Articles | Volume 24, issue 15
https://doi.org/10.5194/acp-24-8865-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Special issue:
https://doi.org/10.5194/acp-24-8865-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Overview: quasi-Lagrangian observations of Arctic air mass transformations – introduction and initial results of the HALO–(𝒜 𝒞)3 aircraft campaign
Manfred Wendisch
CORRESPONDING AUTHOR
Leipziger Institut für Meteorologie (LIM), Universität Leipzig, Leipzig, Germany
Susanne Crewell
Institut für Geophysik und Meteorologie (IGM), Universität zu Köln, Cologne, Germany
André Ehrlich
Leipziger Institut für Meteorologie (LIM), Universität Leipzig, Leipzig, Germany
Andreas Herber
Physik der Atmosphäre Bremerhaven, Alfred–Wegener–Institut, Helmholtz–Zentrum für Polar– und Meeresforschung (AWI), Bremerhaven, Germany
Benjamin Kirbus
Leipziger Institut für Meteorologie (LIM), Universität Leipzig, Leipzig, Germany
Christof Lüpkes
Physik der Atmosphäre Bremerhaven, Alfred–Wegener–Institut, Helmholtz–Zentrum für Polar– und Meeresforschung (AWI), Bremerhaven, Germany
Mario Mech
Institut für Geophysik und Meteorologie (IGM), Universität zu Köln, Cologne, Germany
Steven J. Abel
Met Office, Exeter, United Kingdom
Elisa F. Akansu
Atmosphärische Mikrophysik, Leibniz–Institut für Troposphärenforschung (TROPOS), Leipzig, Germany
Felix Ament
Meteorologisches Institut, Universität Hamburg, Hamburg, Germany
Clémantyne Aubry
Institut für Physik der Atmosphäre, Deutsches Zentrum für Luft- und Raumfahrt (DLR), Oberpfaffenhofen, Germany
Laboratoire Atmosphères, Milieux et Observations Spatiales (LATMOS), Centre National de la Recherche Scientifique (CNRS), Guyancourt, France
Sebastian Becker
Leipziger Institut für Meteorologie (LIM), Universität Leipzig, Leipzig, Germany
Stephan Borrmann
Abteilung für Partikelchemie, Max-Planck-Institut für Chemie (MPIC), Mainz, Germany
Institut für Physik der Atmosphäre (IPA), Johannes Gutenberg-Universität, Mainz, Germany
Heiko Bozem
Institut für Physik der Atmosphäre (IPA), Johannes Gutenberg-Universität, Mainz, Germany
Marlen Brückner
Leipziger Institut für Meteorologie (LIM), Universität Leipzig, Leipzig, Germany
Hans-Christian Clemen
Abteilung für Partikelchemie, Max-Planck-Institut für Chemie (MPIC), Mainz, Germany
Sandro Dahlke
Physik der Atmosphäre, Alfred–Wegener–Institut, Helmholtz–Zentrum für Polar– und Meeresforschung (AWI), Potsdam, Germany
Georgios Dekoutsidis
Institut für Physik der Atmosphäre, Deutsches Zentrum für Luft- und Raumfahrt (DLR), Oberpfaffenhofen, Germany
Julien Delanoë
Laboratoire Atmosphères, Milieux et Observations Spatiales (LATMOS), Centre National de la Recherche Scientifique (CNRS), Guyancourt, France
Elena De La Torre Castro
Institut für Physik der Atmosphäre, Deutsches Zentrum für Luft- und Raumfahrt (DLR), Oberpfaffenhofen, Germany
Institut für Physik der Atmosphäre (IPA), Johannes Gutenberg-Universität, Mainz, Germany
Faculteit Luchtvaart- en Ruimtevaarttechniek, Technische Universiteit Delft, Delft, the Netherlands
Henning Dorff
Meteorologisches Institut, Universität Hamburg, Hamburg, Germany
Regis Dupuy
Laboratoire de Météorologie Physique (LaMP), Université Clermont Auvergne, Centre National de la Recherche Scientifique (CNRS), Clermont-Ferrand, France
Oliver Eppers
Abteilung für Partikelchemie, Max-Planck-Institut für Chemie (MPIC), Mainz, Germany
Florian Ewald
Institut für Physik der Atmosphäre, Deutsches Zentrum für Luft- und Raumfahrt (DLR), Oberpfaffenhofen, Germany
Geet George
Klimaphysik, Max-Planck-Institut für Meteorologie (MPI-M), Hamburg, Germany
now at: Faculty of Civil Engineering and Geosciences, Delft University of Technology (TU Delft), Delft, the Netherlands
Irina V. Gorodetskaya
Centro de Estudos do Ambiente e do Mar (CESAM), Universidade de Aveiro, Aveiro, Portugal
Sarah Grawe
Atmosphärische Mikrophysik, Leibniz–Institut für Troposphärenforschung (TROPOS), Leipzig, Germany
Silke Groß
Institut für Physik der Atmosphäre, Deutsches Zentrum für Luft- und Raumfahrt (DLR), Oberpfaffenhofen, Germany
Jörg Hartmann
