Difference of INP between heated and non-heated samples in the freezing assay measured at the Eastern North Atlantic observatory in autumn 2020

The dataset herein shows median change in ice-nucleating particle concentration after heating for the data from Eastern North Atlantic (ENA). The changes in absolute ice-nucleating particle concentration and percentage for ∆T of 0.5 °C are shown. The uncertainties are ± 0.5 °C with ± 23.5% for tempe...

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Bibliographic Details
Main Authors: Wilbourn, Elise, Hiranuma, Naruki
Format: Dataset
Language:English
Published: PANGAEA 2023
Subjects:
Calculated
Change
cloud
delta
DOE-ARM-ENA
Eastern North Atlantic
Freezing
ice
Ice Nucleating Particle
Ice nucleating particles
per air volume
Monitoring station
MONS
Temperature
technical
North Atlantic
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.964052
https://doi.org/10.1594/PANGAEA.964052
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.964052
record_format openpolar
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.964052 2024-10-06T13:50:56+00:00 Difference of INP between heated and non-heated samples in the freezing assay measured at the Eastern North Atlantic observatory in autumn 2020 Wilbourn, Elise Hiranuma, Naruki LATITUDE: 39.091600 * LONGITUDE: -28.025700 * MINIMUM ELEVATION: 31.0 m * MAXIMUM ELEVATION: 31.0 m 2023 text/tab-separated-values, 120 data points https://doi.pangaea.de/10.1594/PANGAEA.964052 https://doi.org/10.1594/PANGAEA.964052 en eng PANGAEA https://doi.org/10.1594/PANGAEA.964038 https://doi.pangaea.de/10.1594/PANGAEA.964052 https://doi.org/10.1594/PANGAEA.964052 CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess Calculated Change cloud delta DOE-ARM-ENA Eastern North Atlantic Freezing ice Ice Nucleating Particle Ice nucleating particles per air volume Monitoring station MONS Temperature technical dataset 2023 ftpangaea https://doi.org/10.1594/PANGAEA.96405210.1594/PANGAEA.964038 2024-09-11T00:15:19Z The dataset herein shows median change in ice-nucleating particle concentration after heating for the data from Eastern North Atlantic (ENA). The changes in absolute ice-nucleating particle concentration and percentage for ∆T of 0.5 °C are shown. The uncertainties are ± 0.5 °C with ± 23.5% for temperature and ice-nucleating particle concentration. Note: The 100% ice-nucleating particle concentration loss is not displayed. Dataset North Atlantic PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(-28.025700,-28.025700,39.091600,39.091600)
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic Calculated
Change
cloud
delta
DOE-ARM-ENA
Eastern North Atlantic
Freezing
ice
Ice Nucleating Particle
Ice nucleating particles
per air volume
Monitoring station
MONS
Temperature
technical
spellingShingle Calculated
Change
cloud
delta
DOE-ARM-ENA
Eastern North Atlantic
Freezing
ice
Ice Nucleating Particle
Ice nucleating particles
per air volume
Monitoring station
MONS
Temperature
technical
Wilbourn, Elise
Hiranuma, Naruki
Difference of INP between heated and non-heated samples in the freezing assay measured at the Eastern North Atlantic observatory in autumn 2020
topic_facet Calculated
Change
cloud
delta
DOE-ARM-ENA
Eastern North Atlantic
Freezing
ice
Ice Nucleating Particle
Ice nucleating particles
per air volume
Monitoring station
MONS
Temperature
technical
description The dataset herein shows median change in ice-nucleating particle concentration after heating for the data from Eastern North Atlantic (ENA). The changes in absolute ice-nucleating particle concentration and percentage for ∆T of 0.5 °C are shown. The uncertainties are ± 0.5 °C with ± 23.5% for temperature and ice-nucleating particle concentration. Note: The 100% ice-nucleating particle concentration loss is not displayed.
format Dataset
author Wilbourn, Elise
Hiranuma, Naruki
author_facet Wilbourn, Elise
Hiranuma, Naruki
author_sort Wilbourn, Elise
title Difference of INP between heated and non-heated samples in the freezing assay measured at the Eastern North Atlantic observatory in autumn 2020
title_short Difference of INP between heated and non-heated samples in the freezing assay measured at the Eastern North Atlantic observatory in autumn 2020
title_full Difference of INP between heated and non-heated samples in the freezing assay measured at the Eastern North Atlantic observatory in autumn 2020
title_fullStr Difference of INP between heated and non-heated samples in the freezing assay measured at the Eastern North Atlantic observatory in autumn 2020
title_full_unstemmed Difference of INP between heated and non-heated samples in the freezing assay measured at the Eastern North Atlantic observatory in autumn 2020
title_sort difference of inp between heated and non-heated samples in the freezing assay measured at the eastern north atlantic observatory in autumn 2020
publisher PANGAEA
publishDate 2023
url https://doi.pangaea.de/10.1594/PANGAEA.964052
https://doi.org/10.1594/PANGAEA.964052
op_coverage LATITUDE: 39.091600 * LONGITUDE: -28.025700 * MINIMUM ELEVATION: 31.0 m * MAXIMUM ELEVATION: 31.0 m
long_lat ENVELOPE(-28.025700,-28.025700,39.091600,39.091600)
genre North Atlantic
genre_facet North Atlantic
op_relation https://doi.org/10.1594/PANGAEA.964038
https://doi.pangaea.de/10.1594/PANGAEA.964052
https://doi.org/10.1594/PANGAEA.964052
op_rights CC-BY-4.0: Creative Commons Attribution 4.0 International
Access constraints: unrestricted
info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.1594/PANGAEA.96405210.1594/PANGAEA.964038
_version_ 1812179075062562816

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