Solar forced Dansgaard/Oeschger events?
It has been suggested that the strong climatic changes during the last ice age, the so-called Dansgaard/Oeschger (D/O) events, could have been prompted by solar activity changes. This hypothesis is based on the apparent cyclic occurrence of the D/O events and the solar influence on climate during th...
Published in: | Geophysical Research Letters |
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Online Access: | https://doi.org/10.1029/2006GL026779 |
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fteawag:oai:dora:eawag_5319 2024-09-15T18:03:29+00:00 Solar forced Dansgaard/Oeschger events? Muscheler, R. Beer, J. 2006 https://doi.org/10.1029/2006GL026779 eng eng Wiley Geophysical Research Letters--Geophys. Res. Lett.--journals:1144--0094-8276 eawag:5319 journal id: journals:1144 issn: 0094-8276 ut: 000241700000002 local: 10780 scopus: 2-s2.0-33845610051 doi:10.1029/2006GL026779 Text Journal Article 2006 fteawag https://doi.org/10.1029/2006GL026779 2024-08-05T03:04:29Z It has been suggested that the strong climatic changes during the last ice age, the so-called Dansgaard/Oeschger (D/O) events, could have been prompted by solar activity changes. This hypothesis is based on the apparent cyclic occurrence of the D/O events and the solar influence on climate during the Holocene on similar time scales. We test this hypothesis by comparing the 10 Be and δ 18 O records from the GRIP ice core. A superimposed epoch analysis allows us to reduce the noise in the data and to extract estimates of solar activity changes in connection to the D/O events. This comparison does not provide convincing evidence for a persistent solar influence on these strong climatic oscillations during the last ice age. Article in Journal/Newspaper Dansgaard-Oeschger events ice core DORA Eawag Geophysical Research Letters 33 20 |
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Open Polar |
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DORA Eawag |
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language |
English |
description |
It has been suggested that the strong climatic changes during the last ice age, the so-called Dansgaard/Oeschger (D/O) events, could have been prompted by solar activity changes. This hypothesis is based on the apparent cyclic occurrence of the D/O events and the solar influence on climate during the Holocene on similar time scales. We test this hypothesis by comparing the 10 Be and δ 18 O records from the GRIP ice core. A superimposed epoch analysis allows us to reduce the noise in the data and to extract estimates of solar activity changes in connection to the D/O events. This comparison does not provide convincing evidence for a persistent solar influence on these strong climatic oscillations during the last ice age. |
format |
Article in Journal/Newspaper |
author |
Muscheler, R. Beer, J. |
spellingShingle |
Muscheler, R. Beer, J. Solar forced Dansgaard/Oeschger events? |
author_facet |
Muscheler, R. Beer, J. |
author_sort |
Muscheler, R. |
title |
Solar forced Dansgaard/Oeschger events? |
title_short |
Solar forced Dansgaard/Oeschger events? |
title_full |
Solar forced Dansgaard/Oeschger events? |
title_fullStr |
Solar forced Dansgaard/Oeschger events? |
title_full_unstemmed |
Solar forced Dansgaard/Oeschger events? |
title_sort |
solar forced dansgaard/oeschger events? |
publisher |
Wiley |
publishDate |
2006 |
url |
https://doi.org/10.1029/2006GL026779 |
genre |
Dansgaard-Oeschger events ice core |
genre_facet |
Dansgaard-Oeschger events ice core |
op_relation |
Geophysical Research Letters--Geophys. Res. Lett.--journals:1144--0094-8276 eawag:5319 journal id: journals:1144 issn: 0094-8276 ut: 000241700000002 local: 10780 scopus: 2-s2.0-33845610051 doi:10.1029/2006GL026779 |
op_doi |
https://doi.org/10.1029/2006GL026779 |
container_title |
Geophysical Research Letters |
container_volume |
33 |
container_issue |
20 |
_version_ |
1810440965494669312 |