krejci, Radovan, Hansson, Hans-Christien, Bianchi, Federico, Lehtipalo, Katrianne, Wiedensohler, Alfred, Weinhold, Kay, Kulmala, Markku, Petäjä, Tuukka, Sipilä, Mikko, Schmale, Julia, and Jokinen, Tuija

Abstract

The Arctic environment is rapidly changing due to accelerated warming in the region. The warming trend is driving a decline in sea ice extent, which thereby enhances feedback loops in the surface energy budget in the Arctic. Arctic aerosols play an important role in the radiative balance and hence the climate response in the region, yet direct observations of aerosols over the Arctic Ocean are limited. In this study, we investigate the annual cycle in the aerosol particle number size distribution (PNSD), particle number concentration (PNC), and black carbon (BC) mass concentration in the central Arctic during the Multidisciplinary drifting Observatory for the Study of Arctic Climate (MOSAiC) expedition. This is the first continuous, year-long data set of aerosol PNSD ever collected over the sea ice in the central Arctic Ocean. We use a k-means cluster analysis, FLEXPART simulations, and inverse modeling to evaluate seasonal patterns and the influence of different source regions on the Arctic aerosol population. Furthermore, we compare the aerosol observations to land-based sites across the Arctic, using both long-term measurements and observations during the year of the MOSAiC expedition (2019–2020), to investigate interannual variability and to give context to the aerosol characteristics from within the central Arctic. Our analysis identifies that, overall, the central Arctic exhibits typical seasonal patterns of aerosols, including anthropogenic influence from Arctic haze in winter and secondary aerosol processes in summer. The seasonal pattern corresponds to the global radiation, surface air temperature, and timing of sea ice melting/freezing, which drive changes in transport patterns and secondary aerosol processes. In winter, the Norilsk region in Russia/Siberia was the dominant source of Arctic haze signals in the PNSD and BC observations, which contributed to higher accumulation-mode PNC and BC mass concentrations in the central Arctic than at land-based obse

Published
2023

9. A full year of aerosol size distribution data from the central Arctic under an extreme positive Arctic Oscillation: insights from the Multidisciplinary drifting Observatory for the Study of Arctic Climate (MOSAiC) expedition

Author

Boyer, Matthew, primary, Aliaga, Diego, additional, Pernov, Jakob Boyd, additional, Angot, Hélène, additional, Quéléver, Lauriane L. J., additional, Dada, Lubna, additional, Heutte, Benjamin, additional, Dall'Osto, Manuel, additional, Beddows, David C. S., additional, Brasseur, Zoé, additional, Beck, Ivo, additional, Bucci, Silvia, additional, Duetsch, Marina, additional, Stohl, Andreas, additional, Laurila, Tiia, additional, Asmi, Eija, additional, Massling, Andreas, additional, Thomas, Daniel Charles, additional, Nøjgaard, Jakob Klenø, additional, Chan, Tak, additional, Sharma, Sangeeta, additional, Tunved, Peter, additional, Krejci, Radovan, additional, Hansson, Hans Christen, additional, Bianchi, Federico, additional, Lehtipalo, Katrianne, additional, Wiedensohler, Alfred, additional, Weinhold, Kay, additional, Kulmala, Markku, additional, Petäjä, Tuukka, additional, Sipilä, Mikko, additional, Schmale, Julia, additional, and Jokinen, Tuija, additional

Published
2023
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10. Substantial contribution of iodine to Arctic ozone destruction. Nature Geoscience, https://doi.org/10.1038/s41561-022-01018-w

Author

Benavent, Nuria, Mahajan, Anoop S., Li, Qinyi, Cuevas, Carlos A., Schmale, Julia, Angot, Hélène, Jokinen, Tuija, Quéléver, Lauriane L. J., Blechschmidt, Anne-Marlene, Zilker, Bianca, Richter , Andreas, Serna, Jesús A., Garcia-Nieto, David, Fernandez, Rafael P., Skov, Henrik, Dumitrascu, Adela, Pereir, Patric Simões, Abrahamsson, Katarina, Bucci , Silvia, Duetsch, Marina, Stohl, Andreas, Beck, Ivo, Laurila, Tiia, Blomquist, Byron, Howard, Dean, Archer, Stephen D., Bariteau, Ludovic, Helmig, Detlev, Hueber, Jacques, Jacobi, Hans-Werner, Posman, Kevin, Dada, Lubna, Daellenbach, Kaspar R., and Saiz-Lopez, Alfonso

