Overview: quasi-Lagrangian observations of Arctic air mass transformations – introduction and initial results of the HALO–(???? ????)3 aircraft campaign
Global warming is amplified in the Arctic. However, numerical models struggle to represent key processes that determine Arctic weather and climate. To collect data that help to constrain the models, the HALO–( ???????? ) 3 aircraft campaign was conducted over the Norwegian and Greenland seas, the Fr...
Published in: | Atmospheric Chemistry and Physics |
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Language: | English |
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2024
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Online Access: | https://doi.org/10.5194/acp-24-8865-2024 https://acp.copernicus.org/articles/24/8865/2024/ |
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Copernicus Publications: E-Journals |
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English |
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Global warming is amplified in the Arctic. However, numerical models struggle to represent key processes that determine Arctic weather and climate. To collect data that help to constrain the models, the HALO–( ???????? ) 3 aircraft campaign was conducted over the Norwegian and Greenland seas, the Fram Strait, and the central Arctic Ocean in March and April 2022. The campaign focused on one specific challenge posed by the models, namely the reasonable representation of transformations of air masses during their meridional transport into and out of the Arctic via northward moist- and warm-air intrusions (WAIs) and southward marine cold-air outbreaks (CAOs). Observations were made over areas of open ocean, the marginal sea ice zone, and the central Arctic sea ice. Two low-flying and one long-range, high-altitude research aircraft were flown in colocated formation whenever possible. To follow the air mass transformations, a quasi-Lagrangian flight strategy using trajectory calculations was realized, enabling us to sample the same moving-air parcels twice along their trajectories. Seven distinct WAI and 12 CAO cases were probed. From the quasi-Lagrangian measurements, we have quantified the diabatic heating/cooling and moistening/drying of the transported air masses. During CAOs, maximum values of 3 K h −1 warming and 0.3 g kg −1 h −1 moistening were obtained below 1 km altitude. From the observations of WAIs, diabatic cooling rates of up to 0.4 K h −1 and a moisture loss of up to 0.1 g kg −1 h −1 from the ground to about 5.5 km altitude were derived. Furthermore, the development of cloud macrophysical (cloud-top height and horizontal cloud cover) and microphysical (liquid water path, precipitation, and ice index) properties along the southward pathways of the air masses were documented during CAOs, and the moisture budget during a specific WAI event was estimated. In addition, we discuss the statistical frequency of occurrence of the different thermodynamic phases of Arctic low-level clouds, the interaction of Arctic ... |
