Response of the Nevzorov hot wire probe in clouds dominated by droplet conditions in the drizzle size range

During the airborne research mission ASTAR 2004 (Arctic Study of Tropospheric Aerosols, Clouds and Radiation) performed over the island of Svalbard in the Arctic a constant-temperature hot-wire Nevzorov Probe designed for aircraft measurements, has been used onboard the aircraft POLAR 2. The Nevzoro...

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Published in:Atmospheric Measurement Techniques
Main Authors: Schwarzenboeck, A., Mioche, G., Armetta, A., Herber, A., Gayet, J.-F.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/amt-2-779-2009
https://amt.copernicus.org/articles/2/779/2009/
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spelling ftcopernicus:oai:publications.copernicus.org:amt842 2023-05-15T14:57:42+02:00 Response of the Nevzorov hot wire probe in clouds dominated by droplet conditions in the drizzle size range Schwarzenboeck, A. Mioche, G. Armetta, A. Herber, A. Gayet, J.-F. 2018-01-15 application/pdf https://doi.org/10.5194/amt-2-779-2009 https://amt.copernicus.org/articles/2/779/2009/ eng eng doi:10.5194/amt-2-779-2009 https://amt.copernicus.org/articles/2/779/2009/ eISSN: 1867-8548 Text 2018 ftcopernicus https://doi.org/10.5194/amt-2-779-2009 2020-07-20T16:26:31Z During the airborne research mission ASTAR 2004 (Arctic Study of Tropospheric Aerosols, Clouds and Radiation) performed over the island of Svalbard in the Arctic a constant-temperature hot-wire Nevzorov Probe designed for aircraft measurements, has been used onboard the aircraft POLAR 2. The Nevzorov probe measured liquid water (LWC) and total condensed water content (TWC) in supercooled liquid and partly mixed phase clouds, respectively. As for other hotwire probes the calculation of LWC and/or TWC (and thus the ice water content IWC) has to take into account the collection efficiencies of the two separate sensors for LWC and TWC which both react differently with respect to cloud phase and what is even more difficult to quantify with respect to the size of ice and liquid cloud particles. The study demonstrates that during pure liquid cloud sequences the ASTAR data set of the Nevzorov probe allowed to improve the quantification of the collection efficiency, particularly of the LWC probe part with respect to water. The improved quantification of liquid water content should lead to improved retrievals of IWC content. Simultaneous retrievals of LWC and IWC are correlated with the asymmetry factor derived from the Polar Nephelometer instrument. Text Arctic Svalbard Copernicus Publications: E-Journals Arctic Svalbard Atmospheric Measurement Techniques 2 2 779 788
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description During the airborne research mission ASTAR 2004 (Arctic Study of Tropospheric Aerosols, Clouds and Radiation) performed over the island of Svalbard in the Arctic a constant-temperature hot-wire Nevzorov Probe designed for aircraft measurements, has been used onboard the aircraft POLAR 2. The Nevzorov probe measured liquid water (LWC) and total condensed water content (TWC) in supercooled liquid and partly mixed phase clouds, respectively. As for other hotwire probes the calculation of LWC and/or TWC (and thus the ice water content IWC) has to take into account the collection efficiencies of the two separate sensors for LWC and TWC which both react differently with respect to cloud phase and what is even more difficult to quantify with respect to the size of ice and liquid cloud particles. The study demonstrates that during pure liquid cloud sequences the ASTAR data set of the Nevzorov probe allowed to improve the quantification of the collection efficiency, particularly of the LWC probe part with respect to water. The improved quantification of liquid water content should lead to improved retrievals of IWC content. Simultaneous retrievals of LWC and IWC are correlated with the asymmetry factor derived from the Polar Nephelometer instrument.
format Text
author Schwarzenboeck, A.
Mioche, G.
Armetta, A.
Herber, A.
Gayet, J.-F.
spellingShingle Schwarzenboeck, A.
Mioche, G.
Armetta, A.
Herber, A.
Gayet, J.-F.
Response of the Nevzorov hot wire probe in clouds dominated by droplet conditions in the drizzle size range
author_facet Schwarzenboeck, A.
Mioche, G.
Armetta, A.
Herber, A.
Gayet, J.-F.
author_sort Schwarzenboeck, A.
title Response of the Nevzorov hot wire probe in clouds dominated by droplet conditions in the drizzle size range
title_short Response of the Nevzorov hot wire probe in clouds dominated by droplet conditions in the drizzle size range
title_full Response of the Nevzorov hot wire probe in clouds dominated by droplet conditions in the drizzle size range
title_fullStr Response of the Nevzorov hot wire probe in clouds dominated by droplet conditions in the drizzle size range
title_full_unstemmed Response of the Nevzorov hot wire probe in clouds dominated by droplet conditions in the drizzle size range
title_sort response of the nevzorov hot wire probe in clouds dominated by droplet conditions in the drizzle size range
publishDate 2018
url https://doi.org/10.5194/amt-2-779-2009
https://amt.copernicus.org/articles/2/779/2009/
geographic Arctic
Svalbard
geographic_facet Arctic
Svalbard
genre Arctic
Svalbard
genre_facet Arctic
Svalbard
op_source eISSN: 1867-8548
op_relation doi:10.5194/amt-2-779-2009
https://amt.copernicus.org/articles/2/779/2009/
op_doi https://doi.org/10.5194/amt-2-779-2009
container_title Atmospheric Measurement Techniques
container_volume 2
container_issue 2
container_start_page 779
op_container_end_page 788
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