Short-Term Meteorological and Environmental Signals Recorded in a Firn Core from a High-Accumulation Site on Plateau Laclavere, Antarctic Peninsula

High-accumulation sites are crucial for understanding the patterns and mechanisms of climate and environmental change in Antarctica since they allow gaining high-resolution proxy records from firn and ice. Here, we present new glacio- and isotope-geochemical data at sub-annual resolution from a firn...

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Published in:Geosciences
Main Authors: Kirstin Hoffmann-Abdi, Francisco Fernandoy, Hanno Meyer, Johannes Freitag, Thomas Opel, Joseph R. McConnell, Christoph Schneider
Format: Article in Journal/Newspaper
Language:English
Published: MDPI AG 2021
Subjects:
Online Access:https://doi.org/10.3390/geosciences11100428
https://doaj.org/article/ce96a0c3f0d44a93b0c3f470d485ea13
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spelling ftdoajarticles:oai:doaj.org/article:ce96a0c3f0d44a93b0c3f470d485ea13 2023-05-15T13:24:09+02:00 Short-Term Meteorological and Environmental Signals Recorded in a Firn Core from a High-Accumulation Site on Plateau Laclavere, Antarctic Peninsula Kirstin Hoffmann-Abdi Francisco Fernandoy Hanno Meyer Johannes Freitag Thomas Opel Joseph R. McConnell Christoph Schneider 2021-10-01T00:00:00Z https://doi.org/10.3390/geosciences11100428 https://doaj.org/article/ce96a0c3f0d44a93b0c3f470d485ea13 EN eng MDPI AG https://www.mdpi.com/2076-3263/11/10/428 https://doaj.org/toc/2076-3263 doi:10.3390/geosciences11100428 2076-3263 https://doaj.org/article/ce96a0c3f0d44a93b0c3f470d485ea13 Geosciences, Vol 11, Iss 428, p 428 (2021) Antarctic Peninsula firn cores stable water isotopes glacio-chemistry high accumulation surface melt Geology QE1-996.5 article 2021 ftdoajarticles https://doi.org/10.3390/geosciences11100428 2022-12-31T12:49:34Z High-accumulation sites are crucial for understanding the patterns and mechanisms of climate and environmental change in Antarctica since they allow gaining high-resolution proxy records from firn and ice. Here, we present new glacio- and isotope-geochemical data at sub-annual resolution from a firn core retrieved from an ice cap on Plateau Laclavere (LCL), northern Antarctic Peninsula, covering the period 2012–2015. The signals of two volcanic eruptions and two forest fire events in South America could be identified in the non-sea-salt sulphur and black carbon records, respectively. Mean annual snow accumulation on LCL amounts to 2500 kg m −2 a −1 and exhibits low inter-annual variability. Time series of δ 18 O, δD and d excess show no seasonal cyclicity, which may result from (1) a reduced annual temperature amplitude due to the maritime climate and (2) post-depositional processes. The firn core stratigraphy indicates strong surface melt on LCL during austral summers 2013 and 2015, likely related to large-scale warm-air advection from lower latitudes and temporal variations in sea ice extent in the Bellingshausen-Amundsen Sea. The LCL ice cap is a highly valuable natural archive since it captures regional meteorological and environmental signals as well as their connection to the South American continent. Article in Journal/Newspaper Amundsen Sea Antarc* Antarctic Antarctic Peninsula Antarctica Ice cap Sea ice Directory of Open Access Journals: DOAJ Articles Antarctic Antarctic Peninsula Austral Amundsen Sea Geosciences 11 10 428
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Antarctic Peninsula
firn cores
stable water isotopes
glacio-chemistry
high accumulation
surface melt
Geology
QE1-996.5
spellingShingle Antarctic Peninsula
firn cores
stable water isotopes
glacio-chemistry
high accumulation
surface melt
Geology
QE1-996.5
Kirstin Hoffmann-Abdi
Francisco Fernandoy
Hanno Meyer
Johannes Freitag
Thomas Opel
