the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Strateole 2 balloons reveal persistent errors in reanalyzed winds and trajectory calculations in the tropical lower stratosphere
Abstract. Winds in the tropical lower stratosphere raise difficulties for numerical weather prediction models: without geostrophy, winds decouple from temperature and direct observations are scarce. The Strateole 2 project explores the tropical lower stratosphere using superpressure balloons that drift for up to three months between 18 and 21 km altitude. Wind is measured on all flights: eight in the first campaign (2019–2020) and seventeen in the second (2021–2022). These measurements are used to assess errors in the winds of the ERA5 reanalysis for latitudes between 18° S and 10° N. Two additional objectives of this study are to assess errors in modelled balloon trajectories, and to document the dispersion of air below the balloons, in order to facilitate the interpretation of observations made below the balloons. The comparison of measured and reanalyzed winds reveal significant errors, with standard deviations of 3.76 m s−1 for zonal and 3.24 m s−1 for meridional wind. Relative to a previous comparison in 2010, only a modest decrease of 20 and 10 % is found. Trajectory calculations have very variable skill, with median errors after 24 hours of 260 km, but a tenth of the errors larger than 600 km. Factors leading to large errors, such as initial wind error and latitude are identified. Similarly, trajectory dispersion of air below the balloon is very variable, depending on the initial shear. The persistent errors highlight the need for regular obsevations of winds in the tropical lower stratosphere, and emphasize the need for caution when using trajectory calculations for process studies.
Competing interests: At least one of the (co-)authors is a member of the editorial board of Atmospheric Chemistry and Physics.
Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this paper. While Copernicus Publications makes every effort to include appropriate place names, the final responsibility lies with the authors. Views expressed in the text are those of the authors and do not necessarily reflect the views of the publisher.- Preprint
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Status: final response (author comments only)
- RC1: 'Comment on egusphere-2025-3208', Anonymous Referee #1, 22 Aug 2025
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RC2: 'Comment on egusphere-2025-3208', Anonymous Referee #2, 23 Sep 2025
Review of Strateole 2 Balloons Reveals Persistent Errors in Reanalyzed Winds and Trajectory Calculations in the Tropical Lower Stratosphere
In this paper, superpressure balloon measurements from the Strateole 2 campaign have been used to investigate errors in ERA5 reanalysis winds and the dispersion of trajectories in the equatorial lower stratosphere. The analysis appears sound, and the results are useful, especially in relation to forecasting trajectories for future campaigns. The paper can be considered for publication after the authors address the following comments and suggestions:
Comments and Suggestions
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The location of the balloon launch should be marked in Figure 1. Additionally, clarify what the different colors represent in the figure and update the figure caption accordingly.
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Figure 2 is interesting. What is the reason for the large differences in forecasted trajectories between the two launches that occurred during the same season?
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Line 2010: For zonal wind (panel a, not b), remove the extra parenthesis.
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Line 180: Please discuss the importance of the Gaussian distribution of errors.
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The authors attribute biases in wind to missing components of Kelvin wave variability in the reanalysis. What were the phases and amplitudes of the Kelvin waves during the campaign period? Is there any supporting evidence from other observations?
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Rossby waves have comparable amplitudes to Kelvin waves over the analyzed latitudes. Why is the effect of Rossby waves on wind bias minimal compared to Kelvin waves?
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It would also be useful to provide a figure showing the errors in the direction of forecasted/modelled trajectories, similar to Figure 8.
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Line 275: The sentence “in other words, many poorly modelled trajectories are poor from the start because the initial wind is already wrong” reads awkwardly. Please consider rephrasing for clarity.
Citation: https://doi.org/10.5194/egusphere-2025-3208-RC2 -
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AC1: 'Comment on egusphere-2025-3208: reply to the two reviews', Riwal Plougonven, 10 Nov 2025
We are thankful to the reviewers for their comments and suggestions, and for the careful reading of the manuscript. In the attached file we reproduce their comments (in black). We provide our answers and explanations (in blue) and describe how the text has been modified accordingly.
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This manuscript provides a detailed and quantitative assessment of wind and trajectory errors in reanalyses using the highly valuable Strateole-2 balloon data covering the equatorial and subtropical regions. Both the methodology and explanations are reasonable and presented in sufficient detail. I have no major comments, and would only like to point out minor typos and the ordering of figures and tables.