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Abstract: Multi-Decadal Increase of Humidity in the Stratospheric Ozone Layer Caused by Warming of the Tropical Tropopause Layer and by Subsequent Poleward Drift of Brewer-Dobson Circulation (AGU25)

Multi-Decadal Increase of Humidity in the Stratospheric Ozone Layer Caused by Warming of the Tropical Tropopause Layer and by Subsequent Poleward Drift of Brewer-Dobson Circulation

Walter E Janach, Retired, Meggen, Switzerland and Roy Freeman, Self-Employed, Luzern, Switzerland
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