The Influence of Orbital Forcing on 10Be Deposition in Greenland Over the Glacial Period

Understanding the transport and deposition of the cosmogenic isotope 10Be is vital for the application of the isotope data to infer past changes of solar activity, to reconstruct past Earth’s magnetic field intensity and climate change. Here, we use data of the cosmogenic isotope 10Be from the Green...

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Main Authors: Anna Sturevik-Storm, Minjie Zheng, Ala Aldahan, Göran Possnert, Raimund Muscheler
Format: Article
Language:English
Published: Frontiers Media S.A. 2021-09-01
Series:Frontiers in Earth Science
Subjects:
Online Access:https://www.frontiersin.org/articles/10.3389/feart.2021.743640/full
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spelling doaj-4fbe5631a4ba43eebe6daa3718aed01a2021-09-15T04:34:07ZengFrontiers Media S.A.Frontiers in Earth Science2296-64632021-09-01910.3389/feart.2021.743640743640The Influence of Orbital Forcing on 10Be Deposition in Greenland Over the Glacial PeriodAnna Sturevik-Storm0Minjie Zheng1Ala Aldahan2Göran Possnert3Raimund Muscheler4Department of Earth Sciences, Uppsala University, Uppsala, SwedenDepartment of Geology, Lund University, Lund, SwedenDepartment of Geology, United Arab Emirates University, Al Ain, United Arab EmiratesTandem Laboratory, Uppsala University, Uppsala, SwedenDepartment of Geology, Lund University, Lund, SwedenUnderstanding the transport and deposition of the cosmogenic isotope 10Be is vital for the application of the isotope data to infer past changes of solar activity, to reconstruct past Earth’s magnetic field intensity and climate change. Here, we use data of the cosmogenic isotope 10Be from the Greenland ice cores, namely the NEEM and GRIP ice cores, to identify factors controlling its distribution. After removing the effects of the geomagnetic field on the cosmogenic radionuclide production rate, the results expose imprints of the 20–22 ka precession cycle on the Greenland 10Be records of the last glacial period. This finding can further improve the understanding of 10Be variability in ice sheets and has the prospect of providing better reconstructions of geomagnetic and solar activity based on cosmogenic radionuclide records.https://www.frontiersin.org/articles/10.3389/feart.2021.743640/fullorbital forcing10Beatmospheric transportaerosolice coreGreenland
collection DOAJ
language English
format Article
sources DOAJ
author Anna Sturevik-Storm
Minjie Zheng
Ala Aldahan
Göran Possnert
Raimund Muscheler
spellingShingle Anna Sturevik-Storm
Minjie Zheng
Ala Aldahan
Göran Possnert
Raimund Muscheler
The Influence of Orbital Forcing on 10Be Deposition in Greenland Over the Glacial Period
Frontiers in Earth Science
orbital forcing
10Be
atmospheric transport
aerosol
ice core
Greenland
author_facet Anna Sturevik-Storm
Minjie Zheng
Ala Aldahan
Göran Possnert
Raimund Muscheler
author_sort Anna Sturevik-Storm
title The Influence of Orbital Forcing on 10Be Deposition in Greenland Over the Glacial Period
title_short The Influence of Orbital Forcing on 10Be Deposition in Greenland Over the Glacial Period
title_full The Influence of Orbital Forcing on 10Be Deposition in Greenland Over the Glacial Period
title_fullStr The Influence of Orbital Forcing on 10Be Deposition in Greenland Over the Glacial Period
title_full_unstemmed The Influence of Orbital Forcing on 10Be Deposition in Greenland Over the Glacial Period
title_sort influence of orbital forcing on 10be deposition in greenland over the glacial period
publisher Frontiers Media S.A.
series Frontiers in Earth Science
issn 2296-6463
publishDate 2021-09-01
description Understanding the transport and deposition of the cosmogenic isotope 10Be is vital for the application of the isotope data to infer past changes of solar activity, to reconstruct past Earth’s magnetic field intensity and climate change. Here, we use data of the cosmogenic isotope 10Be from the Greenland ice cores, namely the NEEM and GRIP ice cores, to identify factors controlling its distribution. After removing the effects of the geomagnetic field on the cosmogenic radionuclide production rate, the results expose imprints of the 20–22 ka precession cycle on the Greenland 10Be records of the last glacial period. This finding can further improve the understanding of 10Be variability in ice sheets and has the prospect of providing better reconstructions of geomagnetic and solar activity based on cosmogenic radionuclide records.
topic orbital forcing
10Be
atmospheric transport
aerosol
ice core
Greenland
url https://www.frontiersin.org/articles/10.3389/feart.2021.743640/full
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