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Raikoke volcanic sulfate/SO2 anticyclonic contained circulations: in situ proof, morphology, and radiative signature

Abstract:

300–400 km in diameter. Previous reports showed that one of these entities was traceable for 3 months. Anticyclonic circulation was also previously reported. We present multiple lines of evidence to characterize these cloud subelements by their spatial confinement, morphology, and sulfate-dominated aerosol aspect, which was evident from plume onset. In addition, we show that they were ably identifiable in geostationary satellite “cirrus channel” reflectance imagery and had an enduring signal of window infrared absorption, detectable for at least 1 month. The term we apply to this phenomenon is “sulfate/SO2 anticyclonic contained circulation,” abbreviated SSACC. Anticyclonic circulation is first detectable on 24 June, 2 days posteruption. Two SSACCs persist beyond June. One is traceable until mid-August over Canada. The other SSACC was discernible until 5 October after having completed three global circumnavigations. The internal SSACC circulation aspect is gleaned from geostationary-based visible image animations and confirmed in situ via a novel application of high-resolution radiosonde wind direction and balloon position data. We also examine diabatic lofting of both SSACCs in relation to their individual geographic and constituent morphologies. Thermal infrared observations show that SSACC aerosols produce brightness temperature depressions of ~2.6 K, opening a new line of investigation into the source of heating that contributes to diabatic rise.

Publication status:
Published
Peer review status:
Peer reviewed

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Publisher copy:
10.1029/2024jd041653

Authors


More by this author
Role:
Author
ORCID:
0000-0002-0412-9202
More by this author
Role:
Author
ORCID:
0000-0002-0724-7669
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Institution:
University of Oxford
Division:
MPLS
Department:
Physics
Sub department:
Atmos Ocean & Planet Physics
Oxford college:
Queen's College
Role:
Author
ORCID:
0000-0002-6824-893X
More by this author
Institution:
University of Oxford
Division:
MPLS
Department:
Physics
Sub department:
Atmos Ocean & Planet Physics
Oxford college:
St Hugh's College
Role:
Author
ORCID:
0000-0003-0709-1315
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Role:
Author
ORCID:
0000-0003-4047-0181


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Funder identifier:
https://ror.org/02b5d8509
Grant:
NE/S004025/1


Publisher:
Wiley
Journal:
Journal of Geophysical Research: Atmospheres More from this journal
Volume:
130
Issue:
17
Article number:
e2024JD041653
Publication date:
2025-08-29
Acceptance date:
2025-08-05
DOI:
EISSN:
2169-8996
ISSN:
2169-897X


Language:
English
Keywords:
Pubs id:
2285261
Local pid:
pubs:2285261
Deposit date:
2025-09-07

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