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Wendisch, Manfred Crewell, Susanne Ehrlich, André Herber, Andreas Kirbus, Benjamin Lüpkes, Christof Mech, Mario Abel, Steven J. Akansu, Elisa F. Ament, Felix Aubry, Clémantyne Becker, Sebastian Borrmann, Stephan Bozem, Heiko Brückner, Marlen Clemen, Hans-Christian Dahlke, Sandro Dekoutsidis, Georgios Delanoë, Julien Torre Castro, Elena Dorff, Henning Dupuy, Regis Eppers, Oliver Ewald, Florian George, Geet Gorodetskaya, Irina V. Grawe, Sarah Groß, Silke Hartmann, Jörg Henning, Silvia Hirsch, Lutz Jäkel, Evelyn Joppe, Philipp Jourdan, Olivier Jurányi, Zsofia Karalis, Michail Kellermann, Mona Klingebiel, Marcus Lonardi, Michael Lucke, Johannes Luebke, Anna E. Maahn, Maximilian Maherndl, Nina Maturilli, Marion Mayer, Bernhard Mayer, Johanna Mertes, Stephan Michaelis, Janosch Michalkov, Michel Mioche, Guillaume Moser, Manuel Müller, Hanno Neggers, Roel Ori, Davide Paul, Daria Paulus, Fiona M. Pilz, Christian Pithan, Felix Pöhlker, Mira Pörtge, Veronika Ringel, Maximilian Risse, Nils Roberts, Gregory C. Rosenburg, Sophie Röttenbacher, Johannes Rückert, Janna Schäfer, Michael Schaefer, Jonas Schemann, Vera Schirmacher, Imke Schmidt, Jörg Schmidt, Sebastian Schneider, Johannes Schnitt, Sabrina Schwarz, Anja Siebert, Holger Sodemann, Harald Sperzel, Tim Spreen, Gunnar Stevens, Bjorn Stratmann, Frank Svensson, Gunilla Tatzelt, Christian Tuch, Thomas Vihma, Timo Voigt, Christiane Volkmer, Lea Walbröl, Andreas Weber, Anna Wehner, Birgit Wetzel, Bruno Wirth, Martin Zinner, Tobias |
spellingShingle |
Wendisch, Manfred Crewell, Susanne Ehrlich, André Herber, Andreas Kirbus, Benjamin Lüpkes, Christof Mech, Mario Abel, Steven J. Akansu, Elisa F. Ament, Felix Aubry, Clémantyne Becker, Sebastian Borrmann, Stephan Bozem, Heiko Brückner, Marlen Clemen, Hans-Christian Dahlke, Sandro Dekoutsidis, Georgios Delanoë, Julien Torre Castro, Elena Dorff, Henning Dupuy, Regis Eppers, Oliver Ewald, Florian George, Geet Gorodetskaya, Irina V. Grawe, Sarah Groß, Silke Hartmann, Jörg Henning, Silvia Hirsch, Lutz Jäkel, Evelyn Joppe, Philipp Jourdan, Olivier Jurányi, Zsofia Karalis, Michail Kellermann, Mona Klingebiel, Marcus Lonardi, Michael Lucke, Johannes Luebke, Anna E. Maahn, Maximilian Maherndl, Nina Maturilli, Marion Mayer, Bernhard Mayer, Johanna Mertes, Stephan Michaelis, Janosch Michalkov, Michel Mioche, Guillaume Moser, Manuel Müller, Hanno Neggers, Roel Ori, Davide Paul, Daria Paulus, Fiona M. Pilz, Christian Pithan, Felix Pöhlker, Mira Pörtge, Veronika Ringel, Maximilian Risse, Nils Roberts, Gregory C. Rosenburg, Sophie Röttenbacher, Johannes Rückert, Janna Schäfer, Michael Schaefer, Jonas Schemann, Vera Schirmacher, Imke Schmidt, Jörg Schmidt, Sebastian Schneider, Johannes Schnitt, Sabrina Schwarz, Anja Siebert, Holger Sodemann, Harald Sperzel, Tim Spreen, Gunnar Stevens, Bjorn Stratmann, Frank Svensson, Gunilla Tatzelt, Christian Tuch, Thomas Vihma, Timo Voigt, Christiane Volkmer, Lea Walbröl, Andreas Weber, Anna Wehner, Birgit Wetzel, Bruno Wirth, Martin Zinner, Tobias Overview: quasi-Lagrangian observations of Arctic air mass transformations – introduction and initial results of the HALO–(???? ????)3 aircraft campaign |
author_facet |
Wendisch, Manfred Crewell, Susanne Ehrlich, André Herber, Andreas Kirbus, Benjamin Lüpkes, Christof Mech, Mario Abel, Steven J. Akansu, Elisa F. Ament, Felix Aubry, Clémantyne Becker, Sebastian Borrmann, Stephan Bozem, Heiko Brückner, Marlen Clemen, Hans-Christian Dahlke, Sandro Dekoutsidis, Georgios Delanoë, Julien Torre Castro, Elena Dorff, Henning Dupuy, Regis Eppers, Oliver Ewald, Florian George, Geet Gorodetskaya, Irina V. Grawe, Sarah Groß, Silke Hartmann, Jörg Henning, Silvia Hirsch, Lutz Jäkel, Evelyn Joppe, Philipp Jourdan, Olivier Jurányi, Zsofia Karalis, Michail Kellermann, Mona Klingebiel, Marcus Lonardi, Michael