Physik der Atmosphäre Bremerhaven, Alfred–Wegener–Institut, Helmholtz–Zentrum für Polar– und Meeresforschung (AWI), Bremerhaven, Germany
Silvia Henning
Atmosphärische Mikrophysik, Leibniz–Institut für Troposphärenforschung (TROPOS), Leipzig, Germany
Lutz Hirsch
Klimaphysik, Max-Planck-Institut für Meteorologie (MPI-M), Hamburg, Germany
Evelyn Jäkel
Leipziger Institut für Meteorologie (LIM), Universität Leipzig, Leipzig, Germany
Philipp Joppe
Abteilung für Partikelchemie, Max-Planck-Institut für Chemie (MPIC), Mainz, Germany
Institut für Physik der Atmosphäre (IPA), Johannes Gutenberg-Universität, Mainz, Germany
Olivier Jourdan
Laboratoire de Météorologie Physique (LaMP), Université Clermont Auvergne, Centre National de la Recherche Scientifique (CNRS), Clermont-Ferrand, France
Zsofia Jurányi
Physik der Atmosphäre Bremerhaven, Alfred–Wegener–Institut, Helmholtz–Zentrum für Polar– und Meeresforschung (AWI), Bremerhaven, Germany
Michail Karalis
Department of Meteorology and Bolin Centre for Climate research, Stockholm University, Stockholm, Sweden
Mona Kellermann
Atmosphärische Mikrophysik, Leibniz–Institut für Troposphärenforschung (TROPOS), Leipzig, Germany
Marcus Klingebiel
Leipziger Institut für Meteorologie (LIM), Universität Leipzig, Leipzig, Germany
Michael Lonardi
Leipziger Institut für Meteorologie (LIM), Universität Leipzig, Leipzig, Germany
now at: Extreme Environments Research Laboratory (EERL), Ecole Polytechnique Fédérale de Lausanne (EPFL), Sion, Switzerland
Johannes Lucke
Institut für Physik der Atmosphäre, Deutsches Zentrum für Luft- und Raumfahrt (DLR), Oberpfaffenhofen, Germany
Faculteit Luchtvaart- en Ruimtevaarttechniek, Technische Universiteit Delft, Delft, the Netherlands
Anna E. Luebke
Leipziger Institut für Meteorologie (LIM), Universität Leipzig, Leipzig, Germany
Maximilian Maahn
Leipziger Institut für Meteorologie (LIM), Universität Leipzig, Leipzig, Germany
Nina Maherndl
Leipziger Institut für Meteorologie (LIM), Universität Leipzig, Leipzig, Germany
Marion Maturilli
Physik der Atmosphäre, Alfred–Wegener–Institut, Helmholtz–Zentrum für Polar– und Meeresforschung (AWI), Potsdam, Germany
Bernhard Mayer
Meteorologisches Institut, Ludwig-Maximilians-Universität München, Munich, Germany
Johanna Mayer
Institut für Physik der Atmosphäre, Deutsches Zentrum für Luft- und Raumfahrt (DLR), Oberpfaffenhofen, Germany
Stephan Mertes
Atmosphärische Mikrophysik, Leibniz–Institut für Troposphärenforschung (TROPOS), Leipzig, Germany
Janosch Michaelis
Physik der Atmosphäre Bremerhaven, Alfred–Wegener–Institut, Helmholtz–Zentrum für Polar– und Meeresforschung (AWI), Bremerhaven, Germany
now at: Maritime Klimatologie, Maritim-klimatologische Analysen und Produkte, Deutscher Wetterdienst (DWD), Hamburg, Germany
Michel Michalkov
Atmosphärische Mikrophysik, Leibniz–Institut für Troposphärenforschung (TROPOS), Leipzig, Germany
Guillaume Mioche
Laboratoire de Météorologie Physique (LaMP), Université Clermont Auvergne, Centre National de la Recherche Scientifique (CNRS), Clermont-Ferrand, France
Manuel Moser
Institut für Physik der Atmosphäre, Deutsches Zentrum für Luft- und Raumfahrt (DLR), Oberpfaffenhofen, Germany
Institut für Physik der Atmosphäre (IPA), Johannes Gutenberg-Universität, Mainz, Germany
Hanno Müller
Leipziger Institut für Meteorologie (LIM), Universität Leipzig, Leipzig, Germany
Roel Neggers
Institut für Geophysik und Meteorologie (IGM), Universität zu Köln, Cologne, Germany
Davide Ori
Institut für Geophysik und Meteorologie (IGM), Universität zu Köln, Cologne, Germany
Daria Paul
Institut für Geophysik und Meteorologie (IGM), Universität zu Köln, Cologne, Germany
Fiona M. Paulus
Institut für Geophysik und Meteorologie (IGM), Universität zu Köln, Cologne, Germany
Christian Pilz
Atmosphärische Mikrophysik, Leibniz–Institut für Troposphärenforschung (TROPOS), Leipzig, Germany
Felix Pithan
Physik der Atmosphäre Bremerhaven, Alfred–Wegener–Institut, Helmholtz–Zentrum für Polar– und Meeresforschung (AWI), Bremerhaven, Germany
Mira Pöhlker
Atmosphärische Mikrophysik, Leibniz–Institut für Troposphärenforschung (TROPOS), Leipzig, Germany