Abstract

Cuevas, C.A. Schmale, J. Angot, H. Jokinen, T. Quéléver, L.L.J Blechschmidt, A.-M. Zilker, B. Richter, A. Serna, J.A. Garcia-Nieto, D. Fernandez, R.P. Skov, H. Dumitrascu, A. Pereira, P.S. Abrahamsson, K. Bucci, S. Dütsch, M. Stohl, A. Beck, I. Laurila, T. Blomquist, B. Howard, D. Archer, S Bariteau, L. Helmig, D. Hueber, J. Jacobi, H.-W. Posman, K. Dada, L. Daellenbach, K.R and Saiz-Lopez, A. (2022)

Published
2022

11. Supplementary material to "A full year of aerosol size distribution data from the central Arctic under an extreme positive Arctic Oscillation: Insights from the MOSAiC expedition"

Author

Boyer, Matthew, primary, Aliaga, Diego, additional, Pernov, Jakob Boyd, additional, Angot, Hélène, additional, Quéléver, Lauriane L. J., additional, Dada, Lubna, additional, Heutte, Benjamin, additional, Dall’Osto, Manuel, additional, Beddows, David C. S., additional, Brasseur, Zoé, additional, Beck, Ivo, additional, Bucci, Silvia, additional, Duetsch, Marina, additional, Stohl, Andreas, additional, Laurila, Tiia, additional, Asmi, Eija, additional, Massling, Andreas, additional, Thomas, Daniel Charles, additional, Nøjgaard, Jakob Klenø, additional, Chan, Tak, additional, Sharma, Sangeeta, additional, Tunved, Peter, additional, Krejci, Radovan, additional, Hansson, Hans Christen, additional, Kulmala, Markku, additional, Petäjä, Tuukka, additional, Sipilä, Mikko, additional, Schmale, Julia, additional, and Jokinen, Tuija, additional

Published
2022
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12. A full year of aerosol size distribution data from the central Arctic under an extreme positive Arctic Oscillation: Insights from the MOSAiC expedition

Author

Boyer, Matthew, primary, Aliaga, Diego, additional, Pernov, Jakob Boyd, additional, Angot, Hélène, additional, Quéléver, Lauriane L. J., additional, Dada, Lubna, additional, Heutte, Benjamin, additional, Dall’Osto, Manuel, additional, Beddows, David C. S., additional, Brasseur, Zoé, additional, Beck, Ivo, additional, Bucci, Silvia, additional, Duetsch, Marina, additional, Stohl, Andreas, additional, Laurila, Tiia, additional, Asmi, Eija, additional, Massling, Andreas, additional, Thomas, Daniel Charles, additional, Nøjgaard, Jakob Klenø, additional, Chan, Tak, additional, Sharma, Sangeeta, additional, Tunved, Peter, additional, Krejci, Radovan, additional, Hansson, Hans Christen, additional, Kulmala, Markku, additional, Petäjä, Tuukka, additional, Sipilä, Mikko, additional, Schmale, Julia, additional, and Jokinen, Tuija, additional

Published
2022
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13. Overview of the MOSAiC expedition-Atmosphere INTRODUCTION

