High-resolution hydrogen peroxide data of firn core OH-12 from Plateau Laclavere, northern Antarctic Peninsula

The firn core OH-12 was retrieved from Plateau Laclavere, a small ice cap on the northernmost end of the Antarctic Peninsula at about 1090 m above sea level in January 2016. The core was drilled down to 19.93 m depth. Subsamples for stable water isotope analysis were obtained from the core at 5 cm r...

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Main Authors: Hoffmann-Abdi, Kirstin, Fernandoy, Francisco, Meyer, Hanno, Freitag, Johannes, Opel, Thomas, McConnell, Joseph R, Schneider, Christoph
Format: Dataset
Language:English
Published: PANGAEA 2021
Subjects:
Age
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.939717
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.939717
record_format openpolar
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.939717 2023-05-15T13:40:11+02:00 High-resolution hydrogen peroxide data of firn core OH-12 from Plateau Laclavere, northern Antarctic Peninsula Hoffmann-Abdi, Kirstin Fernandoy, Francisco Meyer, Hanno Freitag, Johannes Opel, Thomas McConnell, Joseph R Schneider, Christoph LATITUDE: -63.456970 * LONGITUDE: -57.754176 * DATE/TIME START: 2016-01-15T00:00:00 * DATE/TIME END: 2016-01-15T00:00:00 * MINIMUM DEPTH, ice/snow: 0.03 m * MAXIMUM DEPTH, ice/snow: 19.88 m 2021-12-20 text/tab-separated-values, 25975 data points https://doi.pangaea.de/10.1594/PANGAEA.939717 en eng PANGAEA https://doi.org/10.1594/PANGAEA.939719 Hoffmann-Abdi, Kirstin; Fernandoy, Francisco; Meyer, Hanno; Freitag, Johannes; Opel, Thomas; McConnell, Joseph R; Schneider, Christoph (2021): Short-Term Meteorological and Environmental Signals Recorded in a Firn Core from a High-Accumulation Site on Plateau Laclavere, Antarctic Peninsula. Geosciences, 11(10), 428, https://doi.org/10.3390/geosciences11100428 McConnell, Joseph R; Edwards, Ross; Kok, Gregory L; Flanner, Mark G; Zender, Charles S; Saltzman, Eric S; Banta, J Ryan; Pasteris, Daniel R; Carter, Megan M; Kahl, Jonathan D W (2007): 20th-Century Industrial Black Carbon Emissions Altered Arctic Climate Forcing. Science, 317(5843), 1381-1384, https://doi.org/10.1126/science.1144856 McConnell, Joseph R; Lamorey, Gregg W; Lambert, Steven W; Taylor, Kendrick C (2002): Continuous Ice-Core Chemical Analyses Using Inductively Coupled Plasma Mass Spectrometry. Environmental Science & Technology, 36(1), 7-11, https://doi.org/10.1021/es011088z Röthlisberger, Regine; Bigler, Matthias; Hutterli, Manuel A; Sommer, Stefan; Stauffer, Bernhard; Junghans, Hans G; Wagenbach, Dietmar (2000): Technique for Continuous High-Resolution Analysis of Trace Substances in Firn and Ice Cores. Environmental Science & Technology, 34(2), 338-342, https://doi.org/10.1021/es9907055 https://doi.pangaea.de/10.1594/PANGAEA.939717 Access constraints: access rights needed info:eu-repo/semantics/restrictedAccess Age Antarctic Peninsula ANT-Land_2016_AntarcticPeninsula API2016 AWI_Envi AWI Antarctic Land Expedition DEPTH ice/snow firn core glacio-chemistry Hydrogen peroxide water ICEDRILL Ice drill OH-12 Polar Terrestrial Environmental Systems @ AWI Sample ID stable water isotopes Dataset 2021 ftpangaea https://doi.org/10.1594/PANGAEA.939719 https://doi.org/10.3390/geosciences11100428 https://doi.org/10.1126/science.1144856 2022-12-22T21:54:47Z The firn core OH-12 was retrieved from Plateau Laclavere, a small ice cap on the northernmost end of the Antarctic Peninsula at about 1090 m above sea level in January 