the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
EUREC4A
Bjorn Stevens
David Farrell
Felix Ament
Alan Blyth
Christopher Fairall
Johannes Karstensen
Patricia K. Quinn
Sabrina Speich
Claudia Acquistapace
Franziska Aemisegger
Anna Lea Albright
Hugo Bellenger
Eberhard Bodenschatz
Kathy-Ann Caesar
Rebecca Chewitt-Lucas
Gijs de Boer
Julien Delanoë
Leif Denby
Florian Ewald
Benjamin Fildier
Marvin Forde
Geet George
Silke Gross
Martin Hagen
Andrea Hausold
Karen J. Heywood
Lutz Hirsch
Marek Jacob
Friedhelm Jansen
Stefan Kinne
Daniel Klocke
Tobias Kölling
Heike Konow
Marie Lothon
Wiebke Mohr
Ann Kristin Naumann
Louise Nuijens
Léa Olivier
Robert Pincus
Mira Pöhlker
Gilles Reverdin
Gregory Roberts
Sabrina Schnitt
Hauke Schulz
A. Pier Siebesma
Claudia Christine Stephan
Peter Sullivan
Ludovic Touzé-Peiffer
Jessica Vial
Raphaela Vogel
Paquita Zuidema
Nicola Alexander
Lyndon Alves
Sophian Arixi
Hamish Asmath
Gholamhossein Bagheri
Katharina Baier
Adriana Bailey
Dariusz Baranowski
Alexandre Baron
Sébastien Barrau
Paul A. Barrett
Frédéric Batier
Andreas Behrendt
Arne Bendinger
Florent Beucher
Sebastien Bigorre
Edmund Blades
Peter Blossey
Olivier Bock
Steven Böing
Pierre Bosser
Denis Bourras
Pascale Bouruet-Aubertot
Keith Bower
Pierre Branellec
Hubert Branger
Michal Brennek
Alan Brewer
Pierre-Etienne Brilouet
Björn Brügmann
Stefan A. Buehler
Elmo Burke
Ralph Burton
Radiance Calmer
Jean-Christophe Canonici
Xavier Carton
Gregory Cato Jr.
Jude Andre Charles
Patrick Chazette
Yanxu Chen
Michal T. Chilinski
Thomas Choularton
Patrick Chuang
Shamal Clarke
Céline Cornet
Pierre Coutris
Fleur Couvreux
Susanne Crewell
Timothy Cronin
Zhiqiang Cui
Yannis Cuypers
Alton Daley
Gillian M. Damerell
Thibaut Dauhut
Hartwig Deneke
Jean-Philippe Desbios
Steffen Dörner
Sebastian Donner
Vincent Douet
Kyla Drushka
Marina Dütsch
André Ehrlich
Kerry Emanuel
Alexandros Emmanouilidis
Jean-Claude Etienne
Sheryl Etienne-Leblanc
Ghislain Faure
Graham Feingold
Luca Ferrero
Andreas Fix
Cyrille Flamant
Piotr Jacek Flatau
Gregory R. Foltz
Linda Forster
Iulian Furtuna
Alan Gadian
Joseph Galewsky
Martin Gallagher
Peter Gallimore
Cassandra Gaston
Chelle Gentemann
Nicolas Geyskens
Andreas Giez
John Gollop
Isabelle Gouirand
Christophe Gourbeyre
Dörte de Graaf
Geiske E. de Groot
Robert Grosz
Johannes Güttler
Manuel Gutleben
Kashawn Hall
George Harris
Kevin C. Helfer
Dean Henze
Calvert Herbert
Bruna Holanda
Antonio Ibanez-Landeta
Janet Intrieri
Suneil Iyer
Fabrice Julien
Heike Kalesse
Jan Kazil
Alexander Kellman
Abiel T. Kidane
Ulrike Kirchner
Marcus Klingebiel
Mareike Körner
Leslie Ann Kremper
Jan Kretzschmar
Ovid Krüger
Wojciech Kumala
Armin Kurz
Pierre L'Hégaret
Matthieu Labaste
Tom Lachlan-Cope
Arlene Laing
Peter Landschützer
Theresa Lang
Diego Lange
Ingo Lange
Clément Laplace
Gauke Lavik
Rémi Laxenaire
Caroline Le Bihan
Mason Leandro
Nathalie Lefevre
Marius Lena
Donald Lenschow
Gary Lloyd
Sebastian Los
Niccolò Losi
Oscar Lovell
Christopher Luneau
Przemyslaw Makuch
Szymon Malinowski
Gaston Manta
Eleni Marinou
Nicholas Marsden
Sebastien Masson
Nicolas Maury
Bernhard Mayer
Margarette Mayers-Als
Christophe Mazel
Wayne McGeary
James C. McWilliams
Mario Mech
Melina Mehlmann
Agostino Niyonkuru Meroni
Theresa Mieslinger
Andreas Minikin
Peter Minnett
Gregor Möller
Yanmichel Morfa Avalos
Caroline Muller
Ionela Musat
Anna Napoli
Almuth Neuberger
Christophe Noisel
David Noone
Freja Nordsiek
Jakub L. Nowak
Lothar Oswald
Douglas J. Parker
Carolyn Peck
Renaud Person
Miriam Philippi
Albert Plueddemann
Christopher Pöhlker
Veronika Pörtge
Ulrich Pöschl
Lawrence Pologne
Michał Posyniak
Marc Prange
Estefanía Quiñones Meléndez
Jule Radtke
Karim Ramage
Jens Reimann
Lionel Renault
Klaus Reus
Ashford Reyes
Joachim Ribbe
Maximilian Ringel
Markus Ritschel
Cesar B. Rocha
Nicolas Rochetin
Johannes Röttenbacher
Callum Rollo
Haley Royer
Pauline Sadoulet
Leo Saffin
Sanola Sandiford