Author

Shupe, Matthew D., Rex, Markus, Blomquist, Byron, Persson, P. Ola G., Schmale, Julia, Uttal, Taneil, Althausen, Dietrich, Angot, Helene, Archer, Stephen, Bariteau, Ludovic, Beck, Ivo, Bilberry, John, Bucci, Silvia, Buck, Clifton, Boyer, Matt, Brasseur, Zoe, Brooks, Ian M., Calmer, Radiance, Cassano, John, Castro, Vagner, Chu, David, Costa, David, Cox, Christopher J., Creamean, Jessie, Crewell, Susanne, Dahlke, Sandro, Damm, Ellen, de Boer, Gijs, Deckelmann, Holger, Dethloff, Klaus, Duetsch, Marina, Ebell, Kerstin, Ehrlich, Andre, Ellis, Jody, Engelmann, Ronny, Fong, Allison A., Frey, Markus M., Gallagher, Michael R., Ganzeveld, Laurens, Gradinger, Rolf, Graeser, Juergen, Greenamyer, Vernon, Griesche, Hannes, Griffiths, Steele, Hamilton, Jonathan, Heinemann, Guenther, Helmig, Detlev, Herber, Andreas, Heuze, Celine, Hofer, Julian, Houchens, Todd, Howard, Dean, Inoue, Jun, Jacobi, Hans-Werner, Jaiser, Ralf, Jokinen, Tuija, Jourdan, Olivier, Jozef, Gina, King, Wessley, Kirchgaessner, Amelie, Klingebiel, Marcus, Krassovski, Misha, Krumpen, Thomas, Lampert, Astrid, Landing, William, Laurila, Tiia, Lawrence, Dale, Lonardi, Michael, Loose, Brice, Luepkes, Christof, Maahn, Maximilian, Macke, Andreas, Maslowski, Wieslaw, Marsay, Christopher, Maturilli, Marion, Mech, Mario, Morris, Sara, Moser, Manuel, Nicolaus, Marcel, Ortega, Paul, Osborn, Jackson, Paetzold, Falk, Perovich, Donald K., Petaja, Tuukka, Pilz, Christian, Pirazzini, Roberta, Posman, Kevin, Powers, Heath, Pratt, Kerri A., Preusser, Andreas, Quelever, Lauriane, Radenz, Martin, Rabe, Benjamin, Rinke, Annette, Sachs, Torsten, Schulz, Alexander, Siebert, Holger, Silva, Tercio, Solomon, Amy, Sommerfeld, Anja, Spreen, Gunnar, Stephens, Mark, Stohl, Andreas, Svensson, Gunilla, Uin, Janek, Viegas, Juarez, Voigt, Christiane, von der Gathen, Peter, Wehner, Birgit, Welker, Jeffrey M., Wendisch, Manfred, Werner, Martin, Xie, ZhouQing, Yue, Fange, Shupe, Matthew D., Rex, Markus, Blomquist, Byron, Persson, P. Ola G., Schmale, Julia, Uttal, Taneil, Althausen, Dietrich, Angot, Helene, Archer, Stephen, Bariteau, Ludovic, Beck, Ivo, Bilberry, John, Bucci, Silvia, Buck, Clifton, Boyer, Matt, Brasseur, Zoe, Brooks, Ian M., Calmer, Radiance, Cassano, John, Castro, Vagner, Chu, David, Costa, David, Cox, Christopher J., Creamean, Jessie, Crewell, Susanne, Dahlke, Sandro, Damm, Ellen, de Boer, Gijs, Deckelmann, Holger, Dethloff, Klaus, Duetsch, Marina, Ebell, Kerstin, Ehrlich, Andre, Ellis, Jody, Engelmann, Ronny, Fong, Allison A., Frey, Markus M., Gallagher, Michael R., Ganzeveld, Laurens, Gradinger, Rolf, Graeser, Juergen, Greenamyer, Vernon, Griesche, Hannes, Griffiths, Steele, Hamilton, Jonathan, Heinemann, Guenther, Helmig, Detlev, Herber, Andreas, Heuze, Celine, Hofer, Julian, Houchens, Todd, Howard, Dean, Inoue, Jun, Jacobi, Hans-Werner, Jaiser, Ralf, Jokinen, Tuija, Jourdan, Olivier, Jozef, Gina, King, Wessley, Kirchgaessner, Amelie, Klingebiel, Marcus, Krassovski, Misha, Krumpen, Thomas, Lampert, Astrid, Landing, William, Laurila, Tiia, Lawrence, Dale, Lonardi, Michael, Loose, Brice, Luepkes, Christof, Maahn, Maximilian, Macke, Andreas, Maslowski, Wieslaw, Marsay, Christopher, Maturilli, Marion, Mech, Mario, Morris, Sara, Moser, Manuel, Nicolaus, Marcel, Ortega, Paul, Osborn, Jackson, Paetzold, Falk, Perovich, Donald K., Petaja, Tuukka, Pilz, Christian, Pirazzini, Roberta, Posman, Kevin, Powers, Heath, Pratt, Kerri A., Preusser, Andreas, Quelever, Lauriane, Radenz, Martin, Rabe, Benjamin, Rinke, Annette, Sachs, Torsten, Schulz, Alexander, Siebert, Holger, Silva, Tercio, Solomon, Amy, Sommerfeld, Anja, Spreen, Gunnar, Stephens, Mark, Stohl, Andreas, Svensson, Gunilla, Uin, Janek, Viegas, Juarez, Voigt, Christiane, von der Gathen, Peter, Wehner, Birgit, Welker, Jeffrey M., Wendisch, Manfred, Werner, Martin, Xie, ZhouQing, and Yue, Fange

