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Condensation of HNO3 and HCl in the winter polar stratospheres

Toon, Owen B., Hamill, Patrick, Turco, Richard P., Pinto, Joseph·1986·Geophysical Research Letters

Abstract

Nitric acid and hydrochloric acid vapors may condense in the winter polar stratospheres. Nitric acid clouds, unlike water ice clouds, would form at the temperatures at which polar stratospheric clouds (PSCs) are observed and would have optical depths of the magnitude observed suggesting that HNO 3 is a dominant component of PSCs. ClO, N 2 O 5 and ClNO 3 may react on cloud particle surfaces yielding additional HNO 3, HCl, and HOCL. In the vicinity of PSCs these reactions could deplete the stratosphere of photochemically active NO x species. The sedimentation of PSCs may remove these materials from the stratosphere. The loss of vapor phase NO x might allow halogen‐based chemistry to create the ozone hole.

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Metadata

Authors
Toon, O. B., Hamill, P., Turco, R. P., & Pinto, J.
Venue
Geophysical Research Letters
Published
1986-11
Volume
13
Issue
12
Pages
1284-1287
ISSN
  • 0094-8276 (ISSN-L)
  • 1944-8007
OpenAlex
W2165412911
Cited by
504
References
0
FWCI
35.20
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Condensation of HNO3 and HCl in the winter polar stratospheres. https://app.cochat.ai/papers/10.1029/gl013i012p01284
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Toon, O. B., Hamill, P., Turco, R. P., & Pinto, J. (1986). Condensation of HNO3 and HCl in the winter polar stratospheres. Geophysical Research Letters. https://doi.org/10.1029/gl013i012p01284

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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).

Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.