SID-3 Liquid and Ice Phase Particle Size Distributions measured during ACLOUD ...

This data set contains particle size distributions of spherical and aspherical cloud particles between 5 and 45 microns with a 10-second time resolution calculated from the Small Ice Detector Mark 3 (SID-3). The SID-3 detects individual cloud particles passing a 532 nm laser beam using two nested tr...

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Bibliographic Details
Main Authors: Järvinen, Emma, Schnaiter, Martin
Format: Dataset
Language:English
Published: PANGAEA 2023
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.960269
https://doi.pangaea.de/10.1594/PANGAEA.960269
id ftdatacite:10.1594/pangaea.960269
record_format openpolar
spelling ftdatacite:10.1594/pangaea.960269 2023-12-31T10:03:31+01:00 SID-3 Liquid and Ice Phase Particle Size Distributions measured during ACLOUD ... Järvinen, Emma Schnaiter, Martin 2023 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.960269 https://doi.pangaea.de/10.1594/PANGAEA.960269 en eng PANGAEA https://dx.doi.org/10.5194/acp-23-7611-2023 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 ACLOUD Arctic clouds Polar 6 SID-3 size distribution Event label DATE/TIME netCDF file netCDF file File Size Aircraft Small Ice Detector Mark 3 SID-3 P6_206_ACLOUD_2017 POLAR 6 Arctic Amplification AC3 Dataset dataset 2023 ftdatacite https://doi.org/10.1594/pangaea.96026910.5194/acp-23-7611-2023 2023-12-01T10:50:01Z This data set contains particle size distributions of spherical and aspherical cloud particles between 5 and 45 microns with a 10-second time resolution calculated from the Small Ice Detector Mark 3 (SID-3). The SID-3 detects individual cloud particles passing a 532 nm laser beam using two nested trigger detectors. The trigger signal is recorded as a histogram with a maximum rate of 11 kHz that can be used to derive particle size distributions by using the procedure described in Vochezer et al. (2016), doi:10.5194/amt-9-159-2016. For a sub-set of triggered particles a two-dimensional (2-D) scattering pattern is recorded that can be analysed for particle sphericity by a specifically developed image analysis software. Occasionally, coincidence sampling in the camera field of view causes optical distortions of the 2-D scattering patterns of liquid droplets and, consequently, a misclassification of such scattering patterns to be aspherical by the classification software. For the subsequent identification and ... Dataset Arctic DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic ACLOUD
Arctic clouds
Polar 6
SID-3
size distribution
Event label
DATE/TIME
netCDF file
netCDF file File Size
Aircraft
Small Ice Detector Mark 3 SID-3
P6_206_ACLOUD_2017
POLAR 6
Arctic Amplification AC3
spellingShingle ACLOUD
Arctic clouds
Polar 6
SID-3
size distribution
Event label
DATE/TIME
netCDF file
netCDF file File Size
Aircraft
Small Ice Detector Mark 3 SID-3
P6_206_ACLOUD_2017
POLAR 6
Arctic Amplification AC3
Järvinen, Emma
Schnaiter, Martin
SID-3 Liquid and Ice Phase Particle Size Distributions measured during ACLOUD ...
topic_facet ACLOUD
Arctic clouds
Polar 6
SID-3
size distribution
Event label
DATE/TIME
netCDF file
netCDF file File Size
Aircraft
Small Ice Detector Mark 3 SID-3
P6_206_ACLOUD_2017
POLAR 6
Arctic Amplification AC3
description This data set contains particle size distributions of spherical and aspherical cloud particles between 5 and 45 microns with a 10-second time resolution calculated from the Small Ice Detector Mark 3 (SID-3). The SID-3 detects individual cloud particles passing a 532 nm laser beam using two nested trigger detectors. The trigger signal is recorded as a histogram with a maximum rate of 11 kHz that can be used to derive particle size distributions by using the procedure described in Vochezer et al. (2016), doi:10.5194/amt-9-159-2016. For a sub-set of triggered particles a two-dimensional (2-D) scattering pattern is recorded that can be analysed for particle sphericity by a specifically developed image analysis software. Occasionally, coincidence sampling in the camera field of view causes optical distortions of the 2-D scattering patterns of liquid droplets and, consequently, a misclassification of such scattering patterns to be aspherical by the classification software. For the subsequent identification and ...
format Dataset
author Järvinen, Emma
Schnaiter, Martin
author_facet Järvinen, Emma
Schnaiter, Martin
author_sort Järvinen, Emma
title SID-3 Liquid and Ice Phase Particle Size Distributions measured during ACLOUD ...
title_short SID-3 Liquid and Ice Phase Particle Size Distributions measured during ACLOUD ...
title_full SID-3 Liquid and Ice Phase Particle Size Distributions measured during ACLOUD ...
title_fullStr SID-3 Liquid and Ice Phase Particle Size Distributions measured during ACLOUD ...
title_full_unstemmed SID-3 Liquid and Ice Phase Particle Size Distributions measured during ACLOUD ...
title_sort sid-3 liquid and ice phase particle size distributions measured during acloud ...
publisher PANGAEA
publishDate 2023
url https://dx.doi.org/10.1594/pangaea.960269
https://doi.pangaea.de/10.1594/PANGAEA.960269
genre Arctic
genre_facet Arctic
op_relation https://dx.doi.org/10.5194/acp-23-7611-2023
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_doi https://doi.org/10.1594/pangaea.96026910.5194/acp-23-7611-2023
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