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|a 10.1029/2022GL100091
|2 doi
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|a pubmed24n1528.xml
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|a eng
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|a Taha, G
|e verfasserin
|4 aut
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|a Tracking the 2022 Hunga Tonga-Hunga Ha'apai Aerosol Cloud in the Upper and Middle Stratosphere Using Space-Based Observations
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|c 2022
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|a Text
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|a ƒaComputermedien
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|2 rdamedia
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|a ƒa Online-Ressource
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|a Date Revised 09.09.2024
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|a published: Print-Electronic
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|a Citation Status PubMed-not-MEDLINE
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|a © 2022. The Authors.
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|a On 15 January 2022, the submarine Hunga Tonga volcanic eruption lofted materials high into the upper stratosphere, reaching a record-breaking altitude of ∼58 km, unprecedented in the satellite observations era. Within two weeks, the bulk of the injected material circulated the globe between 20-30 km altitude, as observed by satellite instruments. We estimate that the stratospheric aerosol optical depth (sAOD) is the largest since the Pinatubo eruption and is at least twice as great as the sAOD after the 2015 Calbubo eruption despite the similar SO2 injection from that eruption. We use space-based observations to monitor the Hunga-Tonga volcanic plume evolution and transport at different altitudes as it circulates the globe. While the main aerosol layer remains trapped in the tropical pipe, small parts have already made it to both the northern and southern hemisphere poles by April, which is almost certain to influence this year's ozone hole
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|a Journal Article
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|a OMPS LP
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|a SAGE III/ISS
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|a aerosols
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|a hunga Tonga
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|a stratosphere
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|a volcanic eruption
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|a Loughman, R
|e verfasserin
|4 aut
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|a Colarco, P R
|e verfasserin
|4 aut
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|a Zhu, T
|e verfasserin
|4 aut
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|a Thomason, L W
|e verfasserin
|4 aut
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|a Jaross, G
|e verfasserin
|4 aut
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|i Enthalten in
|t Geophysical research letters
|d 1984
|g 49(2022), 19 vom: 16. Okt., Seite e2022GL100091
|w (DE-627)NLM098182501
|x 0094-8276
|7 nnns
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| 773 |
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|g volume:49
|g year:2022
|g number:19
|g day:16
|g month:10
|g pages:e2022GL100091
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|u http://dx.doi.org/10.1029/2022GL100091
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