the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Atmospheric composition in the European Arctic and 30 years of the Zeppelin Observatory, Ny-Ålesund
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
Kjetil Tørseth
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- Final revised paper (published on 14 Mar 2022)
- Preprint (discussion started on 18 Jun 2021)
Interactive discussion
Status: closed
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RC1: 'Comment on acp-2021-505', Anonymous Referee #1, 23 Jul 2021
This is a comprehensive overview on measurements conducted in the Zeppelin observatory during the past 30 years. The text is longish, which is understandable and acceptable for this kind of a paper. While the manuscript can be considered well-structured in general, its technical quality is somewhat mixed. The paper has a well-written introduction (section 1), an interesting historical overview (section 2), and proper descriptions of both observatory and related measurements (sections 3 and 4). Overview of the obtained results (section 5) has several scientific problems, as outlined below in more detail, and these problems need to be fixed before the paper can be accepted for publication. Concerning section 6, I am not fully in favor of putting strategic/political (section 6.1) and scientific (sections 6.2 and 6.3) aims side by side, but it is up to the editor to decide whether this requires some restructuring of the text.
Scientific issues related to sections 5 and 6
Section 5.1.
I do not understand the first statement of section 5.1 (lines 652-653). Based on figure 6, it is impossible to see whether OC and EC resemble each other at any time (their concentrations levels certainly do not, and resemblance of concentrations ratios is also questionable). Overall, I do not see how Figure 6 could tell anything about the similarities in OC and EC source regions.
The statement on lines 575-677 is unclear. I suppose that the authors mean that the CF conversion factor typical for aged aerosols should be applicable for Zeppelin because of its remote location from main sources. The wording (complies well with) gives an impression that this thing has somehow confirmed for Zeppelin.
Russian is a very large territory. Do the authors have more detailed information on the main source areas for high sulfur episodes, e.g. the Kola Peninsula area discussed a lot in previous literature?
When discussing about past trends of inorganic ion concentrations in atmospheric aerosols (lines 686-696), I wonder why the authors refer to targeted emission reductions during 1990-2010, not the real emission reduction that took place. Data on actual emission reductions during that period is certainly available.
Section 5.2.
This section is about aerosol physical and optical properties (the word optical could be included into the title), so why do the author start the section by mentioning CCN and cloud properties which are not discussed at all in this section?
lines 702-704: The authors assume implicitly here that the particle size is some sort of proxy for its ageing. This is probably true but should be explained for readers not familiar with combined effects of aerosol sources and aerosol dynamics taking place during atmospheric transportation.
Please explain in more detail what is meant by “light period” and “summer” (lines 710 and 711), and whether “sunlit period” (line 724) means something else.
The discussion about aerosol optical properties is vague (lines 732-745). The authors try to relate changes in optical properties to those in particle concentrations (number or mass, not explained?), but the relevance or purpose of this exercise has not been explained. I do not understand what the authors mean be stating the particle concentrations increase through the year (line 740). This whole paragraph needs to be re-written.
The discussion on lines 755-764 is rather general and appears to be loosely connected with other contents of section 5.2.
Section 5.3
What is the point of bringing up CO2 concentration in 2019 and its increase from the previous year? The CO2 increase is a well-known fact, while its annual increase rate varies from year to year. Data from one single year provide little insight on this matter (lines 766-768).
What is the basis for stating that the CO2 concentration increase rata is exponential? (line 769)
line 793: any explanation for the stated pause of CH4 mixing ratio?
There is repetition of text between the lines 838-844 and lines 858-869. Also figure 12 appears twice in the paper.
Section 5.6: Based on measurements of just one site in Arctic and one site outside Arctic, it is impossible to make any general statement about differences between Article areas and those outside Arctic (lines 992-994).
Section 6.2: There is much new scientific work and findings on arctic amplification and related issues that seem to be missing in the introductory part of this section (lines 1204-1212).
Section 6.3, lines 1325-1326: I do not think statements like this should be included when discussing future aspects of research.
