Journal Article FZJ-2025-02682

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No severe ozone depletion in the tropical stratosphere in recent decades

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2024
EGU Katlenburg-Lindau

Atmospheric chemistry and physics 24(11), 6743 - 6756 () [10.5194/acp-24-6743-2024]

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Abstract: Stratospheric ozone is an important constituent of the atmosphere. Significant changes in its concentrations have great consequences for the environment in general and for ecosystems in particular. Here, we analyse ground-based, ozonesonde and satellite ozone measurements to examine the ozone depletion and the spatiotemporal trends in ozone in the tropics during the past 5 decades (1980–2020). The amount of column ozone in the tropics is relatively small (250–270 DU) compared to high and mid-latitudes (Northern Hemisphere (NH) 275–425 DU; Southern Hemisphere (SH) 275–350 DU). In addition, the tropical total ozone trend is very small (±0–0.2 DU yr−1), as estimated for the period 1998–2022. No observational evidence is found regarding the indications or signatures of severe stratospheric ozone depletion in the tropics in contrast to a recent claim. Finally, current understanding and observational evidence do not provide any support for the possibility of an ozone hole occurring outside Antarctica today with respect to the present-day stratospheric halogen levels.

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Note: open access

Contributing Institute(s):
  1. Stratosphäre (ICE-4)
Research Program(s):
  1. 2112 - Climate Feedbacks (POF4-211) (POF4-211)

Appears in the scientific report 2024; 2025
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 Record created 2025-05-28, last modified 2026-02-20


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