Lucke, Johannes Luebke, Anna E. Maahn, Maximilian Maherndl, Nina Maturilli, Marion Mayer, Bernhard Mayer, Johanna Mertes, Stephan Michaelis, Janosch Michalkov, Michel Mioche, Guillaume Moser, Manuel Müller, Hanno Neggers, Roel Ori, Davide Paul, Daria Paulus, Fiona M. Pilz, Christian Pithan, Felix Pöhlker, Mira Pörtge, Veronika Ringel, Maximilian Risse, Nils Roberts, Gregory C. Rosenburg, Sophie Röttenbacher, Johannes Rückert, Janna Schäfer, Michael Schaefer, Jonas Schemann, Vera Schirmacher, Imke Schmidt, Jörg Schmidt, Sebastian Schneider, Johannes Schnitt, Sabrina Schwarz, Anja Siebert, Holger Sodemann, Harald Sperzel, Tim Spreen, Gunnar Stevens, Bjorn Stratmann, Frank Svensson, Gunilla Tatzelt, Christian Tuch, Thomas Vihma, Timo Voigt, Christiane Volkmer, Lea Walbröl, Andreas Weber, Anna Wehner, Birgit Wetzel, Bruno Wirth, Martin Zinner, Tobias |
author_sort |
Wendisch, Manfred |
title |
Overview: quasi-Lagrangian observations of Arctic air mass transformations – introduction and initial results of the HALO–(???? ????)3 aircraft campaign |
title_short |
Overview: quasi-Lagrangian observations of Arctic air mass transformations – introduction and initial results of the HALO–(???? ????)3 aircraft campaign |
title_full |
Overview: quasi-Lagrangian observations of Arctic air mass transformations – introduction and initial results of the HALO–(???? ????)3 aircraft campaign |
title_fullStr |
Overview: quasi-Lagrangian observations of Arctic air mass transformations – introduction and initial results of the HALO–(???? ????)3 aircraft campaign |
title_full_unstemmed |
Overview: quasi-Lagrangian observations of Arctic air mass transformations – introduction and initial results of the HALO–(???? ????)3 aircraft campaign |
title_sort |
overview: quasi-lagrangian observations of arctic air mass transformations – introduction and initial results of the halo–(???? ????)3 aircraft campaign |
publishDate |
2024 |
url |
https://doi.org/10.5194/acp-24-8865-2024 https://acp.copernicus.org/articles/24/8865/2024/ |
geographic |
Arctic Arctic Ocean Greenland |
geographic_facet |
Arctic Arctic Ocean Greenland |
genre |
Arctic Arctic Ocean Fram Strait Global warming Greenland Sea ice |
genre_facet |
Arctic Arctic Ocean Fram Strait Global warming Greenland Sea ice |
op_source |
eISSN: 1680-7324 |
op_relation |
doi:10.5194/acp-24-8865-2024 https://acp.copernicus.org/articles/24/8865/2024/ |
op_doi |
https://doi.org/10.5194/acp-24-8865-2024 |
container_title |
Atmospheric Chemistry and Physics |
container_volume |
24 |
container_issue |
15 |
container_start_page |
8865 |
op_container_end_page |
8892 |
_version_ |
1809759162323697664 |
spelling |
ftcopernicus:oai:publications.copernicus.org:acp118835 2024-09-09T19:19:02+00:00 Overview: quasi-Lagrangian observations of Arctic air mass transformations – introduction and initial results of the HALO–(???? ????)3 aircraft campaign Wendisch, Manfred Crewell, Susanne Ehrlich, André Herber, Andreas Kirbus, Benjamin Lüpkes, Christof Mech, Mario Abel, Steven J. Akansu, Elisa F. Ament, Felix Aubry, Clémantyne Becker, Sebastian Borrmann, Stephan Bozem, Heiko Brückner, Marlen Clemen, Hans-Christian Dahlke, Sandro Dekoutsidis, Georgios Delanoë, Julien Torre Castro, Elena Dorff, Henning Dupuy, Regis Eppers, Oliver Ewald, Florian George, Geet Gorodetskaya, Irina V. Grawe, Sarah Groß, Silke Hartmann, Jörg Henning, Silvia Hirsch, Lutz Jäkel, Evelyn Joppe, Philipp Jourdan, Olivier Jurányi, Zsofia Karalis, Michail