Abstract

With the Arctic rapidly changing, the needs to observe, understand, and model the changes are essential. To support these needs, an annual cycle of observations of atmospheric properties, processes, and interactions were made while drifting with the sea ice across the central Arctic during the Multidisciplinary drifting Observatory for the Study of Arctic Climate (MOSAiC) expedition from October 2019 to September 2020. An international team designed and implemented the comprehensive program to document and characterize all aspects of the Arctic atmospheric system in unprecedented detail, using a variety of approaches, and across multiple scales. These measurements were coordinated with other observational teams to explore crosscutting and coupled interactions with the Arctic Ocean, sea ice, and ecosystem through a variety of physical and biogeochemical processes. This overview outlines the breadth and complexity of the atmospheric research program, which was organized into 4 subgroups: atmospheric state, clouds and precipitation, gases and aerosols, and energy budgets. Atmospheric variability over the annual cycle revealed important influences from a persistent large-scale winter circulation pattern, leading to some storms with pressure and winds that were outside the interquartile range of past conditions suggested by long-term reanalysis. Similarly, the MOSAiC location was warmer and wetter in summer than the reanalysis climatology, in part due to its close proximity to the sea ice edge. The comprehensiveness of the observational program for characterizing and analyzing atmospheric phenomena is demonstrated via a winter case study examining air mass transitions and a summer case study examining vertical atmospheric evolution. Overall, the MOSAiC atmospheric program successfully met its objectives and was the most comprehensive atmospheric measurement program to date conducted over the Arctic sea ice. The obtained data will support a broad range of coupled-system s

Published
2022

17. A full year of aerosol size distribution data from the central Arctic under an extreme positive Arctic Oscillation: Insights from the MOSAiC expedition.

Author

Boyer, Matthew, Aliaga, Diego, Pernov, Jakob Boyd, Angot, Hélène, Quéléver, Lauriane L. J., Dada, Lubna, Heutte, Benjamin, Dall'Osto, Manuel, Beddows, David C. S., Brasseur, Zoé, Beck, Ivo, Bucci, Silvia, Duetsch, Marina, Stohl, Andreas, Laurila, Tiia, Asmi, Eija, Massling, Andreas, Thomas, Daniel Charles, Nøjgaard, Jakob Klenø, and Tak Chan

Abstract

The Arctic environment is rapidly changing due to accelerated warming in the region. The warming trend is driving a decline in sea ice extent, which thereby enhances feedback loops in the surface energy budget in the Arctic. Arctic aerosols play an important role in the radiative balance, and hence the climate response, in the region; yet direct observations of aerosols over the Arctic Ocean are limited. In this study, we investigate the annual cycle in the aerosol particle number size distribution (PNSD), particle number concentration (PNC), and black carbon (BC) mass concentration in the central Arctic during the Multidisciplinary drifting Observatory for the Study of Arctic Climate (MOSAiC) expedition. This is the first continuous, year-long dataset of aerosol PNSD ever collected over the sea ice in the central Arctic Ocean. We use a k-means cluster analysis, FLEXPART simulations, and inverse modeling to evaluate seasonal patterns and the influence of different source regions on the Arctic aerosol population. Furthermore, we compare the aerosol observations to land-based sites across the Arctic, using both long-term measurements and observations during the year of the MOSAiC expedition (2019 - 2020), to investigate interannual variability and to give context to the aerosol characteristics from within the central Arctic. Our analysis identifies that, overall, the central Arctic exhibits typical seasonal patterns of aerosols, including anthropogenic influence from Arctic Haze in winter and secondary aerosol processes in summer. The seasonal pattern corresponds with the global radiation, surface air temperature, and the timing of sea ice melting/freezing, which drives changes in transport patterns and secondary aerosol processes. In winter, the Norilsk region in Russia/Siberia was the dominant source of Arctic Haze signal in the PNSD and BC observations, which contributed to higher accumulation mode PNC and BC mass concentration in the central Arctic than at land-based observatories. We also show that the wintertime Arctic Oscillation (AO) phenomenon, which was reported to achieve a record-breaking positive phase during January - March 2020, explains the unusual timing and magnitude of Arctic Haze across the Arctic region compared to longer-term observations. In summer, the PNC of nucleation and Aitken mode aerosol is enhanced, but concentrations were notably lower in the central Arctic over the ice pack than at land-based sites further south. The analysis presented herein provides a current snapshot of Arctic aerosol processes in an environment that is characterized by rapid changes, which will be crucial for improving climate model predictions, understanding linkages between different environmental processes, and investigating the impacts of climate change in future Arctic aerosol studies. [ABSTRACT FROM AUTHOR]

