Automated ice-core layer-counting with strong univariate signals

We present an automated process for determining the annual layer chronology of an ice-core with a strong annual signal, utilising the hydrogen peroxide record from an Antarctic Peninsula ice-core as a test signal on which to count annual cycles and explain the Methods. The signal is de-trended and n...

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Main Authors: Wheatley, J.J., Blackwell, P.G., Abram, Nerilie, McConnell, J.R., Thomas, E.R., Wolff, E.W.
Format: Article in Journal/Newspaper
Language:unknown
Published: Copernicus GmbH 2015
Subjects:
Online Access:http://hdl.handle.net/1885/69420
id ftanucanberra:oai:digitalcollections.anu.edu.au:1885/69420
record_format openpolar
spelling ftanucanberra:oai:digitalcollections.anu.edu.au:1885/69420 2023-05-15T13:36:32+02:00 Automated ice-core layer-counting with strong univariate signals Wheatley, J.J. Blackwell, P.G. Abram, Nerilie McConnell, J.R. Thomas, E.R. Wolff, E.W. 2015-12-10T23:34:24Z http://hdl.handle.net/1885/69420 unknown Copernicus GmbH 1814-9324 http://hdl.handle.net/1885/69420 Climate of the Past Journal article 2015 ftanucanberra 2015-12-28T23:34:29Z We present an automated process for determining the annual layer chronology of an ice-core with a strong annual signal, utilising the hydrogen peroxide record from an Antarctic Peninsula ice-core as a test signal on which to count annual cycles and explain the Methods. The signal is de-trended and normalised before being split into sections with a deterministic cycle count and those that need more attention. Possible reconstructions for the uncertain sections are determined which could be used as a visual aid for manual counting, and a simple method for assigning probability measures to each reconstruction is discussed. The robustness of this process is explored by applying it to versions of two different chemistry signals from the same stretch of the NGRIP (North Greenland Ice Core Project) ice-core, which shows more variation in annual layer thickness, with and without thinning to mimic poorer quality data. An adapted version of these Methods is applied to the more challenging non-sea-salt sulphur signal from the same Antarctic Peninsula core from which the hydrogen peroxide signal was taken. These Methods could readily be adapted for use on much longer datasets, thereby reducing manual effort and providing a robust automated layer-counting methodology. Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula Greenland Greenland ice core Greenland Ice core Project ice core NGRIP North Greenland North Greenland Ice Core Project Australian National University: ANU Digital Collections Antarctic Antarctic Peninsula Greenland
institution Open Polar
collection Australian National University: ANU Digital Collections
op_collection_id ftanucanberra
language unknown
description We present an automated process for determining the annual layer chronology of an ice-core with a strong annual signal, utilising the hydrogen peroxide record from an Antarctic Peninsula ice-core as a test signal on which to count annual cycles and explain the Methods. The signal is de-trended and normalised before being split into sections with a deterministic cycle count and those that need more attention. Possible reconstructions for the uncertain sections are determined which could be used as a visual aid for manual counting, and a simple method for assigning probability measures to each reconstruction is discussed. The robustness of this process is explored by applying it to versions of two different chemistry signals from the same stretch of the NGRIP (North Greenland Ice Core Project) ice-core, which shows more variation in annual layer thickness, with and without thinning to mimic poorer quality data. An adapted version of these Methods is applied to the more challenging non-sea-salt sulphur signal from the same Antarctic Peninsula core from which the hydrogen peroxide signal was taken. These Methods could readily be adapted for use on much longer datasets, thereby reducing manual effort and providing a robust automated layer-counting methodology.
format Article in Journal/Newspaper
author Wheatley, J.J.
Blackwell, P.G.
Abram, Nerilie
McConnell, J.R.
Thomas, E.R.
Wolff, E.W.
spellingShingle Wheatley, J.J.
Blackwell, P.G.
Abram, Nerilie
McConnell, J.R.
Thomas, E.R.
Wolff, E.W.
Automated ice-core layer-counting with strong univariate signals
author_facet Wheatley, J.J.
Blackwell, P.G.
Abram, Nerilie
McConnell, J.R.
Thomas, E.R.
Wolff, E.W.
author_sort Wheatley, J.J.
title Automated ice-core layer-counting with strong univariate signals
title_short Automated ice-core layer-counting with strong univariate signals
title_full Automated ice-core layer-counting with strong univariate signals
title_fullStr Automated ice-core layer-counting with strong univariate signals
title_full_unstemmed Automated ice-core layer-counting with strong univariate signals
title_sort automated ice-core layer-counting with strong univariate signals
publisher Copernicus GmbH
publishDate 2015
url http://hdl.handle.net/1885/69420
geographic Antarctic
Antarctic Peninsula
Greenland
geographic_facet Antarctic
Antarctic Peninsula
Greenland
genre Antarc*
Antarctic
Antarctic Peninsula
Greenland
Greenland ice core
Greenland Ice core Project
ice core
NGRIP
North Greenland
North Greenland Ice Core Project
genre_facet Antarc*
Antarctic
Antarctic Peninsula
Greenland
Greenland ice core
Greenland Ice core Project
ice core
NGRIP
North Greenland
North Greenland Ice Core Project
op_source Climate of the Past
op_relation 1814-9324
http://hdl.handle.net/1885/69420
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