Exploring the uncertainties in the aviation soot-cirrus effect

A global aerosol-climate model, including a two-moment cloud microphysical scheme and a parametrization for aerosol-induced ice formation in cirrus clouds, is applied in order to quantify the impact of aviation soot on natural cirrus clouds. Several sensitivity experiments are performed to assess th...

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Main Authors: Righi, Mattia, Hendricks, Johannes, Beer, Christof Gerhard
Format: Text
Language:English
Published: 2021
Subjects:
Online Access:https://doi.org/10.5194/acp-2021-329
https://acp.copernicus.org/preprints/acp-2021-329/
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spelling ftcopernicus:oai:publications.copernicus.org:acpd94133 2023-05-15T18:18:47+02:00 Exploring the uncertainties in the aviation soot-cirrus effect Righi, Mattia Hendricks, Johannes Beer, Christof Gerhard 2021-06-18 application/pdf https://doi.org/10.5194/acp-2021-329 https://acp.copernicus.org/preprints/acp-2021-329/ eng eng doi:10.5194/acp-2021-329 https://acp.copernicus.org/preprints/acp-2021-329/ eISSN: 1680-7324 Text 2021 ftcopernicus https://doi.org/10.5194/acp-2021-329 2021-06-21T16:22:14Z A global aerosol-climate model, including a two-moment cloud microphysical scheme and a parametrization for aerosol-induced ice formation in cirrus clouds, is applied in order to quantify the impact of aviation soot on natural cirrus clouds. Several sensitivity experiments are performed to assess the uncertainties in this effect related to (i) the assumptions on the ice nucleation abilities of aviation soot; (ii) the representation of vertical updrafts in the model; and (iii) the use of reanalysis data to relax the model dynamics (the so-called nudging technique). Based on the results of the model simulations, a radiative forcing from the aviation soot-cirrus effect in the range of −35 mW m −2 to 13 mW m −2 is quantified, depending on the assumed critical saturation ratio for ice nucleation and active fraction of aviation soot, but with a confidence level below 95 % in several cases. Simple idealized experiments with prescribed vertical velocities further show that the uncertainties on this aspect of the model dynamics are critical for the investigated effect and could potentially add a factor of about two of further uncertainty to the model estimates of the resulting radiative forcing. The use of the nudging technique to relax model dynamics is proved essential in order to identify a statistically significant signal from the model internal variability, while simulations performed in free-running mode and with prescribed sea-surface temperatures and sea-ice concentrations are shown to be unable to provide robust estimates of the investigated effect. A comparison with analogous model studies on the aviation-soot cirrus effect show a very large model diversity, with a conspicuous lack of consensus across the various estimates, which points to the need for more in-depth analyses on the roots of such discrepancies. Text Sea ice Copernicus Publications: E-Journals
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description A global aerosol-climate model, including a two-moment cloud microphysical scheme and a parametrization for aerosol-induced ice formation in cirrus clouds, is applied in order to quantify the impact of aviation soot on natural cirrus clouds. Several sensitivity experiments are performed to assess the uncertainties in this effect related to (i) the assumptions on the ice nucleation abilities of aviation soot; (ii) the representation of vertical updrafts in the model; and (iii) the use of reanalysis data to relax the model dynamics (the so-called nudging technique). Based on the results of the model simulations, a radiative forcing from the aviation soot-cirrus effect in the range of −35 mW m −2 to 13 mW m −2 is quantified, depending on the assumed critical saturation ratio for ice nucleation and active fraction of aviation soot, but with a confidence level below 95 % in several cases. Simple idealized experiments with prescribed vertical velocities further show that the uncertainties on this aspect of the model dynamics are critical for the investigated effect and could potentially add a factor of about two of further uncertainty to the model estimates of the resulting radiative forcing. The use of the nudging technique to relax model dynamics is proved essential in order to identify a statistically significant signal from the model internal variability, while simulations performed in free-running mode and with prescribed sea-surface temperatures and sea-ice concentrations are shown to be unable to provide robust estimates of the investigated effect. A comparison with analogous model studies on the aviation-soot cirrus effect show a very large model diversity, with a conspicuous lack of consensus across the various estimates, which points to the need for more in-depth analyses on the roots of such discrepancies.
format Text
author Righi, Mattia
Hendricks, Johannes
Beer, Christof Gerhard
spellingShingle Righi, Mattia
Hendricks, Johannes
Beer, Christof Gerhard
Exploring the uncertainties in the aviation soot-cirrus effect
author_facet Righi, Mattia
Hendricks, Johannes
Beer, Christof Gerhard
author_sort Righi, Mattia
title Exploring the uncertainties in the aviation soot-cirrus effect
title_short Exploring the uncertainties in the aviation soot-cirrus effect
title_full Exploring the uncertainties in the aviation soot-cirrus effect
title_fullStr Exploring the uncertainties in the aviation soot-cirrus effect
title_full_unstemmed Exploring the uncertainties in the aviation soot-cirrus effect
title_sort exploring the uncertainties in the aviation soot-cirrus effect
publishDate 2021
url https://doi.org/10.5194/acp-2021-329
https://acp.copernicus.org/preprints/acp-2021-329/
genre Sea ice
genre_facet Sea ice
op_source eISSN: 1680-7324
op_relation doi:10.5194/acp-2021-329
https://acp.copernicus.org/preprints/acp-2021-329/
op_doi https://doi.org/10.5194/acp-2021-329
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