The DOI matches its Crossref record; 17 of the 17 references it cites were found in a registry or an index.
Stratospheric aerosol growth and HNO3 gas phase depletion from coupled HNO3 and water uptake by liquid particles
Abstract
Aqueous sulphuric acid droplets, which constitute the background stratospheric aerosol, strongly absorb HNO 3 and HCl under cold conditions. A thermodynamic model is used to predict partitioning of HNO 3, HCl and H 2 O between gas and aerosol phases, and show that a 50‐fold increase in aerosol volume, observed in the Arctic stratosphere as temperature approached the frost point (188.9 K), can be explained in terms of uptake of HNO 3 and H 2 O by liquid aerosols. Calculated degrees of saturation of the droplets with respect to solid hydrates, taking into account the reduction in vapour phase HNO 3, suggest that the droplets remain liquid to the frost point. Near this temperature, they can yield larger aerosol volumes than would have been the case for solid NAT (HNO 3•3H 2 O) particles. The depletion of gas phase HNO 3 into enhanced volumes of liquid aerosols resulting from volcanic eruptions may hamper NAT formation.
Overview
The claims and statistics of this paper haven’t been checked yet.
Run the check — free, no account needed. It reads the open-access text and checks the sources it cites.
Integrity signals
Registry
Cites
Statistics
Verification
Claims the paper makes
The claims and statistics of this paper haven’t been checked yet.
Run the check — free, no account needed. It reads the open-access text and checks the sources it cites.
Self-check
Percentages, sums and reported differences re-computed from the paper’s own numbers.
The self-check needs the paper’s full text.
Citations
Cites
Laboratory studies of the nitric acid trihydrate: Implications for the south polar stratosphere
Hanson, D., & Mauersberger, K. (1988) · Geophysical Research Letters · doi:10.1029/gl015i008p00855 · Cited by 755
Heterogeneous reactions in sulfuric acid aerosols: A framework for model calculations
Hanson, D. R., Ravishankara, A. R., & Solomon, S. (1994) · Journal of Geophysical Research: Atmospheres · doi:10.1029/93jd02932 · Cited by 473
Clegg, S. L., Pitzer, K. S., & Brimblecombe, P. (1992) · The Journal of Physical Chemistry · doi:10.1021/j100202a074 · Cited by 362
Self-citationDye, J. E., Baumgardner, D., Gandrud, B. W., Kawa, S. R., Kelly, K. K., Loewenstein, M., Ferry, G. V., Chan, K. R., & Gary, B. L. (1992) · Journal of Geophysical Research: Atmospheres · doi:10.1029/91jd02740 · Cited by 259
Physical Chemistry of the H 2 SO 4 /HNO 3 /H 2 O System: Implications for Polar Stratospheric Clouds
Molina, M. J., Zhang, R., Wooldridge, P. J., McMahon, J. R., Kim, J. E., Chang, H. Y., & Beyer, K. D. (1993) · Science · doi:10.1126/science.261.5127.1418 · Cited by 257
Role of heterogeneous conversion of N2O5 on sulphate aerosols in global ozone losses
Rodriguez, J. M., Ko, M. K. W., & Sze, N. D. (1991) · Nature · doi:10.1038/352134a0 · Cited by 231
A study of type I polar stratospheric cloud formation
Tabazadeh, A., Turco, R. P., Drdla, K., Jacobson, M. Z., & Toon, O. B. (1994) · Geophysical Research Letters · doi:10.1029/94gl01368 · Cited by 223
An analysis of lidar observations of polar stratospheric clouds
Toon, O. B., Browell, E. V., Kinne, S., & Jordan, J. (1990) · Geophysical Research Letters · doi:10.1029/gl017i004p00393 · Cited by 193
Deshler, T., Hofmann, D. J., Johnson, B. J., & Rozier, W. R. (1992) · Geophysical Research Letters · doi:10.1029/91gl02787 · Cited by 188
A model for studying the composition and chemical effects of stratospheric aerosols
Tabazadeh, A., TURCO, R. P., & Jacobson, M. Z. (1994) · Journal of Geophysical Research Atmospheres · doi:10.1029/94jd00820 · Cited by 154
Cited by
Stratospheric ozone depletion: A review of concepts and history
Solomon, S. (1999) · Reviews of Geophysics · doi:10.1029/1999rg900008 · Cited by 2,008
Thermodynamic Model of the System H+−NH4+−SO42-−NO3-−H2O at Tropospheric Temperatures
Clegg, S. L., Brimblecombe, P., & Wexler, A. S. (1998) · The Journal of Physical Chemistry A · doi:10.1021/jp973042r · Cited by 782
Self-citationPhase Transitions of Aqueous Atmospheric Particles
Martin, S. T. (2000) · Chemical Reviews · doi:10.1021/cr990034t · Cited by 718
Voigt, C., Schlager, H., Luo, B. P., Dörnbrack, A., Roiger, A., Stock, P., Curtius, J., Vössing, H., Borrmann, S., Davies, S., et al. (2005) · Atmospheric Chemistry and Physics · doi:10.5194/acp-5-1371-2005 · Cited by 161
Self-citationObservations of the chemical composition of stratospheric aerosol particles
Murphy, D. M., Froyd, K. D., Schwarz, J. P., & Wilson, J. C. (2014) · Quarterly Journal of the Royal Meteorological Society · doi:10.1002/qj.2213 · Cited by 141
Metadata
- Authors
- Carslaw, K. S., Luo, B. P., Clegg, S. L., Peter, T., Brimblecombe, P., & Crutzen, P. J.
- Venue
- Geophysical Research Letters
- Publisher
- American Geophysical Union (AGU)
- Published
- 1994-11-15
- Volume
- 21
- Issue
- 23
- Pages
- 2479-2482
- ISSN
- 0094-8276 (ISSN-L)
- 1944-8007
- OpenAlex
- W2030397317
- Cited by
- 374
- References
- 17
- FWCI
- 25.81
- Type
- journal article
- Language
- en
- Open access
- closed
About these checks
Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
Statistics and arithmetic are recomputed, not judged.
Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.
What counts as a claim ›How we measure confidence ›How we check this ›
Are you an author, or do you see a problem with this page? Request a review
How to cite
Cite CoChat for the checks on this page, and the paper for its own findings.
- This page
- CoChat. (2026). Citation check: Stratospheric aerosol growth and HNO3 gas phase depletion from coupled HNO3 and water uptake by liquid particles. https://app.cochat.ai/papers/10.1029/94gl02799
- The paper
- Carslaw, K. S., Luo, B. P., Clegg, S. L., Peter, T., Brimblecombe, P., & Crutzen, P. J. (1994). Stratospheric aerosol growth and HNO3 gas phase depletion from coupled HNO3 and water uptake by liquid particles. Geophysical Research Letters. https://doi.org/10.1029/94gl02799
Data sources
Bibliographic data: Semantic Scholar, OpenAlex, Crossref.
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.