2016. The core was drilled down to 19.93 m depth. Subsamples for stable water isotope analysis were obtained from the core at 5 cm resolution. Glacio-chemical parameters (hydrogen peroxide, sulphur, sodium, black carbon) were determined in summer 2017 using a Continuous Flow Analysis (CFA) system as described by Röthlisberger et al. (2000) and McConnell et al. (2002, 2007). The core was dated using annual layer counting of hydrogen peroxide measurements. We additionally accounted for precipitation intermittency at the drill site by using precipitation data from the European Centre for Medium-Range Weather Forecasts (ECMWF) ERA5 Reanalysis extracted from the grid point closest to the firn-core drill site. The core covers the period from July 2011 to January 2016. The data has been used for investigating recent climate and environmental changes in the northern Antarctic Peninsula region providing the basis for the retrieval and analysis of a deeper ice core from the same site. Dataset Antarc* Antarctic Antarctic Peninsula Arctic Ice cap ice core PANGAEA - Data Publisher for Earth & Environmental Science Antarctic Antarctic Peninsula The Antarctic ENVELOPE(-57.754176,-57.754176,-63.456970,-63.456970)
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic Age
Antarctic Peninsula
ANT-Land_2016_AntarcticPeninsula
API2016
AWI_Envi
AWI Antarctic Land Expedition
DEPTH
ice/snow
firn core
glacio-chemistry
Hydrogen peroxide
water
ICEDRILL
Ice drill
OH-12
Polar Terrestrial Environmental Systems @ AWI
Sample ID
stable water isotopes
spellingShingle Age
Antarctic Peninsula
ANT-Land_2016_AntarcticPeninsula
API2016
AWI_Envi
AWI Antarctic Land Expedition
DEPTH
ice/snow
firn core
glacio-chemistry
Hydrogen peroxide
water
ICEDRILL
Ice drill
OH-12
Polar Terrestrial Environmental Systems @ AWI
Sample ID
stable water isotopes
Hoffmann-Abdi, Kirstin
Fernandoy, Francisco
Meyer, Hanno
Freitag, Johannes
Opel, Thomas
McConnell, Joseph R
Schneider, Christoph
High-resolution hydrogen peroxide data of firn core OH-12 from Plateau Laclavere, northern Antarctic Peninsula
topic_facet Age
Antarctic Peninsula
ANT-Land_2016_AntarcticPeninsula
API2016
AWI_Envi
AWI Antarctic Land Expedition
DEPTH
ice/snow
firn core
glacio-chemistry
Hydrogen peroxide
water
ICEDRILL
Ice drill
OH-12
Polar Terrestrial Environmental Systems @ AWI
Sample ID
stable water isotopes
description The firn core OH-12 was retrieved from Plateau Laclavere, a small ice cap on the northernmost end of the Antarctic Peninsula at about 1090 m above sea level in January 2016. The core was drilled down to 19.93 m depth. Subsamples for stable water isotope analysis were obtained from the core at 5 cm resolution. Glacio-chemical parameters (hydrogen peroxide, sulphur, sodium, black carbon) were determined in summer 2017 using a Continuous Flow Analysis (CFA) system as described by Röthlisberger et al. (2000) and McConnell et al. (2002, 2007). The core was dated using annual layer counting of hydrogen peroxide measurements. We additionally accounted for precipitation intermittency at the drill site by using precipitation data from the European Centre for Medium-Range Weather Forecasts (ECMWF) ERA5 Reanalysis extracted from the grid point closest to the firn-core drill site. The core covers the period from July 2011 to January 2016. The data has been used for investigating recent climate and environmental changes in the northern Antarctic Peninsula region providing the basis for the retrieval and analysis of a deeper ice core from the same site.
