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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Online Access: | https://dx.doi.org/10.1594/pangaea.960269 https://doi.pangaea.de/10.1594/PANGAEA.960269 |
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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 |
_version_ |
1786822537664004096 |