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...

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Published in:Geophysical Research Letters
Main Authors: Muscheler, R., Beer, J.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2006
Subjects:
Online Access:https://doi.org/10.1029/2006GL026779
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spelling 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
institution Open Polar
collection DORA Eawag
op_collection_id fteawag
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
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