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- W4220672591 abstract "<strong class=journal-contentHeaderColor>Abstract.</strong> The Mt. Pinatubo eruption in 1991 had a severe impact on the Earth system, with a well-documented warming of the tropical lower stratosphere and a general cooling of the surface. This study focuses on the impact of this event on the mesosphere by analyzing solar occultation temperature data from the Halogen Occultation Experiment (HALOE) instrument on the Upper Atmosphere Research Satellite (UARS). Previous analyses of lidar temperature data found positive temperature anomalies of up to 12.9âK in the upper mesosphere that peaked in 1993 and were attributed to the Pinatubo eruption. Fitting the HALOE data according to a previously published method indicates a maximum warming of the mesosphere region of 4.1â<span class=inline-formula>±</span>â1.4âK and does not confirm significantly higher values reported for that lidar time series. An alternative fit is proposed that assumes a more rapid response of the mesosphere to the volcanic event and approximates the signature of the Pinatubo with an exponential decay function having an <span class=inline-formula><i>e</i></span>-folding time of 6 months. It suggests a maximum warming of 5.4â<span class=inline-formula>±</span>â3.0âK, if the mesospheric perturbation is assumed to reach its peak 4 months after the eruption. We conclude that the HALOE time series probably captures the decay of a Pinatubo-induced mesospheric warming at the beginning of its measurement period." @default.
- W4220672591 created "2022-04-03" @default.
- W4220672591 creator A5066014775 @default.
- W4220672591 date "2022-03-16" @default.
- W4220672591 modified "2023-09-30" @default.
- W4220672591 title "Reply on CC1" @default.
- W4220672591 doi "https://doi.org/10.5194/angeo-2021-50-ac2" @default.
- W4220672591 hasPublicationYear "2022" @default.
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