Irina Sandu
Michael Schäfer
Vera Schemann
Imke Schirmacher
Oliver Schlenczek
Jerome Schmidt
Marcel Schröder
Alfons Schwarzenboeck
Andrea Sealy
Christoph J. Senff
Ilya Serikov
Samkeyat Shohan
Elizabeth Siddle
Alexander Smirnov
Florian Späth
Branden Spooner
M. Katharina Stolla
Wojciech Szkółka
Simon P. de Szoeke
Stéphane Tarot
Eleni Tetoni
Elizabeth Thompson
Jim Thomson
Lorenzo Tomassini
Julien Totems
Alma Anna Ubele
Leonie Villiger
Jan von Arx
Thomas Wagner
Andi Walther
Ben Webber
Manfred Wendisch
Shanice Whitehall
Anton Wiltshire
Allison A. Wing
Martin Wirth
Jonathan Wiskandt
Kevin Wolf
Ludwig Worbes
Ethan Wright
Volker Wulfmeyer
Shanea Young
Chidong Zhang
Dongxiao Zhang
Florian Ziemen
Tobias Zinner
Martin Zöger
Download
- Final revised paper (published on 25 Aug 2021)
- Preprint (discussion started on 28 Jan 2021)
Interactive discussion
Status: closed
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RC1: 'Comment on essd-2021-18', Anonymous Referee #1, 02 Mar 2021
General comments
This paper is a comprehensive review of the data collected during EUREC4A, which was conducted in the Atlantic trade wind region near Barbados in January-February 2020. The goal of the EUREC4A was to observe the atmosphere and ocean on multiple time and space scales using a large array of ocean and atmosphere instrumentation in order to better constrain environmental controls on trade wind cloud fields. It is anticipated that the experiment will lead to an improved understanding of how global warming might influence such clouds and their climate impacts.
EURIC4A was a massive, complex field campaign involving many measurement systems and numerous investigators from many nations. As such, undertaking a review of the measurement systems and data collected is daunting, but the authors have successfully created a readable, interesting, and comprehensible narrative. The paper contains lucid and pertinent graphics of the data collected, showing both some preliminary results and evidence of how the measurements link together to address the common goal of the paper. It is a credit to the project lead scientists to include all participants as co-authors of the paper. This is one of the best papers on field campaign data that I have read.
Specific comments
I have only minor comments.
- What are the impacts of Barbados island on measurements taken on and near the island? Data from the lidar on the island show a prominent diurnal cycle. Can you comment on the issue of representativeness of those island observations with respect to open-ocean conditions? Also, with the 300 m+ Barbados terrain, there may be some blocking effects on the flow upstream of the barrier that would influence observations there.
- Figure 12 shows that about half the campaign had elevated background concentrations of aerosols, presumably from African dust. The rest of the period had more-typical open-ocean concentrations, which would argue that for those times EURIC4A results might be transferrable to other ocean basins. The rapid ramp-ups and ramp-downs in February suggest there may sharp horizontal gradients in aerosols over the domain. While the variability offers the opportunity to investigate aerosol impacts on warm-rain formation, it may also present analysis challenges owing to large horizontal and vertical variations in CCN concentrations.
- Figure 17 figure shows a diurnal cycle of the SST. Will the data collected in EURIC4A be sufficient for a thorough analysis of effects of the radiation diurnal cycle on the cloud fields?
- Data policy on p. 38: “To actively support the initial dispersal of data by making (even preliminary) data available to everyone as quickly as possible through the AERIS archive.” Is it possible to be more specific about timing on data release?
Technical comments
- 16: In Fig. 8, define S and “black dashed line shows.”
