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Visible spectroscopy at McMurdo Station, Antarctica: 2. Observations of OClO

Solomon, S., Mount, G. H., Sanders, R. W., Schmeltekopf, A. L.·1987·Journal of Geophysical Research: Atmospheres

Abstract

The column abundance of OClO at McMurdo Station, Antarctica, was measured by visible absorption spectroscopy during austral spring in 1986. Observations were obtained during the day using scattered sunlight and at night using direct light from the moon. The observed total column amounts in Antarctica were about 20–50 times larger than would be expected for standard homogeneous photochemistry, suggesting that the halogen chemistry of Antarctic spring is profoundly different from such standard theoretical expectations and may play a role in the development of the springtime Antarctic ozone “hole.”

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Metadata

Authors
Solomon, S., Mount, G. H., Sanders, R. W., & Schmeltekopf, A. L.
Venue
Journal of Geophysical Research: Atmospheres
Published
1987-07-20
Volume
92
Issue
D7
Pages
8329-8338
ISSN
0148-0227 (ISSN-L)
OpenAlex
W1971513090
Cited by
242
References
0
FWCI
25.57
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Visible spectroscopy at McMurdo Station, Antarctica: 2. Observations of OClO. https://app.cochat.ai/papers/10.1029/jd092id07p08329
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Solomon, S., Mount, G. H., Sanders, R. W., & Schmeltekopf, A. L. (1987). Visible spectroscopy at McMurdo Station, Antarctica: 2. Observations of OClO. Journal of Geophysical Research: Atmospheres. https://doi.org/10.1029/jd092id07p08329

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