format Dataset
author Hoffmann-Abdi, Kirstin
Fernandoy, Francisco
Meyer, Hanno
Freitag, Johannes
Opel, Thomas
McConnell, Joseph R
Schneider, Christoph
author_facet Hoffmann-Abdi, Kirstin
Fernandoy, Francisco
Meyer, Hanno
Freitag, Johannes
Opel, Thomas
McConnell, Joseph R
Schneider, Christoph
author_sort Hoffmann-Abdi, Kirstin
title High-resolution hydrogen peroxide data of firn core OH-12 from Plateau Laclavere, northern Antarctic Peninsula
title_short High-resolution hydrogen peroxide data of firn core OH-12 from Plateau Laclavere, northern Antarctic Peninsula
title_full High-resolution hydrogen peroxide data of firn core OH-12 from Plateau Laclavere, northern Antarctic Peninsula
title_fullStr High-resolution hydrogen peroxide data of firn core OH-12 from Plateau Laclavere, northern Antarctic Peninsula
title_full_unstemmed High-resolution hydrogen peroxide data of firn core OH-12 from Plateau Laclavere, northern Antarctic Peninsula
title_sort high-resolution hydrogen peroxide data of firn core oh-12 from plateau laclavere, northern antarctic peninsula
publisher PANGAEA
publishDate 2021
url https://doi.pangaea.de/10.1594/PANGAEA.939717
op_coverage LATITUDE: -63.456970 * LONGITUDE: -57.754176 * DATE/TIME START: 2016-01-15T00:00:00 * DATE/TIME END: 2016-01-15T00:00:00 * MINIMUM DEPTH, ice/snow: 0.03 m * MAXIMUM DEPTH, ice/snow: 19.88 m
long_lat ENVELOPE(-57.754176,-57.754176,-63.456970,-63.456970)
geographic Antarctic
Antarctic Peninsula
The Antarctic
geographic_facet Antarctic
Antarctic Peninsula
The Antarctic
genre Antarc*
Antarctic
Antarctic Peninsula
Arctic
Ice cap
ice core
genre_facet Antarc*
Antarctic
Antarctic Peninsula
Arctic
Ice cap
ice core
op_relation https://doi.org/10.1594/PANGAEA.939719
Hoffmann-Abdi, Kirstin; Fernandoy, Francisco; Meyer, Hanno; Freitag, Johannes; Opel, Thomas; McConnell, Joseph R; Schneider, Christoph (2021): Short-Term Meteorological and Environmental Signals Recorded in a Firn Core from a High-Accumulation Site on Plateau Laclavere, Antarctic Peninsula. Geosciences, 11(10), 428, https://doi.org/10.3390/geosciences11100428
McConnell, Joseph R; Edwards, Ross; Kok, Gregory L; Flanner, Mark G; Zender, Charles S; Saltzman, Eric S; Banta, J Ryan; Pasteris, Daniel R; Carter, Megan M; Kahl, Jonathan D W (2007): 20th-Century Industrial Black Carbon Emissions Altered Arctic Climate Forcing. Science, 317(5843), 1381-1384, https://doi.org/10.1126/science.1144856
McConnell, Joseph R; Lamorey, Gregg W; Lambert, Steven W; Taylor, Kendrick C (2002): Continuous Ice-Core Chemical Analyses Using Inductively Coupled Plasma Mass Spectrometry. Environmental Science & Technology, 36(1), 7-11, https://doi.org/10.1021/es011088z
Röthlisberger, Regine; Bigler, Matthias; Hutterli, Manuel A; Sommer, Stefan; Stauffer, Bernhard; Junghans, Hans G; Wagenbach, Dietmar (2000): Technique for Continuous High-Resolution Analysis of Trace Substances in Firn and Ice Cores. Environmental Science & Technology, 34(2), 338-342, https://doi.org/10.1021/es9907055
https://doi.pangaea.de/10.1594/PANGAEA.939717
op_rights Access constraints: access rights needed
info:eu-repo/semantics/restrictedAccess
op_doi https://doi.org/10.1594/PANGAEA.939719
https://doi.org/10.3390/geosciences11100428
https://doi.org/10.1126/science.1144856
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