Joseph R. McConnell
Christoph Schneider
Short-Term Meteorological and Environmental Signals Recorded in a Firn Core from a High-Accumulation Site on Plateau Laclavere, Antarctic Peninsula
topic_facet Antarctic Peninsula
firn cores
stable water isotopes
glacio-chemistry
high accumulation
surface melt
Geology
QE1-996.5
description High-accumulation sites are crucial for understanding the patterns and mechanisms of climate and environmental change in Antarctica since they allow gaining high-resolution proxy records from firn and ice. Here, we present new glacio- and isotope-geochemical data at sub-annual resolution from a firn core retrieved from an ice cap on Plateau Laclavere (LCL), northern Antarctic Peninsula, covering the period 2012–2015. The signals of two volcanic eruptions and two forest fire events in South America could be identified in the non-sea-salt sulphur and black carbon records, respectively. Mean annual snow accumulation on LCL amounts to 2500 kg m −2 a −1 and exhibits low inter-annual variability. Time series of δ 18 O, δD and d excess show no seasonal cyclicity, which may result from (1) a reduced annual temperature amplitude due to the maritime climate and (2) post-depositional processes. The firn core stratigraphy indicates strong surface melt on LCL during austral summers 2013 and 2015, likely related to large-scale warm-air advection from lower latitudes and temporal variations in sea ice extent in the Bellingshausen-Amundsen Sea. The LCL ice cap is a highly valuable natural archive since it captures regional meteorological and environmental signals as well as their connection to the South American continent.
format Article in Journal/Newspaper
author Kirstin Hoffmann-Abdi
Francisco Fernandoy
Hanno Meyer
Johannes Freitag
Thomas Opel
Joseph R. McConnell
Christoph Schneider
author_facet Kirstin Hoffmann-Abdi
Francisco Fernandoy
Hanno Meyer
Johannes Freitag
Thomas Opel
Joseph R. McConnell
Christoph Schneider
author_sort Kirstin Hoffmann-Abdi
title Short-Term Meteorological and Environmental Signals Recorded in a Firn Core from a High-Accumulation Site on Plateau Laclavere, Antarctic Peninsula
title_short Short-Term Meteorological and Environmental Signals Recorded in a Firn Core from a High-Accumulation Site on Plateau Laclavere, Antarctic Peninsula
title_full Short-Term Meteorological and Environmental Signals Recorded in a Firn Core from a High-Accumulation Site on Plateau Laclavere, Antarctic Peninsula
title_fullStr Short-Term Meteorological and Environmental Signals Recorded in a Firn Core from a High-Accumulation Site on Plateau Laclavere, Antarctic Peninsula
title_full_unstemmed Short-Term Meteorological and Environmental Signals Recorded in a Firn Core from a High-Accumulation Site on Plateau Laclavere, Antarctic Peninsula
title_sort short-term meteorological and environmental signals recorded in a firn core from a high-accumulation site on plateau laclavere, antarctic peninsula
publisher MDPI AG
publishDate 2021
url https://doi.org/10.3390/geosciences11100428
https://doaj.org/article/ce96a0c3f0d44a93b0c3f470d485ea13
geographic Antarctic
Antarctic Peninsula
Austral
Amundsen Sea
geographic_facet Antarctic
Antarctic Peninsula
Austral
Amundsen Sea
genre Amundsen Sea
Antarc*
Antarctic
Antarctic Peninsula
Antarctica
Ice cap
Sea ice
genre_facet Amundsen Sea
Antarc*
Antarctic
Antarctic Peninsula
Antarctica
Ice cap
Sea ice
op_source Geosciences, Vol 11, Iss 428, p 428 (2021)
op_relation https://www.mdpi.com/2076-3263/11/10/428
https://doaj.org/toc/2076-3263
doi:10.3390/geosciences11100428
2076-3263
https://doaj.org/article/ce96a0c3f0d44a93b0c3f470d485ea13
op_doi https://doi.org/10.3390/geosciences11100428
container_title Geosciences
container_volume 11
container_issue 10
container_start_page 428
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