ARCtic Study of Permafrost Ice Nucleation (ARCSPIN) Cumulative Ice Nucleating Particles (INP) Data, Alaska, 2021

We proposed to analyze samples for ice nucleating particles (INPs) and microbial composition through a land-based field study, and to eventually simulate observations in an Earth System model. Our overarching hypothesis is that INPs released from thawing permafrost—a hitherto overlooked source of IN...

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Main Author: Kevin Barry
Format: Dataset
Language:unknown
Published: Arctic Data Center 2023
Subjects:
Ice
Online Access:https://doi.org/10.18739/A2833N072
id dataone:doi:10.18739/A2833N072
record_format openpolar
spelling dataone:doi:10.18739/A2833N072 2024-06-03T18:46:34+00:00 ARCtic Study of Permafrost Ice Nucleation (ARCSPIN) Cumulative Ice Nucleating Particles (INP) Data, Alaska, 2021 Kevin Barry Utqiaġvik, Alaska and surrounding area ENVELOPE(-157.06609,-155.85379,71.38535,71.15311) BEGINDATE: 2021-08-21T00:00:00Z ENDDATE: 2021-09-17T00:00:00Z 2023-01-01T00:00:00Z https://doi.org/10.18739/A2833N072 unknown Arctic Data Center Dataset 2023 dataone:urn:node:ARCTIC https://doi.org/10.18739/A2833N072 2024-06-03T18:20:17Z We proposed to analyze samples for ice nucleating particles (INPs) and microbial composition through a land-based field study, and to eventually simulate observations in an Earth System model. Our overarching hypothesis is that INPs released from thawing permafrost—a hitherto overlooked source of INPs—significantly influence cloud radiative properties in the Arctic. The primary field deployment called ARCSPIN (ARCtic Study of Permafrost Ice Nucleation) was conducted from September 1-17, 2021, within and near Utqiaġvik, Alaska. Permafrost, seasonally thawed active layer, ice wedge, vegetation, water, and aerosol samples were collected. Samples targeted downwind of thermokarst lakes, with some days that collected measurements upwind as well. We also include aerosol filters collected at a fixed site at the Department of Energy Atmospheric Radiation Measurement North Slope of Alaska atmospheric observatory (DOE). Here, we provide the INP-temperature spectra along with 95% confidence interval widths, which follow Agresti and Coull (1998). All samples were processed with the Colorado State University (CSU) Ice Spectrometer (IS), most recently described in Creamean et al. (2022). Agresti, A. and Coull, B. A. (1998). Approximate is better than “exact” for interval estimation of binomial proportions. The American Statistician, 52, 119–126. https://doi.org/10.2307/2685469 Creamean, J.M., Hill, T.C.J., and Hume, C. (2022). Ice Nucleation Spectrometer (INS) Instrument Handbook(DOE/SC-ARM-TR-278, 1846263; p. DOE/SC-ARM-TR-278, 1846263), OSTI.GOV, https://doi.org/10.2172/1846263 Dataset Arctic Ice north slope permafrost Thermokarst wedge* Alaska Arctic Data Center (via DataONE) Arctic ENVELOPE(-157.06609,-155.85379,71.38535,71.15311)
institution Open Polar
collection Arctic Data Center (via DataONE)
op_collection_id dataone:urn:node:ARCTIC
language unknown
description We proposed to analyze samples for ice nucleating particles (INPs) and microbial composition through a land-based field study, and to eventually simulate observations in an Earth System model. Our overarching hypothesis is that INPs released from thawing permafrost—a hitherto overlooked source of INPs—significantly influence cloud radiative properties in the Arctic. The primary field deployment called ARCSPIN (ARCtic Study of Permafrost Ice Nucleation) was conducted from September 1-17, 2021, within and near Utqiaġvik, Alaska. Permafrost, seasonally thawed active layer, ice wedge, vegetation, water, and aerosol samples were collected. Samples targeted downwind of thermokarst lakes, with some days that collected measurements upwind as well. We also include aerosol filters collected at a fixed site at the Department of Energy Atmospheric Radiation Measurement North Slope of Alaska atmospheric observatory (DOE). Here, we provide the INP-temperature spectra along with 95% confidence interval widths, which follow Agresti and Coull (1998). All samples were processed with the Colorado State University (CSU) Ice Spectrometer (IS), most recently described in Creamean et al. (2022). Agresti, A. and Coull, B. A. (1998). Approximate is better than “exact” for interval estimation of binomial proportions. The American Statistician, 52, 119–126. https://doi.org/10.2307/2685469 Creamean, J.M., Hill, T.C.J., and Hume, C. (2022). Ice Nucleation Spectrometer (INS) Instrument Handbook(DOE/SC-ARM-TR-278, 1846263; p. DOE/SC-ARM-TR-278, 1846263), OSTI.GOV, https://doi.org/10.2172/1846263
format Dataset
author Kevin Barry
spellingShingle Kevin Barry
ARCtic Study of Permafrost Ice Nucleation (ARCSPIN) Cumulative Ice Nucleating Particles (INP) Data, Alaska, 2021
author_facet Kevin Barry
author_sort Kevin Barry
title ARCtic Study of Permafrost Ice Nucleation (ARCSPIN) Cumulative Ice Nucleating Particles (INP) Data, Alaska, 2021
title_short ARCtic Study of Permafrost Ice Nucleation (ARCSPIN) Cumulative Ice Nucleating Particles (INP) Data, Alaska, 2021
title_full ARCtic Study of Permafrost Ice Nucleation (ARCSPIN) Cumulative Ice Nucleating Particles (INP) Data, Alaska, 2021
title_fullStr ARCtic Study of Permafrost Ice Nucleation (ARCSPIN) Cumulative Ice Nucleating Particles (INP) Data, Alaska, 2021
title_full_unstemmed ARCtic Study of Permafrost Ice Nucleation (ARCSPIN) Cumulative Ice Nucleating Particles (INP) Data, Alaska, 2021
title_sort arctic study of permafrost ice nucleation (arcspin) cumulative ice nucleating particles (inp) data, alaska, 2021
publisher Arctic Data Center
publishDate 2023
url https://doi.org/10.18739/A2833N072
op_coverage Utqiaġvik, Alaska and surrounding area
ENVELOPE(-157.06609,-155.85379,71.38535,71.15311)
BEGINDATE: 2021-08-21T00:00:00Z ENDDATE: 2021-09-17T00:00:00Z
long_lat ENVELOPE(-157.06609,-155.85379,71.38535,71.15311)
geographic Arctic
geographic_facet Arctic
genre Arctic
Ice
north slope
permafrost
Thermokarst
wedge*
Alaska
genre_facet Arctic
Ice
north slope
permafrost
Thermokarst
wedge*
Alaska
op_doi https://doi.org/10.18739/A2833N072
_version_ 1800868024138334208