Leipziger Institut für Meteorologie (LIM), Universität Leipzig, Leipzig, Germany
Veronika Pörtge
Meteorologisches Institut, Ludwig-Maximilians-Universität München, Munich, Germany
Maximilian Ringel
Meteorologisches Institut, Universität Hamburg, Hamburg, Germany
Nils Risse
Institut für Geophysik und Meteorologie (IGM), Universität zu Köln, Cologne, Germany
Gregory C. Roberts
Scripps Institution of Oceanography, University of California San Diego, La Jolla, USA
Sophie Rosenburg
Leipziger Institut für Meteorologie (LIM), Universität Leipzig, Leipzig, Germany
Johannes Röttenbacher
Leipziger Institut für Meteorologie (LIM), Universität Leipzig, Leipzig, Germany
Janna Rückert
Institut für Umweltphysik (IUP), Universität Bremen, Bremen, Germany
Michael Schäfer
Leipziger Institut für Meteorologie (LIM), Universität Leipzig, Leipzig, Germany
Jonas Schaefer
Atmosphärische Mikrophysik, Leibniz–Institut für Troposphärenforschung (TROPOS), Leipzig, Germany
Vera Schemann
Institut für Geophysik und Meteorologie (IGM), Universität zu Köln, Cologne, Germany
Imke Schirmacher
Institut für Geophysik und Meteorologie (IGM), Universität zu Köln, Cologne, Germany
Jörg Schmidt
Leipziger Institut für Meteorologie (LIM), Universität Leipzig, Leipzig, Germany
Sebastian Schmidt
Department of Atmospheric and Oceanic Sciences, Laboratory for Atmospheric and Space Physics (LASP), University of Colorado Boulder, Boulder, CO, USA
Johannes Schneider
Abteilung für Partikelchemie, Max-Planck-Institut für Chemie (MPIC), Mainz, Germany
Sabrina Schnitt
Institut für Geophysik und Meteorologie (IGM), Universität zu Köln, Cologne, Germany
Anja Schwarz
Leipziger Institut für Meteorologie (LIM), Universität Leipzig, Leipzig, Germany
Holger Siebert
Atmosphärische Mikrophysik, Leibniz–Institut für Troposphärenforschung (TROPOS), Leipzig, Germany
Harald Sodemann
Geophysical Institute, University of Bergen, Bergen, Norway
Bjerknes Centre for Climate Research, Bergen, Norway
Tim Sperzel
Leipziger Institut für Meteorologie (LIM), Universität Leipzig, Leipzig, Germany
now at: Abteilung Klima und Umwelt, Deutscher Wetterdienst, Offenbach am Main, Germany
Gunnar Spreen
Institut für Umweltphysik (IUP), Universität Bremen, Bremen, Germany
Bjorn Stevens
Klimaphysik, Max-Planck-Institut für Meteorologie (MPI-M), Hamburg, Germany
Frank Stratmann
Atmosphärische Mikrophysik, Leibniz–Institut für Troposphärenforschung (TROPOS), Leipzig, Germany
Gunilla Svensson
Department of Meteorology and Bolin Centre for Climate research, Stockholm University, Stockholm, Sweden
Christian Tatzelt
Atmosphärische Mikrophysik, Leibniz–Institut für Troposphärenforschung (TROPOS), Leipzig, Germany
Thomas Tuch
Atmosphärische Mikrophysik, Leibniz–Institut für Troposphärenforschung (TROPOS), Leipzig, Germany
Timo Vihma
Finnish Meteorological Institute (FMI), Helsinki, Finland
Christiane Voigt
Institut für Physik der Atmosphäre, Deutsches Zentrum für Luft- und Raumfahrt (DLR), Oberpfaffenhofen, Germany
Institut für Physik der Atmosphäre (IPA), Johannes Gutenberg-Universität, Mainz, Germany
Lea Volkmer
Meteorologisches Institut, Ludwig-Maximilians-Universität München, Munich, Germany
Andreas Walbröl
Institut für Geophysik und Meteorologie (IGM), Universität zu Köln, Cologne, Germany
Anna Weber
Meteorologisches Institut, Ludwig-Maximilians-Universität München, Munich, Germany
Birgit Wehner
Atmosphärische Mikrophysik, Leibniz–Institut für Troposphärenforschung (TROPOS), Leipzig, Germany
Bruno Wetzel
Atmosphärische Mikrophysik, Leibniz–Institut für Troposphärenforschung (TROPOS), Leipzig, Germany
Martin Wirth
Institut für Physik der Atmosphäre, Deutsches Zentrum für Luft- und Raumfahrt (DLR), Oberpfaffenhofen, Germany
Tobias Zinner
Meteorologisches Institut, Ludwig-Maximilians-Universität München, Munich, Germany
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- Final revised paper (published on 13 Aug 2024)
- Preprint (discussion started on 26 Mar 2024)
Interactive discussion
Status: closed
Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor
