Polar mesospheric ozone loss initiates downward coupling of solar signal in the Northern Hemisphere
Annika Seppälä (),
Niilo Kalakoski,
Pekka T. Verronen,
Daniel R. Marsh,
Alexey Yu. Karpechko and
Monika E. Szelag
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Annika Seppälä: University of Otago
Niilo Kalakoski: Finnish Meteorological Institute
Pekka T. Verronen: Finnish Meteorological Institute
Daniel R. Marsh: National Center for Atmospheric Research
Alexey Yu. Karpechko: Finnish Meteorological Institute
Monika E. Szelag: Finnish Meteorological Institute
Nature Communications, 2025, vol. 16, issue 1, 1-7
Abstract:
Abstract Solar driven energetic particle precipitation (EPP) is an important factor in polar atmospheric ozone balance and has been linked to ground-level regional climate variability. However, the linking mechanism has remained ambiguous. The observed and simulated ground-level changes start well before the processes from the main candidate, the so-called EPP-indirect effect, would start. Here we show that initial reduction of polar mesospheric ozone and the resulting change in atmospheric heating rapidly couples to dynamics, transferring the signal downwards, shifting the tropospheric jet polewards. This pathway is not constrained to the polar vortex. Rather, a subtropical route initiated by a changing wind shear plays a key role. Our results show that the signal propagates downwards in timescales consistent with observed tropospheric level climatic changes linked to EPP. This pathway, from mesospheric ozone to regional climate, is independent of the EPP-indirect effect, and solves the long-standing mechanism problem for EPP effects on climate.
Date: 2025
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DOI: 10.1038/s41467-025-55966-z
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