Technical and minor scientific issues
line 227: something is missing from here (e.g. … during 1971 to 1980)
line 435: INP should be in parenthesis
line 440 (and later line 765): The term “climate gases” is not commonly in use. Please consider modifying the titles.
line 711: Figure 8 does not tell anything about nucleation and particle growth, so it should not be referred to here but later in the text.
line 795: is it possible to measure the CH4 concentration with a 5-digit accuracy?
line 801: an increase from 28 to 32 is not consistent with 25% increase.
lines 811 and 815: suggest à suggested
line 1008: MC or MCM?
lines 1013-1014: it is enough to explain GEM one time.
line 1037: … Asia, including China, contribute…
line 1092 vs. line 1143: please use only a single term for LOE (episodes of very low ozone vs. low ozone episodes).
lines 1119-1121: Unclear sentence, please modify.
lines 1166-1168: the first sentence of section 6 is unclear. Please re-write.
line 1184: please correct the grammar (that need study)
line 1125: a paper in preparation is not a proper reference.
line 1316: please correct the grammar (will need study)
lines 1332 and 1334: CEAC or CEC?
lines 1363-1364: unclear sentence, please modify
Some of the figures (figs. 13, 14 and 20) are of poor technical quality.
Figures 12 and 18 appear twice in the text.
Citation: https://doi.org/10.5194/acp-2021-505-RC1 - AC1: 'Reply on RC1', Stephen Platt, 04 Oct 2021
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RC2: 'Comment on acp-2021-505', Anonymous Referee #2, 12 Aug 2021
REFEREE COMMENTS
General comments
The paper provides an overview on The Zeppelin Observatory, a history of the station, measurements and trends and a review of the current state of the European Arctic atmosphere. The paper is well structured and written. However, it is quite long and the authors could consider shorten the text and add some summarizing figures or statistics. The abstract could include short statement on the most scientific significant result(s). For demonstrating the scientific impact of the observatory there could be also some statistics of the published papers, number international projects over the years when / where Zeppelin dataset has been used.
Specific / minor comments
- line 53: how the decision of the Swedish parliament accepted for a Swedish monitoring program in connected to the Norwegian approach. Please clarify.
- line 842: History; you could add the time line figure demonstrating the different atmospheric composition measurements at different locations. This would also provide a general overview on the development and availability of long term measurements and address the role of Zeppelin measurements.
- line 113: add “full stop” after parenthesis.
- lines 195-199: please add references for the location climate / vegetation classification.
- line 224: please add a reference if possible.
- line 255: you could use “/sios-svalbard.org/”
- line 285: open the acronym FLEXPART particle dispersion model:>>> “FLEXible PARTicle dispersion model”. Please re-check all the acronyms in the text and open the acronym when mentioned for the first time
- Fig 3: improve quality (resolution) of the figure
- line 316: Aitken mode particles, please add size
- Fig 4 please improve quality (resolution) of the figure
- line 340: you could add a short overall (meta) description / table of all measurements which would better describe the overall measurement capacity of the station. And give some general statistics of the measurements.
- line 350-365: (4.1) this is very detailed description of the samplings and filters, you could consider a schematic figure of the process or an annex.
- line 366: add the reference for Mann-Kendall Test/Sen’s slope.
- Fig 6., 7., 8. technical quality of the fig should be improved
- line 439: “With this set-up the Zeppelin Observatory is now one of the first global aerosol observatories with semi-continuous in-situ cloud sampling”. What are the other stations ?
- line 839, 865: some error with the reference (Error! Not a valid bookmark self-reference)
- line(s) 925 & 962 please check, add the reference Petäjä et al.2020 Overview: Integrative and Comprehensive Understanding on Polar Environments (iCUPE) – concept and initial results, Atmos. Chem. Phys., 20, 8551–8592, https://doi.org/10.5194/acp-20-8551-2020, 2020.
- line 1074: please add some specification for the acronyms “POLARCAT” “TOPSE”
- line 1172: “strengthen the position of the Zeppelin Observatory as a leading global measurement platform, perhaps” one of the ? / Arctic ?
- line 1200: Refer to “open access”, how is the data access to Zeppelin measurements currently organized ?
- line 1227: “Changes in the Arctic aerosol burden will in turn influence climate via direct and indirect aerosol effects, i.e. via increased absorption and scattering, and changes in CCN and ice nucleating particles (INP), respectively. “ - add reference
- line 1228: “Another important non-CO2greenhouse gas is N2O, with a global warming potential 265–298 times that of CO2.” - add reference
- AC2: 'Reply on RC2', Stephen Platt, 06 Oct 2021