Synchronization of ice core records via atmospheric gases
To interpret new high resolution climate records it becomes more and more important to know about the succession of climate events. Such knowledge is hard to get especially when dealing with different types of climate archives. Even for ice cores a direct synchronization between ice cores from Green...
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fttriple:oai:gotriple.eu:10670/1.nt567c 2023-05-15T13:32:54+02:00 Synchronization of ice core records via atmospheric gases Blunier, T. Spahni, R. Barnola, J.-M. Chappellaz, J. Loulergue, L. Schwander, J. 2018-09-27 https://doi.org/10.5194/cp-3-325-2007 https://cp.copernicus.org/articles/3/325/2007/ en eng doi:10.5194/cp-3-325-2007 10670/1.nt567c https://cp.copernicus.org/articles/3/325/2007/ undefined Geographica Helvetica - geography eISSN: 1814-9332 geo envir Text https://vocabularies.coar-repositories.org/resource_types/c_18cf/ 2018 fttriple https://doi.org/10.5194/cp-3-325-2007 2023-01-22T17:00:44Z To interpret new high resolution climate records it becomes more and more important to know about the succession of climate events. Such knowledge is hard to get especially when dealing with different types of climate archives. Even for ice cores a direct synchronization between ice cores from Greenland and Antarctica has not been possible so far due to the lack of time markers occurring in both hemispheres. Fortunately, variations in the time series of global gas records can be used as indirect time markers. Here we discuss in detail the steps that are necessary to synchronize ice cores via global gas records exemplified on the synchronization of the EPICA ice core from Dronning Maud Land to a Greenland record from North GRIP. Text Antarc* Antarctica Dronning Maud Land EPICA Greenland GRIP ice core Unknown Dronning Maud Land Greenland Climate of the Past 3 2 325 330 |
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geo envir Blunier, T. Spahni, R. Barnola, J.-M. Chappellaz, J. Loulergue, L. Schwander, J. Synchronization of ice core records via atmospheric gases |
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geo envir |
description |
To interpret new high resolution climate records it becomes more and more important to know about the succession of climate events. Such knowledge is hard to get especially when dealing with different types of climate archives. Even for ice cores a direct synchronization between ice cores from Greenland and Antarctica has not been possible so far due to the lack of time markers occurring in both hemispheres. Fortunately, variations in the time series of global gas records can be used as indirect time markers. Here we discuss in detail the steps that are necessary to synchronize ice cores via global gas records exemplified on the synchronization of the EPICA ice core from Dronning Maud Land to a Greenland record from North GRIP. |
format |
Text |
author |
Blunier, T. Spahni, R. Barnola, J.-M. Chappellaz, J. Loulergue, L. Schwander, J. |
author_facet |
Blunier, T. Spahni, R. Barnola, J.-M. Chappellaz, J. Loulergue, L. Schwander, J. |
author_sort |
Blunier, T. |
title |
Synchronization of ice core records via atmospheric gases |
title_short |
Synchronization of ice core records via atmospheric gases |
title_full |
Synchronization of ice core records via atmospheric gases |
title_fullStr |
Synchronization of ice core records via atmospheric gases |
title_full_unstemmed |
Synchronization of ice core records via atmospheric gases |
title_sort |
synchronization of ice core records via atmospheric gases |
publishDate |
2018 |
url |
https://doi.org/10.5194/cp-3-325-2007 https://cp.copernicus.org/articles/3/325/2007/ |
geographic |
Dronning Maud Land Greenland |
geographic_facet |
Dronning Maud Land Greenland |
genre |
Antarc* Antarctica Dronning Maud Land EPICA Greenland GRIP ice core |
genre_facet |
Antarc* Antarctica Dronning Maud Land EPICA Greenland GRIP ice core |
op_source |
Geographica Helvetica - geography eISSN: 1814-9332 |
op_relation |
doi:10.5194/cp-3-325-2007 10670/1.nt567c https://cp.copernicus.org/articles/3/325/2007/ |
op_rights |
undefined |
op_doi |
https://doi.org/10.5194/cp-3-325-2007 |
container_title |
Climate of the Past |
container_volume |
3 |
container_issue |
2 |
container_start_page |
325 |
op_container_end_page |
330 |
_version_ |
1766036875254956032 |