Classification of Arctic multilayer clouds using radiosonde and radar data in Svalbard

<p>Multilayer clouds (MLCs) occur more often in the Arctic than globally. In this study we present the results of a detection algorithm applied to radiosonde and radar data from an 1-year time period in Ny-Ålesund, Svalbard. Multilayer cloud occurrence is found on 29&thinsp;% of the invest...

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Main Authors: M. Vassel, L. Ickes, M. Maturilli, C. Hoose
Format: Article
Language:English
Published: Copernicus Publications 2019-04-01
Series:Atmospheric Chemistry and Physics
Online Access:https://www.atmos-chem-phys.net/19/5111/2019/acp-19-5111-2019.pdf
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spelling doaj-d000dff0d81547949a5f203bd14fe8732020-11-24T22:44:32ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242019-04-01195111512610.5194/acp-19-5111-2019Classification of Arctic multilayer clouds using radiosonde and radar data in SvalbardM. Vassel0L. Ickes1M. Maturilli2C. Hoose3Institute of Meteorology and Climate Research, Karlsruhe Institute of Technology, Karlsruhe, GermanyDepartment of Meteorology, Stockholm University, Stockholm, SwedenAlfred Wegener Institute for Polar and Marine Research, Potsdam, GermanyInstitute of Meteorology and Climate Research, Karlsruhe Institute of Technology, Karlsruhe, Germany<p>Multilayer clouds (MLCs) occur more often in the Arctic than globally. In this study we present the results of a detection algorithm applied to radiosonde and radar data from an 1-year time period in Ny-Ålesund, Svalbard. Multilayer cloud occurrence is found on 29&thinsp;% of the investigated days. These multilayer cloud cases are further analysed regarding the possibility of ice crystal seeding, meaning that an ice crystal can survive sublimation in a subsaturated layer between two cloud layers when falling through this layer. For this we analyse profiles of relative humidity with respect to ice to identify super- and subsaturated air layers. Then the sublimation of an ice crystal of an assumed initial size of <span class="inline-formula"><i>r</i>=400</span>&thinsp;<span class="inline-formula">µ</span>m on its way through the subsaturated layer is calculated. If the ice crystal still exists when reaching a lower supersaturated layer, ice crystal seeding can potentially take place. Seeding cases are found often, in 23&thinsp;% of the investigated days (100&thinsp;% includes all days, as well as non-cloudy days). The identification of seeding cases is limited by the radar signal inside the subsaturated layer. Clearly separated multilayer clouds, defined by a clear interstice in the radar image, do not interact through seeding (9&thinsp;% of the investigated days). There are various deviations between the relative humidity profiles and the radar images, e.g. due to the lack of ice-nucleating particles (INPs) and cloud condensation nuclei (CCN). Additionally, horizontal wind drift of the radiosonde and time restriction when comparing radiosonde and radar data cause further deviations. In order to account for some of these deviations, an evaluation by manual visual inspection is done for the non-seeding cases.</p>https://www.atmos-chem-phys.net/19/5111/2019/acp-19-5111-2019.pdf
collection DOAJ
language English
format Article
sources DOAJ
author M. Vassel
L. Ickes
M. Maturilli
C. Hoose
spellingShingle M. Vassel
L. Ickes
M. Maturilli
C. Hoose
Classification of Arctic multilayer clouds using radiosonde and radar data in Svalbard
Atmospheric Chemistry and Physics
author_facet M. Vassel
L. Ickes
M. Maturilli
C. Hoose
author_sort M. Vassel
title Classification of Arctic multilayer clouds using radiosonde and radar data in Svalbard
title_short Classification of Arctic multilayer clouds using radiosonde and radar data in Svalbard
title_full Classification of Arctic multilayer clouds using radiosonde and radar data in Svalbard
title_fullStr Classification of Arctic multilayer clouds using radiosonde and radar data in Svalbard
title_full_unstemmed Classification of Arctic multilayer clouds using radiosonde and radar data in Svalbard
title_sort classification of arctic multilayer clouds using radiosonde and radar data in svalbard
publisher Copernicus Publications
series Atmospheric Chemistry and Physics
issn 1680-7316
1680-7324
publishDate 2019-04-01
description <p>Multilayer clouds (MLCs) occur more often in the Arctic than globally. In this study we present the results of a detection algorithm applied to radiosonde and radar data from an 1-year time period in Ny-Ålesund, Svalbard. Multilayer cloud occurrence is found on 29&thinsp;% of the investigated days. These multilayer cloud cases are further analysed regarding the possibility of ice crystal seeding, meaning that an ice crystal can survive sublimation in a subsaturated layer between two cloud layers when falling through this layer. For this we analyse profiles of relative humidity with respect to ice to identify super- and subsaturated air layers. Then the sublimation of an ice crystal of an assumed initial size of <span class="inline-formula"><i>r</i>=400</span>&thinsp;<span class="inline-formula">µ</span>m on its way through the subsaturated layer is calculated. If the ice crystal still exists when reaching a lower supersaturated layer, ice crystal seeding can potentially take place. Seeding cases are found often, in 23&thinsp;% of the investigated days (100&thinsp;% includes all days, as well as non-cloudy days). The identification of seeding cases is limited by the radar signal inside the subsaturated layer. Clearly separated multilayer clouds, defined by a clear interstice in the radar image, do not interact through seeding (9&thinsp;% of the investigated days). There are various deviations between the relative humidity profiles and the radar images, e.g. due to the lack of ice-nucleating particles (INPs) and cloud condensation nuclei (CCN). Additionally, horizontal wind drift of the radiosonde and time restriction when comparing radiosonde and radar data cause further deviations. In order to account for some of these deviations, an evaluation by manual visual inspection is done for the non-seeding cases.</p>
url https://www.atmos-chem-phys.net/19/5111/2019/acp-19-5111-2019.pdf
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