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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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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1766377679280406528 |