- 23: Explain in caption the arrow in the upper panel and the vertical gray lines in the lower panels.
- 24, line 360: “The latter is the focus of the zoom in the lower panels of Fig. 13…”
- 29, Fig. 17: Define p in the caption.
- 38, line 585: Word missing after “resultant”
Citation: https://doi.org/10.5194/essd-2021-18-RC1 -
AC1: 'Reply on RC1', Bjorn Stevens, 14 May 2021
We thank the reviewer for their encouraging comments, and suggestions for improvement. We have addressed all the rcomments as suggested. On the more substantial points:
- We have analyzed the diurnal cycle over the BCO at the surface and at 400 me and compared these to near surface measurements from the Meteor. A diurnal cycle is evident in both locations, and is similar but substantially more pronounced (1.27 K vs 0.53 K) at the BCO. This is now discussed in the manuscript.
- We analyzed the 3hr changes in Ragged Point CCN measurements. These are usually less than 10%, and 80% of the time less than 30%. Given the much larger changes over periods of day and that an analysis period roughly corresponds to the 3hr period of the ATR, Twin-Otter and HALO circling, this is encouraging for the utility of the data for exploring aerosol-cloud interactions
The other minor comments were addressed by discussing the adequacy of the measurements for measuring the diel cycle and addressing the data availability quesiton -- most data is already available. Technical comments were addressed as suggested.
Citation: https://doi.org/10.5194/essd-2021-18-AC1
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RC2: 'Comment on essd-2021-18', Anonymous Referee #2, 18 Mar 2021
General comments
The paper presents an overview of goals, design, the proceeding and first outcomes of EUREC4A project conducted in January and February 2020 in the vicinity of Barbados island on Atlantic trade winds region. Observations merged measurements conducted in the atmosphere (trade wind clouds) and in the ocean in wide span of time and space scales. The ultimate goal of the campaign was to improving our understanding of how the global warming could affect the trade wind clouds.
EUREC4A was undoubtedly the more complex and exhaustive observation campaign conducted ever. It is not common to review a paper describing such a complex experiment, probably because it is the first publication that engages with the challenge to present in a concise way such diverse measurements. Being specialist on atmospheric physics I won’t pretend that I understood all subtleties of ocean measurements. However, the paper offers a fluent narrative that allows even a non-specialist to catch the main ideas of observations performed. Still, I have few suggestions that could improve the overall understanding of the project (see below).
Specific comments:
Figures give a general overview of a kind of measurements performed during the experiment. Very often they are very complex and I think that they deserve more descriptions. I understand that those figures should give only an overview of what was observed, however a huge diversity of data make it difficult to understand for non-specialists (as atmospheric scientists versus oceanic scientists). I would appreciate if more attention is given to explain in some general yet concise manner what message could be inferred from those measurements.
Technical remarks:
p.4 Abstract, line 5; ‘or’ used twice.
p.5 l. 30: ‘to RICO’ should be probably ‘and RICO’
Figure 2, what is really shown in this figure? Is it a composition of all flights, dropsondes patterns, radiosonde soundings from the whole experiment? Colors in the figure don’t correspond exactly to the colors in the legend…. Or it is only me that cannot see correctly.
Figure 8, the scale for the isentropic lapse rate is missing, or I cannot see where it is. Or the dashed line does not represent a lapse rate?
p. 18, l. 268-269: ‘eighteen coordinated (4h flight segments)’ …. Should ‘segments’ be outside the parantheses?
Figure 11 deserves a legend more ‘compatible’ with descriptions in different parts of the figure. For instance: in the figure we see ‘CloudKite hologram’ that is described as MPCK+ in the legend.
p. 22 l 329: Prospero and Carlson, 2020, NOT ‘J M Prospero….’
p. 35 l. 535: ‘Holland’ should be ‘The Netherlands’
Citation: https://doi.org/10.5194/essd-2021-18-RC2 -
AC2: 'Comment on essd-2021-18', Bjorn Stevens, 14 May 2021
We have substantially addressed all of the comments in this reviews, as was suggested. The major change has been to revise most figures and figure captions to more consistently adhere to standards (also for names, and distinguishing between quantites such as height, altitude and depth), clarify figure elements, changing colors to make some aspects more clear, and to strengthen the description of the figure in the captions.
The one comment where there is a slight chance we misunderstood the reviewer comment, or did not address it adquately was on the laspe rate for the composite boundary layer figure, Fig 8. The dashed line is constant as the lifted parcel is unsaturated and then Θ increases after it ascends beyond the LCL. Originally we desribed the dashline as denoting the lapse rate, which is incorrect, what it describes is the potential temperature along an isentrope of near-surface air. If this was the point of confusion, it has been corrected.
Citation: https://doi.org/10.5194/essd-2021-18-AC2