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RC1: 'Comment on egusphere-2024-783', Anonymous Referee #1, 30 Apr 2024
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AC1: 'Reply on RC1', Manfred Wendisch, 12 Jun 2024
The comment was uploaded in the form of a supplement: https://egusphere.copernicus.org/preprints/2024/egusphere-2024-783/egusphere-2024-783-AC1-supplement.pdf
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AC1: 'Reply on RC1', Manfred Wendisch, 12 Jun 2024
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RC2: 'Comment on egusphere-2024-783', Anonymous Referee #2, 23 May 2024
The comment was uploaded in the form of a supplement: https://egusphere.copernicus.org/preprints/2024/egusphere-2024-783/egusphere-2024-783-RC2-supplement.pdf
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AC2: 'Reply on RC2', Manfred Wendisch, 12 Jun 2024
The comment was uploaded in the form of a supplement: https://egusphere.copernicus.org/preprints/2024/egusphere-2024-783/egusphere-2024-783-AC2-supplement.pdf
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AC2: 'Reply on RC2', Manfred Wendisch, 12 Jun 2024
Peer review completion
AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
AR by Manfred Wendisch on behalf of the Authors (12 Jun 2024)
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ED: Publish subject to technical corrections (19 Jun 2024) by Farahnaz Khosrawi
AR by Manfred Wendisch on behalf of the Authors (24 Jun 2024)
Manuscript
Short summary
The Arctic is warming faster than the rest of the globe. Warm-air intrusions (WAIs) into the Arctic may play an important role in explaining this phenomenon. Cold-air outbreaks (CAOs) out of the Arctic may link the Arctic climate changes to mid-latitude weather. In our article, we describe how to observe air mass transformations during CAOs and WAIs using three research aircraft instrumented with state-of-the-art remote-sensing and in situ measurement devices.
The Arctic is warming faster than the rest of the globe. Warm-air intrusions (WAIs) into the...
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Review of “Overview: Quasi-Lagrangian observations of Arctic air mass transformations – Introduction and initial results of the HALO–(AC)3 aircraft campaign” by Wendisch et al., for publication in Atmospheric Chemistry and Physics
Summary
This paper provides an overview of the recent HALO-(AC)3 aircraft campaign highlighting the flight plans/strategy, measurements, and various measurement/sampling techniques of Arctic air masses. Some of the novelties of this study include quasi-Lagrangian measurements from eight warm-air intrusion (WAI) and twelve cold-air outbreak (CAO) cases, derived surface heating/cooling and moistening/drying estimates, comprehensive aerosol/CCN data, and estimates of mesoscale divergence using dropsondes released during circular flight patterns. The abstract is very well written, concise, and clearly conveys the novelties and (initial) results of the AC3 campaign. The quasi-lagrangian sampling strategy is very clearly defined, thought out, and easy to follow in the text/results. The section on Arctic clouds nicely highlights cloud phase as a function of the underlying surface (open water versus sea ice) as well as a simultaneous retrieval of effective radius for both ice crystals and liquid drops. These results, in my view, appropriately highlight and contextualize the various datasets as well as set the table for a number of planned (and likely interdisciplinary) analyses across a wide array of Arctic climate science sub-disciplines. Aside from a couple of very minor comments (indicated in the Specific Comments) and with a few of the figures being quite “busy” with lines and markers, every figure – in my view – is justified in its content with each figure adding very clear and rich context to the paper. Another strength of this manuscript is that, given volume of data and analysis in this manuscript, all sources of uncertainty (e.g., LWP and snowfall) are well characterized and quantified.
