Two-dimensional insights into the signal formation in low-accumulation firn-cores

Ice-cores have been proven to be a key climate archive to reconstruct glacial interglacial changes in temperature, greenhouse gases and many other climate parameters. By contrast, the reliability of ice-cores as a recorder of the Holocene climate evolution is less clear. The small amplitude of Holoc...

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Main Authors: Münch, Thomas, Freitag, Johannes, Meyer, Hanno, Kipfstuhl, Sepp, Laepple, Thomas
Format: Conference Object
Language:unknown
Published: 2014
Subjects:
Online Access:https://epic.awi.de/id/eprint/38307/
http://meetingorganizer.copernicus.org/EGU2014/EGU2014-12069.pdf
https://hdl.handle.net/10013/epic.45777
id ftawi:oai:epic.awi.de:38307
record_format openpolar
spelling ftawi:oai:epic.awi.de:38307 2023-05-15T13:40:27+02:00 Two-dimensional insights into the signal formation in low-accumulation firn-cores Münch, Thomas Freitag, Johannes Meyer, Hanno Kipfstuhl, Sepp Laepple, Thomas 2014 https://epic.awi.de/id/eprint/38307/ http://meetingorganizer.copernicus.org/EGU2014/EGU2014-12069.pdf https://hdl.handle.net/10013/epic.45777 unknown Münch, T. orcid:0000-0002-5492-7544 , Freitag, J. orcid:0000-0003-2654-9440 , Meyer, H. orcid:0000-0003-4129-4706 , Kipfstuhl, S. and Laepple, T. orcid:0000-0001-8108-7520 (2014) Two-dimensional insights into the signal formation in low-accumulation firn-cores , EGU General Assembly 2014, Vienna, Austria, 27 April 2014 - 2 May 2014 . hdl:10013/epic.45777 EPIC3EGU General Assembly 2014, Vienna, Austria, 2014-04-27-2014-05-02 Conference notRev 2014 ftawi 2021-12-24T15:40:34Z Ice-cores have been proven to be a key climate archive to reconstruct glacial interglacial changes in temperature, greenhouse gases and many other climate parameters. By contrast, the reliability of ice-cores as a recorder of the Holocene climate evolution is less clear. The small amplitude of Holocene climate changes, and the aim to reconstruct high-temporal resolution records, poses a challenge to the interpretation of ice-core signals. This is especially true for low accumulation sites as here the non-climate noise may often be too high to accurately extract a climatic signal. To develop a mechanistic understanding of the signal and noise in low-accumulation firn and ice cores, we undertook a study of the signal formation in firn and ice-cores at Kohnen station on Dronning Maud Land, Antarctica. This included extensive surface sampling, replicate coring of firn cores, and the analysis of water isotopes and the snow stratigraphy in snow pits and snow trenches. Thereby, we provide the basis for a systematic interpretation of the climate signal stored in ice at this site. In this contribution, we present first results from two 1m deep, 45m long snow trenches which were probed in two dimensions to provide a two-dimensional image of the dielectric properties and oxygen isotopes. The statistical analysis of the results provides insight about the horizontal and vertical scales of stratigraphic noise, the relation between the dielectric stratigraphy and the oxygen isotopes, and the ability of firn-cores to reconstruct high-resolution records of past climate changes. Conference Object Antarc* Antarctica Dronning Maud Land ice core Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) Dronning Maud Land Kohnen ENVELOPE(0.000,0.000,-75.000,-75.000) Kohnen Station ENVELOPE(0.000,0.000,-75.000,-75.000)
institution Open Polar
collection Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center)
op_collection_id ftawi
language unknown
description Ice-cores have been proven to be a key climate archive to reconstruct glacial interglacial changes in temperature, greenhouse gases and many other climate parameters. By contrast, the reliability of ice-cores as a recorder of the Holocene climate evolution is less clear. The small amplitude of Holocene climate changes, and the aim to reconstruct high-temporal resolution records, poses a challenge to the interpretation of ice-core signals. This is especially true for low accumulation sites as here the non-climate noise may often be too high to accurately extract a climatic signal. To develop a mechanistic understanding of the signal and noise in low-accumulation firn and ice cores, we undertook a study of the signal formation in firn and ice-cores at Kohnen station on Dronning Maud Land, Antarctica. This included extensive surface sampling, replicate coring of firn cores, and the analysis of water isotopes and the snow stratigraphy in snow pits and snow trenches. Thereby, we provide the basis for a systematic interpretation of the climate signal stored in ice at this site. In this contribution, we present first results from two 1m deep, 45m long snow trenches which were probed in two dimensions to provide a two-dimensional image of the dielectric properties and oxygen isotopes. The statistical analysis of the results provides insight about the horizontal and vertical scales of stratigraphic noise, the relation between the dielectric stratigraphy and the oxygen isotopes, and the ability of firn-cores to reconstruct high-resolution records of past climate changes.
format Conference Object
author Münch, Thomas
Freitag, Johannes
Meyer, Hanno
Kipfstuhl, Sepp
Laepple, Thomas
spellingShingle Münch, Thomas
Freitag, Johannes
Meyer, Hanno
Kipfstuhl, Sepp
Laepple, Thomas
Two-dimensional insights into the signal formation in low-accumulation firn-cores
author_facet Münch, Thomas
Freitag, Johannes
Meyer, Hanno
Kipfstuhl, Sepp
Laepple, Thomas
author_sort Münch, Thomas
title Two-dimensional insights into the signal formation in low-accumulation firn-cores
title_short Two-dimensional insights into the signal formation in low-accumulation firn-cores
title_full Two-dimensional insights into the signal formation in low-accumulation firn-cores
title_fullStr Two-dimensional insights into the signal formation in low-accumulation firn-cores
title_full_unstemmed Two-dimensional insights into the signal formation in low-accumulation firn-cores
title_sort two-dimensional insights into the signal formation in low-accumulation firn-cores
publishDate 2014
url https://epic.awi.de/id/eprint/38307/
http://meetingorganizer.copernicus.org/EGU2014/EGU2014-12069.pdf
https://hdl.handle.net/10013/epic.45777
long_lat ENVELOPE(0.000,0.000,-75.000,-75.000)
ENVELOPE(0.000,0.000,-75.000,-75.000)
geographic Dronning Maud Land
Kohnen
Kohnen Station
geographic_facet Dronning Maud Land
Kohnen
Kohnen Station
genre Antarc*
Antarctica
Dronning Maud Land
ice core
genre_facet Antarc*
Antarctica
Dronning Maud Land
ice core
op_source EPIC3EGU General Assembly 2014, Vienna, Austria, 2014-04-27-2014-05-02
op_relation Münch, T. orcid:0000-0002-5492-7544 , Freitag, J. orcid:0000-0003-2654-9440 , Meyer, H. orcid:0000-0003-4129-4706 , Kipfstuhl, S. and Laepple, T. orcid:0000-0001-8108-7520 (2014) Two-dimensional insights into the signal formation in low-accumulation firn-cores , EGU General Assembly 2014, Vienna, Austria, 27 April 2014 - 2 May 2014 . hdl:10013/epic.45777
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