Published
2022
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21. Substantial contribution of iodine to Arctic ozone destruction

Author

Nuria Benavent, Anoop S. Mahajan, Qinyi Li, Carlos A. Cuevas, Julia Schmale, Hélène Angot, Tuija Jokinen, Lauriane L. J. Quéléver, Anne-Marlene Blechschmidt, Bianca Zilker, Andreas Richter, Jesús A. Serna, David Garcia-Nieto, Rafael P. Fernandez, Henrik Skov, Adela Dumitrascu, Patric Simões Pereira, Katarina Abrahamsson, Silvia Bucci, Marina Duetsch, Andreas Stohl, Ivo Beck, Tiia Laurila, Byron Blomquist, Dean Howard, Stephen D. Archer, Ludovic Bariteau, Detlev Helmig, Jacques Hueber, Hans-Werner Jacobi, Kevin Posman, Lubna Dada, Kaspar R. Daellenbach, Alfonso Saiz-Lopez, European Commission, Consejo Superior de Investigaciones Científicas (España), Academy of Finland, Ministry of Earth Sciences (India), Swiss National Science Foundation, Swiss Polar Institute, National Science Foundation (US), Ferring Pharmaceuticals, German Research Foundation, Mahajan, Anoop S., Li, Qinyi, Cuevas, Carlos A., Schmale, Julia, Angot, Hélène, Richter, Andreas, Fernandez, Rafael P., Skov, Henrik, Bucci, Silvia, Duetsch, Marina, Stohl, Andreas, Archer, Stephen D., Dada, Lubna, Daellenbach, Kaspar R., Saiz-Lopez, A., Institute for Atmospheric and Earth System Research (INAR), Polar and arctic atmospheric research (PANDA), and Air quality research group

Subjects
General Earth and Planetary Sciences, 114 Physical sciences
Abstract

6 pags., 2 figs., Unlike bromine, the effect of iodine chemistry on the Arctic surface ozone budget is poorly constrained. We present ship-based measurements of halogen oxides in the high Arctic boundary layer from the sunlit period of March to October 2020 and show that iodine enhances springtime tropospheric ozone depletion. We find that chemical reactions between iodine and ozone are the second highest contributor to ozone loss over the study period, after ozone photolysis-initiated loss and ahead of bromine., This study received funding from the European Research Council Executive Agency under the European Union’s Horizon 2020 Research and Innovation Program (project ERC‐2016‐COG 726349 CLIMAHAL and ERC-2016-STG 714621 GASPARCON) and the European Commission via the EMME-CARE project and was supported by the Consejo Superior de Investigaciones Científicas of Spain. This work was supported by the European Union’s Horizon 2020 Research and Innovation Programme under grant agreement no. 856612 and the Academy of Finland (project no. 334514). The Indian Institute of Tropical Meteorology is funded by the Ministry of Earth Sciences, Government of India. Ozone, CO, CH4 and AMS measurements were funded by the Swiss National Science Foundation (grant 200021_188478), the Swiss Polar Institute and U.S. National Science Foundation grants 1914781 and 1807163. J.S. holds the Ingvar Kamprad chair for extreme environments research, sponsored by Ferring Pharmaceuticals. Data reported in this manuscript were produced as part of the international MOSAiC expedition with tag MOSAiC20192020, with activities supported by Polarstern expedition AWI-PS122_00. H.S. was funded by the European ERA-PLANET projects iGOSP and iCUPE (consortium agreement no. 689443 for both projects). We thank FORMAS and the Swedish Polar Research Secretariat for support. We gratefully acknowledge funding by the Deutsche Forschungsgemeinschaft (project no. 268020496 – TRR 172) within the Transregional Collaborative Research Center ‘ArctiC Amplification: Climate Relevant Atmospheric and SurfaCe Processes, and Feedback Mechanisms (AC)3’ in subproject C03. We thank I. Bourgeois (NOAA/CIRES) for providing the ATom NOx data.

Published
2022

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