Kellermann, Mona Klingebiel, Marcus Lonardi, Michael Lucke, Johannes Luebke, Anna E. Maahn, Maximilian Maherndl, Nina Maturilli, Marion Mayer, Bernhard Mayer, Johanna Mertes, Stephan Michaelis, Janosch Michalkov, Michel Mioche, Guillaume Moser, Manuel Müller, Hanno Neggers, Roel Ori, Davide Paul, Daria Paulus, Fiona M. Pilz, Christian Pithan, Felix Pöhlker, Mira Pörtge, Veronika Ringel, Maximilian Risse, Nils Roberts, Gregory C. Rosenburg, Sophie Röttenbacher, Johannes Rückert, Janna Schäfer, Michael Schaefer, Jonas Schemann, Vera Schirmacher, Imke Schmidt, Jörg Schmidt, Sebastian Schneider, Johannes Schnitt, Sabrina Schwarz, Anja Siebert, Holger Sodemann, Harald Sperzel, Tim Spreen, Gunnar Stevens, Bjorn Stratmann, Frank Svensson, Gunilla Tatzelt, Christian Tuch, Thomas Vihma, Timo Voigt, Christiane Volkmer, Lea Walbröl, Andreas Weber, Anna Wehner, Birgit Wetzel, Bruno Wirth, Martin Zinner, Tobias 2024-08-13 application/pdf https://doi.org/10.5194/acp-24-8865-2024 https://acp.copernicus.org/articles/24/8865/2024/ eng eng doi:10.5194/acp-24-8865-2024 https://acp.copernicus.org/articles/24/8865/2024/ eISSN: 1680-7324 Text 2024 ftcopernicus https://doi.org/10.5194/acp-24-8865-2024 2024-08-19T14:05:25Z Global warming is amplified in the Arctic. However, numerical models struggle to represent key processes that determine Arctic weather and climate. To collect data that help to constrain the models, the HALO–( ???????? ) 3 aircraft campaign was conducted over the Norwegian and Greenland seas, the Fram Strait, and the central Arctic Ocean in March and April 2022. The campaign focused on one specific challenge posed by the models, namely the reasonable representation of transformations of air masses during their meridional transport into and out of the Arctic via northward moist- and warm-air intrusions (WAIs) and southward marine cold-air outbreaks (CAOs). Observations were made over areas of open ocean, the marginal sea ice zone, and the central Arctic sea ice. Two low-flying and one long-range, high-altitude research aircraft were flown in colocated formation whenever possible. To follow the air mass transformations, a quasi-Lagrangian flight strategy using trajectory calculations was realized, enabling us to sample the same moving-air parcels twice along their trajectories. Seven distinct WAI and 12 CAO cases were probed. From the quasi-Lagrangian measurements, we have quantified the diabatic heating/cooling and moistening/drying of the transported air masses. During CAOs, maximum values of 3 K h −1 warming and 0.3 g kg −1 h −1 moistening were obtained below 1 km altitude. From the observations of WAIs, diabatic cooling rates of up to 0.4 K h −1 and a moisture loss of up to 0.1 g kg −1 h −1 from the ground to about 5.5 km altitude were derived. Furthermore, the development of cloud macrophysical (cloud-top height and horizontal cloud cover) and microphysical (liquid water path, precipitation, and ice index) properties along the southward pathways of the air masses were documented during CAOs, and the moisture budget during a specific WAI event was estimated. In addition, we discuss the statistical frequency of occurrence of the different thermodynamic phases of Arctic low-level clouds, the interaction of Arctic ... Text Arctic Arctic Ocean Fram Strait Global warming Greenland Sea ice Copernicus Publications: E-Journals Arctic Arctic Ocean Greenland Atmospheric Chemistry and Physics 24 15 8865 8892 |