the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Observational ozone data over the global oceans and polar regions: The TOAR-II Oceans data set version 2024
Abstract. Studying tropospheric ozone over the remote areas of the planet, such as the open oceans and the polar regions, is crucial to understand the role of ozone as a global climate forcer and regulator of atmospheric oxidative capacity. A focus on the pristine oceanic and polar regions complements the available land-based data sets and provides insights into key photochemical and depositional loss processes that control the concentrations, spatio-temporal variability of ozone, and the physico-chemical mechanisms driving these patterns. However, an assessment of the role of ozone over the oceanic and polar regions has been hampered by a lack of comprehensive observational data sets. Here, we present the first comprehensive collection of ozone data over the oceans and the polar regions. The overall data set consists of 77 ship cruises/buoy-based observations and 48 aircraft-based campaigns. The data set, consisting of more than 630,000 independent ozone measurement data points covering the period from 1977 to 2022 and an altitude range from the surface to 5000 m (with a focus on the lowest 2000 m), allows systematic analyses of the spatio-temporal distribution and long-term trends over the defined 11 ocean/polar regions. The data sets from ships, buoys, and aircrafts are complemented with an ozonesonde data set from 29 launch sites or field campaigns, and by 21 non-polar and 17 polar ground-based stations data sets. The data were filtered by using backward trajectories calculated with the HYSPLIT model from the individual observation points to extract essentially oceanic observations, defined as air masses that have travelled over oceans for 72 hours or more, which were further tested with the coincident Radon observations. The oceanic and polar data thus selected showed typically flat diurnal patterns at high latitudes and daytime decreases (11–16 %) at low latitudes, indicating the adequacy of the data collection and processing procedures, as well as the potential for further studies of processes with statistical robustness and coverage. The ship/buoy- and aircraft-based data sets presented here will supplement the land-based ones in the TOAR-II database to provide a fully global assessment of tropospheric ozone.
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Status: open (until 16 Apr 2025)
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RC1: 'Comment on essd-2024-566', Anonymous Referee #1, 18 Mar 2025
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General Comments
This study describes a new database of tropospheric ozone measurements over the oceans, coastal, and polar regions from buoys, ships, aircraft, ozonesondes, and surface sites. The creation of this database is important since measurements of tropospheric ozone are lacking over these sink regions, and this study is an important component of TOAR-II. The authors present a comprehensive description of data sources, flagging methods, and backward trajectory methods. They provide a preliminary assessment of the data statistics and diurnal patterns, in preparation for the TOAR-II assessment report on this topic. I recommend that this paper be accepted after minor revisions.
Specific Comments
- In the first paragraph of the Introduction, the authors state that “The overall budget of tropospheric ozone is dominated by the photochemical production and loss terms” and then important loss terms over the ocean and in remote regions are discussed, but none of the production terms are discussed. To better tie in this sentence and fully explain how global ozone is controlled, it could be helpful to add a sentence somewhere in this paragraph about the photochemical production of ozone and whether it’s location dependent.
- Lines 149-151 state that no data are assigned to the Mediterranean Sea and Black Sea region because of the predominant continental influences. Was there data available over those bodies of water? If data was available but then excluded because the air masses would’ve had a too-high influence from the land, this should be stated.
- In the paragraph beginning on line 203, the authors should consider adding a statement describing why Radon is used as a tracer for land influence.
- Why is IAGOS data not included in the aircraft data set?
- When selecting a sonde data point every 200 m (line 240), did you ensure that the data point had high quality? For example, some sonde profiles are noisy, so you may select a data point that is erroneously low or high. This issue may be resolved by first smoothing the profiles.
- Line 290: Do you mean “longitudinal distribution”?
- Tables 1-5 are very detailed and long. Consider moving them to the SI.
- Consider adding a reference to Chang et al. (2024, https://doi.org/10.5194/acp-24-6197-2024) in the last paragraph of the Conclusions when you mention the lack of dense/homogeneous data.
- This paper does not mention satellites which provide data over the oceans and coasts. The authors should mention that this data exists but is being managed by another TOAR working group and is therefore not within the scope of this paper/database.
Technical Corrections
- The legend and region labels (R1, R2, etc.) in Figure 1 should be larger.
- Line 170: “e.g.” should be “i.e.” if you list all cruises with 1-minute based data.
- Section 2.2 should reference Figure 1.
- To the Figure S2 caption, add a comment about why the top row is red and the bottom row is blue.
- Many acronyms are undefined. Rather than defining them in-text, consider adding a table of acronyms to the SI.
- Please replace the in-text URLs with proper references:
- Line 144
- Line 190
- Line 242 (can reference Van Malderen et al., 2025 instead)
- Line 257
- Line 263
Citation: https://doi.org/10.5194/essd-2024-566-RC1
Data sets
Observational ozone data over the global oceans and polar regions: The TOAR-II Oceans data set version 2024 Y. Kanaya et al. https://www.jamstec.go.jp/egcr/e/atmos/observation/toar2oceansdata/index.html
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