Sulfur isotopes of sulfate measurements from a Greenland ice core (1850-2006)

Anthropogenic sulfate aerosols are estimated to have offset sixty percent of greenhouse-gas-induced warming in the Arctic, a region warming four times faster than the rest of the world. However, sulfate radiative forcing estimates remain uncertain because the relative contributions from anthropogeni...

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Main Authors: Ursula Jongebloed, Becky Alexander, Jihong Cole-Dai, Andrew Schauer, Carleigh Larrick, Shohei Hattori, Sara Salimi, Shana Edouard, Lei Geng
Format: Dataset
Language:unknown
Published: Arctic Data Center 2023
Subjects:
Online Access:https://doi.org/10.18739/A26T0GX7K
id dataone:doi:10.18739/A26T0GX7K
record_format openpolar
spelling dataone:doi:10.18739/A26T0GX7K 2024-06-03T18:46:38+00:00 Sulfur isotopes of sulfate measurements from a Greenland ice core (1850-2006) Ursula Jongebloed Becky Alexander Jihong Cole-Dai Andrew Schauer Carleigh Larrick Shohei Hattori Sara Salimi Shana Edouard Lei Geng Summit, Greenland ENVELOPE(-38.62,-38.62,72.58,72.58) BEGINDATE: 1850-01-01T00:00:00Z ENDDATE: 2006-01-01T00:00:00Z 2023-05-11T00:00:00Z https://doi.org/10.18739/A26T0GX7K unknown Arctic Data Center ice core sulfur sulfate isotope anthropogenic pollution Dataset 2023 dataone:urn:node:ARCTIC https://doi.org/10.18739/A26T0GX7K 2024-06-03T18:19:30Z Anthropogenic sulfate aerosols are estimated to have offset sixty percent of greenhouse-gas-induced warming in the Arctic, a region warming four times faster than the rest of the world. However, sulfate radiative forcing estimates remain uncertain because the relative contributions from anthropogenic versus natural sources to total sulfate aerosols are unknown. Here we measure sulfur isotopes of sulfate in a Summit, Greenland ice core from 1850 to 2006 CE to quantify the contribution of anthropogenic sulfur emissions to ice core sulfate. We use a Keeling Plot to determine the anthropogenic sulfur isotopic signature (δ34Santhro = +2.9  0.3 ‰), and compare this result to a compilation of sulfur isotope measurements of oil and coal. Using δ34Santhro, we quantify anthropogenic sulfate concentration separated from natural sulfate. Anthropogenic sulfate concentration increases to 68 ± 7% of non-sea-salt sulfate (65.1 ± 20.2 µg kg-1) during peak anthropogenic emissions from 1960 to 1990 and decreases to 45 ± 11% of non-sea-salt sulfate (25.4 ± 12.8 µg kg-1) from 1996 to 2006. These observations provide the first long-term record of anthropogenic sulfate distinguished from natural sources (e.g., volcanoes, dimethyl sulfide), and can be used to evaluate model characterization of anthropogenic sulfate aerosol fraction and radiative forcing over the industrial era. These data include sulfur isotopes of sulfate measurements from a Greenland ice core from 1850-2006. The preindustrial dataset (1200-1850) is uploaded to the Arctic data center here: doi:10.18739/A2N873162 Dataset Arctic Greenland Greenland ice core ice core Arctic Data Center (via DataONE) Arctic Greenland ENVELOPE(-38.62,-38.62,72.58,72.58)
institution Open Polar
collection Arctic Data Center (via DataONE)
op_collection_id dataone:urn:node:ARCTIC
language unknown
topic ice core
sulfur
sulfate
isotope
anthropogenic
pollution
spellingShingle ice core
sulfur
sulfate
isotope
anthropogenic
pollution
Ursula Jongebloed
Becky Alexander
Jihong Cole-Dai
Andrew Schauer
Carleigh Larrick
Shohei Hattori
Sara Salimi
Shana Edouard
Lei Geng
Sulfur isotopes of sulfate measurements from a Greenland ice core (1850-2006)
topic_facet ice core
sulfur
sulfate
isotope
anthropogenic
pollution
description Anthropogenic sulfate aerosols are estimated to have offset sixty percent of greenhouse-gas-induced warming in the Arctic, a region warming four times faster than the rest of the world. However, sulfate radiative forcing estimates remain uncertain because the relative contributions from anthropogenic versus natural sources to total sulfate aerosols are unknown. Here we measure sulfur isotopes of sulfate in a Summit, Greenland ice core from 1850 to 2006 CE to quantify the contribution of anthropogenic sulfur emissions to ice core sulfate. We use a Keeling Plot to determine the anthropogenic sulfur isotopic signature (δ34Santhro = +2.9  0.3 ‰), and compare this result to a compilation of sulfur isotope measurements of oil and coal. Using δ34Santhro, we quantify anthropogenic sulfate concentration separated from natural sulfate. Anthropogenic sulfate concentration increases to 68 ± 7% of non-sea-salt sulfate (65.1 ± 20.2 µg kg-1) during peak anthropogenic emissions from 1960 to 1990 and decreases to 45 ± 11% of non-sea-salt sulfate (25.4 ± 12.8 µg kg-1) from 1996 to 2006. These observations provide the first long-term record of anthropogenic sulfate distinguished from natural sources (e.g., volcanoes, dimethyl sulfide), and can be used to evaluate model characterization of anthropogenic sulfate aerosol fraction and radiative forcing over the industrial era. These data include sulfur isotopes of sulfate measurements from a Greenland ice core from 1850-2006. The preindustrial dataset (1200-1850) is uploaded to the Arctic data center here: doi:10.18739/A2N873162
format Dataset
author Ursula Jongebloed
Becky Alexander
Jihong Cole-Dai
Andrew Schauer
Carleigh Larrick
Shohei Hattori
Sara Salimi
Shana Edouard
Lei Geng
author_facet Ursula Jongebloed
Becky Alexander
Jihong Cole-Dai
Andrew Schauer
Carleigh Larrick
Shohei Hattori
Sara Salimi
Shana Edouard
Lei Geng
author_sort Ursula Jongebloed
title Sulfur isotopes of sulfate measurements from a Greenland ice core (1850-2006)
title_short Sulfur isotopes of sulfate measurements from a Greenland ice core (1850-2006)
title_full Sulfur isotopes of sulfate measurements from a Greenland ice core (1850-2006)
title_fullStr Sulfur isotopes of sulfate measurements from a Greenland ice core (1850-2006)
title_full_unstemmed Sulfur isotopes of sulfate measurements from a Greenland ice core (1850-2006)
title_sort sulfur isotopes of sulfate measurements from a greenland ice core (1850-2006)
publisher Arctic Data Center
publishDate 2023
url https://doi.org/10.18739/A26T0GX7K
op_coverage Summit, Greenland
ENVELOPE(-38.62,-38.62,72.58,72.58)
BEGINDATE: 1850-01-01T00:00:00Z ENDDATE: 2006-01-01T00:00:00Z
long_lat ENVELOPE(-38.62,-38.62,72.58,72.58)
geographic Arctic
Greenland
geographic_facet Arctic
Greenland
genre Arctic
Greenland
Greenland ice core
ice core
genre_facet Arctic
Greenland
Greenland ice core
ice core
op_doi https://doi.org/10.18739/A26T0GX7K
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