This is a commendable effort by all authors and contributors. For a very lengthy manuscript with 17 figures and 3 appendices, this was a very fun read with a lot of concise, “to-the-point” information that many sub-disciplines within the Arctic science community will be eager to read. I liken this manuscript to a fine 7-course dinner: it may take a while before you’re finished, but every course delivers masterfully crafted dishes by world-class chefs with each dish delivering a palette of flavors certain to whet every appetite in the Arctic climate community. The manuscript in its present form is perfect in the sense that it captures just the right amount of detail (in my view) for an overview paper. While I have a number of very specific comments that would improve clarity in a few spots, they are extremely minor and can be addressed quickly without the need for a second review. I have no general concerns/comments for this manuscript, and overall, I believe this manuscript is publishable in its present form to Atmospheric Chemistry and Physics.
I look forward to many more in-depth studies following and building upon the excellent work presented in this manuscript.
Specific Comments
L23-24: “... was more than 1.5 K warmer than during pre-industrial times” though it’s stated “Data published by the Copernicus Climate Change Service show...”, this statement needs a citable reference.
L24: “numerous feedback mechanisms in the Earth’s climate system” it would be good to list 2-3 or so of these feedback mechanisms here.
L44: A reference or two here would be good.
L105: This is a very lengthy introduction, but a necessary one as each paragraph here has a clear focus and motivation for the AC3 campaign.
L124: Add latitude/longitude coordinates for Kiruna and Longyearbyen here.
L134: Add latitude/longitude coordinates for Ny-Ålesund.
Section 2, like the introduction, is very well structured and written.
L171: Casual readers may not fully understand what a “Lagrangian” frame of reference is and how it ties into the sampling strategy described in this paragraph. A sentence to open up this paragraph describing what “Lagrangian” is, in my view, would lead the rest of this paragraph better and make the sampling strategy clearer to the reader in its objective.
L174: “Because of their...” I would lead this sentence with “For example, ...” as this would more clearly lead the reader into a discussion of balloon-related drawbacks described in the previous sentence.
Figure 2 Caption: Recommend changing “enables to observe the changes” to “enables observational changes”
L248: I am slightly confused by the writing here – what do you mean by a “quality of possibilities”? I think “provides unprecedented quantity of possibilities” would work here.
Figure 5: This is a very well-constructed figure that clearly contrasts CAOs with WAIs.
L305: How exactly is the “ice growth process” inferred or done using measurements here?
L306: Can you point to or reference where “we also detect stronger riming”?
Figure 6: Very picky comment here... “weak” should be capitalized in the Figure Title.
L317-319: Very interesting result!
Figure 7: I love the setup of this figure – it is definitely one of the most informative figures I’ve ever seen relating ice index and distance from the ice edge to actual cloud morphology. I hope to see versions of this figure in your future papers.
Figure 8 caption: Is it really necessary to call this a “Shapiro-Keyser cyclone” here? I think it would be better if this were referenced (including the citation) in the main text rather than the figure caption.
L374 and Figure 10 caption: One of the other prevailing cloud phase/microphysics algorithms for ground-based cloud remote sensors follows the widely-used Shupe et al. (2008, and references therein). I think it would be useful for the Arctic cloud/climate community to comment on how your algorithm compares with the Shupe et al. algorithm (and perhaps discuss how a comparison of these algorithms might be done in a future AC3-related study which would also be very interesting!).
Shupe, M. D., and Coauthors, 2008: A Focus On Mixed-Phase Clouds. Bull. Amer. Meteor. Soc., 89, 1549–1562, https://doi.org/10.1175/2008BAMS2378.1.
L382: Just say “Future studies” rather than “near future studies”.
L390: Following my previous comment for L374, this might be a good spot to discuss potential differences in these algorithms.
L430: How typical are RHi values of 140%? Might be good to add a reference or two here for comparison sake.
L455-456: I’d merge these two sentences.
L512-513: I agree with this conclusion.
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