Secondary ice production in summer clouds over the Antarctic coast: an underappreciated process in atmospheric models
<p>The correct representation of Antarctic clouds in atmospheric models is crucial for accurate projections of the future Antarctic climate. This is particularly true for summer clouds which play a critical role in the surface melting of the ice shelves in the vicinity of the Weddell Sea. The...
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doaj-e8065b01149c4cd9af52de171f6523c62021-01-19T15:33:10ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242021-01-012175577110.5194/acp-21-755-2021Secondary ice production in summer clouds over the Antarctic coast: an underappreciated process in atmospheric modelsG. Sotiropoulou0G. Sotiropoulou1É. Vignon2É. Vignon3G. Young4H. Morrison5H. Morrison6S. J. O'Shea7T. Lachlan-Cope8A. Berne9A. Nenes10A. Nenes11Laboratory of Atmospheric Processes and their Impacts (LAPI), École Polytechnique Fédérale de Lausanne (EPFL), Lausanne, SwitzerlandDepartment of Meteorology, Stockholm University & Bolin Center for Climate Research, Stockholm, SwedenEnvironmental Remote Sensing Laboratory (LTE), EPFL, Lausanne, SwitzerlandLaboratoire de Météorologie Dynamique (LMD), IPSL, Sorbonne Université, CNRS, UMR 8539, Paris, FranceSchool of Earth and Environment, University of Leeds, Leeds, UKNational Center for Atmospheric Research, Boulder, CO, USAARC Centre for Excellence in Climate System Science, University of New South Wales, Sydney, AustraliaCentre for Atmospheric Science, University of Manchester, Manchester, UKBritish Antarctic Survey, Cambridge, UKEnvironmental Remote Sensing Laboratory (LTE), EPFL, Lausanne, SwitzerlandLaboratory of Atmospheric Processes and their Impacts (LAPI), École Polytechnique Fédérale de Lausanne (EPFL), Lausanne, SwitzerlandICE-HT, Foundation for Research and Technology Hellas (FORTH), Patras, Greece<p>The correct representation of Antarctic clouds in atmospheric models is crucial for accurate projections of the future Antarctic climate. This is particularly true for summer clouds which play a critical role in the surface melting of the ice shelves in the vicinity of the Weddell Sea. The pristine atmosphere over the Antarctic coast is characterized by low concentrations of ice nucleating particles (INPs) which often result in the formation of supercooled liquid clouds. However, when ice formation occurs, the ice crystal number concentrations (ICNCs) are substantially higher than those predicted by existing primary ice nucleation parameterizations. The rime-splintering mechanism, thought to be the dominant secondary ice production (SIP) mechanism at temperatures between <span class="inline-formula">−8</span> and <span class="inline-formula">−3</span> <span class="inline-formula"><sup>∘</sup></span>C, is also weak in the Weather and Research Forecasting model. Including a parameterization for SIP due to breakup (BR) from collisions between ice particles improves the ICNC representation in the modeled mixed-phase clouds, suggesting that BR could account for the enhanced ICNCs often found in Antarctic clouds. The model results indicate that a minimum concentration of about <span class="inline-formula">∼</span> 0.1 L<span class="inline-formula"><sup>−1</sup></span> of primary ice crystals is necessary and sufficient to initiate significant breakup to explain the observations, while our findings show little sensitivity to increasing INPs. The BR mechanism is currently not represented in most weather prediction and climate models; including this process can have a significant impact on the Antarctic radiation budget.</p>https://acp.copernicus.org/articles/21/755/2021/acp-21-755-2021.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
G. Sotiropoulou G. Sotiropoulou É. Vignon É. Vignon G. Young H. Morrison H. Morrison S. J. O'Shea T. Lachlan-Cope A. Berne A. Nenes A. Nenes |
spellingShingle |
G. Sotiropoulou G. Sotiropoulou É. Vignon É. Vignon G. Young H. Morrison H. Morrison S. J. O'Shea T. Lachlan-Cope A. Berne A. Nenes A. Nenes Secondary ice production in summer clouds over the Antarctic coast: an underappreciated process in atmospheric models Atmospheric Chemistry and Physics |
author_facet |
G. Sotiropoulou G. Sotiropoulou É. Vignon É. Vignon G. Young H. Morrison H. Morrison S. J. O'Shea T. Lachlan-Cope A. Berne A. Nenes A. Nenes |
author_sort |
G. Sotiropoulou |
title |
Secondary ice production in summer clouds over the Antarctic coast: an underappreciated process in atmospheric models |
title_short |
Secondary ice production in summer clouds over the Antarctic coast: an underappreciated process in atmospheric models |
title_full |
Secondary ice production in summer clouds over the Antarctic coast: an underappreciated process in atmospheric models |
title_fullStr |
Secondary ice production in summer clouds over the Antarctic coast: an underappreciated process in atmospheric models |
title_full_unstemmed |
Secondary ice production in summer clouds over the Antarctic coast: an underappreciated process in atmospheric models |
title_sort |
secondary ice production in summer clouds over the antarctic coast: an underappreciated process in atmospheric models |
publisher |
Copernicus Publications |
series |
Atmospheric Chemistry and Physics |
issn |
1680-7316 1680-7324 |
publishDate |
2021-01-01 |
description |
<p>The correct representation of Antarctic clouds in atmospheric models is
crucial for accurate projections of the future Antarctic climate. This is
particularly true for summer clouds which play a critical role in the
surface melting of the ice shelves in the vicinity of the Weddell Sea. The
pristine atmosphere over the Antarctic coast is characterized by low
concentrations of ice nucleating particles (INPs) which often result in the
formation of supercooled liquid clouds. However, when ice formation occurs,
the ice crystal number concentrations (ICNCs) are substantially higher than
those predicted by existing primary ice nucleation parameterizations. The
rime-splintering mechanism, thought to be the dominant secondary ice
production (SIP) mechanism at temperatures between <span class="inline-formula">−8</span> and <span class="inline-formula">−3</span> <span class="inline-formula"><sup>∘</sup></span>C,
is also weak in the Weather and Research Forecasting model. Including a
parameterization for SIP due to breakup (BR) from collisions between ice
particles improves the ICNC representation in the modeled mixed-phase clouds,
suggesting that BR could account for the enhanced ICNCs often found in
Antarctic clouds. The model results indicate that a minimum concentration of
about <span class="inline-formula">∼</span> 0.1 L<span class="inline-formula"><sup>−1</sup></span> of primary ice crystals is necessary and
sufficient to initiate significant breakup to explain the observations,
while our findings show little sensitivity to increasing INPs. The BR
mechanism is currently not represented in most weather prediction and
climate models; including this process can have a significant impact on the
Antarctic radiation budget.</p> |
url |
https://acp.copernicus.org/articles/21/755/2021/acp-21-755-2021.pdf |
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