Heterogeneous formation of polar stratospheric clouds – Part 1: Nucleation of nitric acid trihydrate (NAT)

Satellite-based observations during the Arctic winter of 2009/2010 provide firm evidence that, in contrast to the current understanding, the nucleation of nitric acid trihydrate (NAT) in the polar stratosphere does not only occur on preexisting ice particles. In order to explain the NAT clouds obser...

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Published in:Atmospheric Chemistry and Physics
Main Authors: Hoyle, C. R., Engel, I., Luo, B. P., Pitts, M. C., Poole, L. R., Grooß, J.-U., Peter, T.
Format: Other/Unknown Material
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/acp-13-9577-2013
https://www.atmos-chem-phys.net/13/9577/2013/
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author Hoyle, C. R.
Engel, I.
Luo, B. P.
Pitts, M. C.
Poole, L. R.
Grooß, J.-U.
Peter, T.
author_facet Hoyle, C. R.
Engel, I.
Luo, B. P.
Pitts, M. C.
Poole, L. R.
Grooß, J.-U.
Peter, T.
author_sort Hoyle, C. R.
collection Copernicus Publications: E-Journals
container_issue 18
container_start_page 9577
container_title Atmospheric Chemistry and Physics
container_volume 13
description Satellite-based observations during the Arctic winter of 2009/2010 provide firm evidence that, in contrast to the current understanding, the nucleation of nitric acid trihydrate (NAT) in the polar stratosphere does not only occur on preexisting ice particles. In order to explain the NAT clouds observed over the Arctic in mid-December 2009, a heterogeneous nucleation mechanism is required, occurring via immersion freezing on the surface of solid particles, likely of meteoritic origin. For the first time, a detailed microphysical modelling of this NAT formation pathway has been carried out. Heterogeneous NAT formation was calculated along more than sixty thousand trajectories, ending at Cloud Aerosol Lidar with Orthogonal Polarization (CALIOP) observation points. Comparing the optical properties of the modelled NAT with these observations enabled a thorough validation of a newly developed NAT nucleation parameterisation, which has been built into the Zurich Optical and Microphysical box Model (ZOMM). The parameterisation is based on active site theory, is simple to implement in models and provides substantial advantages over previous approaches which involved a constant rate of NAT nucleation in a given volume of air. It is shown that the new method is capable of reproducing observed polar stratospheric clouds (PSCs) very well, despite the varied conditions experienced by air parcels travelling along the different trajectories. In a companion paper, ZOMM is applied to a later period of the winter, when ice PSCs are also present, and it is shown that the observed PSCs are also represented extremely well under these conditions.
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spelling ftcopernicus:oai:publications.copernicus.org:acp19438 2025-01-16T20:31:12+00:00 Heterogeneous formation of polar stratospheric clouds – Part 1: Nucleation of nitric acid trihydrate (NAT) Hoyle, C. R. Engel, I. Luo, B. P. Pitts, M. C. Poole, L. R. Grooß, J.-U. Peter, T. 2018-01-15 info:eu-repo/semantics/application/pdf https://doi.org/10.5194/acp-13-9577-2013 https://www.atmos-chem-phys.net/13/9577/2013/ eng eng info:eu-repo/grantAgreement/EC/FP7/226365 doi:10.5194/acp-13-9577-2013 https://www.atmos-chem-phys.net/13/9577/2013/ info:eu-repo/semantics/openAccess eISSN: 1680-7324 info:eu-repo/semantics/Text 2018 ftcopernicus https://doi.org/10.5194/acp-13-9577-2013 2019-12-24T09:55:01Z Satellite-based observations during the Arctic winter of 2009/2010 provide firm evidence that, in contrast to the current understanding, the nucleation of nitric acid trihydrate (NAT) in the polar stratosphere does not only occur on preexisting ice particles. In order to explain the NAT clouds observed over the Arctic in mid-December 2009, a heterogeneous nucleation mechanism is required, occurring via immersion freezing on the surface of solid particles, likely of meteoritic origin. For the first time, a detailed microphysical modelling of this NAT formation pathway has been carried out. Heterogeneous NAT formation was calculated along more than sixty thousand trajectories, ending at Cloud Aerosol Lidar with Orthogonal Polarization (CALIOP) observation points. Comparing the optical properties of the modelled NAT with these observations enabled a thorough validation of a newly developed NAT nucleation parameterisation, which has been built into the Zurich Optical and Microphysical box Model (ZOMM). The parameterisation is based on active site theory, is simple to implement in models and provides substantial advantages over previous approaches which involved a constant rate of NAT nucleation in a given volume of air. It is shown that the new method is capable of reproducing observed polar stratospheric clouds (PSCs) very well, despite the varied conditions experienced by air parcels travelling along the different trajectories. In a companion paper, ZOMM is applied to a later period of the winter, when ice PSCs are also present, and it is shown that the observed PSCs are also represented extremely well under these conditions. Other/Unknown Material Arctic Copernicus Publications: E-Journals Arctic Atmospheric Chemistry and Physics 13 18 9577 9595
spellingShingle Hoyle, C. R.
Engel, I.
Luo, B. P.
Pitts, M. C.
Poole, L. R.
Grooß, J.-U.
Peter, T.
Heterogeneous formation of polar stratospheric clouds – Part 1: Nucleation of nitric acid trihydrate (NAT)
title Heterogeneous formation of polar stratospheric clouds – Part 1: Nucleation of nitric acid trihydrate (NAT)
title_full Heterogeneous formation of polar stratospheric clouds – Part 1: Nucleation of nitric acid trihydrate (NAT)
title_fullStr Heterogeneous formation of polar stratospheric clouds – Part 1: Nucleation of nitric acid trihydrate (NAT)
title_full_unstemmed Heterogeneous formation of polar stratospheric clouds – Part 1: Nucleation of nitric acid trihydrate (NAT)
title_short Heterogeneous formation of polar stratospheric clouds – Part 1: Nucleation of nitric acid trihydrate (NAT)
title_sort heterogeneous formation of polar stratospheric clouds – part 1: nucleation of nitric acid trihydrate (nat)
url https://doi.org/10.5194/acp-13-9577-2013
https://www.atmos-chem-phys.net/13/9577/2013/