DataSheet1_The Influence of Orbital Forcing on 10Be Deposition in Greenland Over the Glacial Period.docx
Understanding the transport and deposition of the cosmogenic isotope 10 Be 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 10 Be from the Gre...
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ftfrontimediafig:oai:figshare.com:article/16621282 2023-05-15T16:26:17+02:00 DataSheet1_The Influence of Orbital Forcing on 10Be Deposition in Greenland Over the Glacial Period.docx Anna Sturevik-Storm Minjie Zheng Ala Aldahan Göran Possnert Raimund Muscheler 2021-09-15T04:12:23Z https://doi.org/10.3389/feart.2021.743640.s001 https://figshare.com/articles/dataset/DataSheet1_The_Influence_of_Orbital_Forcing_on_10Be_Deposition_in_Greenland_Over_the_Glacial_Period_docx/16621282 unknown doi:10.3389/feart.2021.743640.s001 https://figshare.com/articles/dataset/DataSheet1_The_Influence_of_Orbital_Forcing_on_10Be_Deposition_in_Greenland_Over_the_Glacial_Period_docx/16621282 CC BY 4.0 CC-BY Solid Earth Sciences Climate Science Atmospheric Sciences not elsewhere classified Exploration Geochemistry Inorganic Geochemistry Isotope Geochemistry Organic Geochemistry Geochemistry not elsewhere classified Igneous and Metamorphic Petrology Ore Deposit Petrology Palaeontology (incl. Palynology) Structural Geology Tectonics Volcanology Geology not elsewhere classified Seismology and Seismic Exploration Glaciology Hydrogeology Natural Hazards Quaternary Environments Earth Sciences not elsewhere classified Evolutionary Impacts of Climate Change orbital forcing 10Be atmospheric transport aerosol ice core Greenland glacial period Dataset 2021 ftfrontimediafig https://doi.org/10.3389/feart.2021.743640.s001 2021-09-15T22:58:29Z Understanding the transport and deposition of the cosmogenic isotope 10 Be 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 10 Be 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 10 Be records of the last glacial period. This finding can further improve the understanding of 10 Be variability in ice sheets and has the prospect of providing better reconstructions of geomagnetic and solar activity based on cosmogenic radionuclide records. Dataset Greenland Greenland ice cores GRIP ice core Frontiers: Figshare Greenland |
institution |
Open Polar |
collection |
Frontiers: Figshare |
op_collection_id |
ftfrontimediafig |
language |
unknown |
topic |
Solid Earth Sciences Climate Science Atmospheric Sciences not elsewhere classified Exploration Geochemistry Inorganic Geochemistry Isotope Geochemistry Organic Geochemistry Geochemistry not elsewhere classified Igneous and Metamorphic Petrology Ore Deposit Petrology Palaeontology (incl. Palynology) Structural Geology Tectonics Volcanology Geology not elsewhere classified Seismology and Seismic Exploration Glaciology Hydrogeology Natural Hazards Quaternary Environments Earth Sciences not elsewhere classified Evolutionary Impacts of Climate Change orbital forcing 10Be atmospheric transport aerosol ice core Greenland glacial period |
spellingShingle |
Solid Earth Sciences Climate Science Atmospheric Sciences not elsewhere classified Exploration Geochemistry Inorganic Geochemistry Isotope Geochemistry Organic Geochemistry Geochemistry not elsewhere classified Igneous and Metamorphic Petrology Ore Deposit Petrology Palaeontology (incl. Palynology) Structural Geology Tectonics Volcanology Geology not elsewhere classified Seismology and Seismic Exploration Glaciology Hydrogeology Natural Hazards Quaternary Environments Earth Sciences not elsewhere classified Evolutionary Impacts of Climate Change orbital forcing 10Be atmospheric transport aerosol ice core Greenland glacial period Anna Sturevik-Storm Minjie Zheng Ala Aldahan Göran Possnert Raimund Muscheler DataSheet1_The Influence of Orbital Forcing on 10Be Deposition in Greenland Over the Glacial Period.docx |
topic_facet |
Solid Earth Sciences Climate Science Atmospheric Sciences not elsewhere classified Exploration Geochemistry Inorganic Geochemistry Isotope Geochemistry Organic Geochemistry Geochemistry not elsewhere classified Igneous and Metamorphic Petrology Ore Deposit Petrology Palaeontology (incl. Palynology) Structural Geology Tectonics Volcanology Geology not elsewhere classified Seismology and Seismic Exploration Glaciology Hydrogeology Natural Hazards Quaternary Environments Earth Sciences not elsewhere classified Evolutionary Impacts of Climate Change orbital forcing 10Be atmospheric transport aerosol ice core Greenland glacial period |
description |
Understanding the transport and deposition of the cosmogenic isotope 10 Be 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 10 Be 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 10 Be records of the last glacial period. This finding can further improve the understanding of 10 Be variability in ice sheets and has the prospect of providing better reconstructions of geomagnetic and solar activity based on cosmogenic radionuclide records. |
format |
Dataset |
author |
Anna Sturevik-Storm Minjie Zheng Ala Aldahan Göran Possnert Raimund Muscheler |
author_facet |
Anna Sturevik-Storm Minjie Zheng Ala Aldahan Göran Possnert Raimund Muscheler |
author_sort |
Anna Sturevik-Storm |
title |
DataSheet1_The Influence of Orbital Forcing on 10Be Deposition in Greenland Over the Glacial Period.docx |
title_short |
DataSheet1_The Influence of Orbital Forcing on 10Be Deposition in Greenland Over the Glacial Period.docx |
title_full |
DataSheet1_The Influence of Orbital Forcing on 10Be Deposition in Greenland Over the Glacial Period.docx |
title_fullStr |
DataSheet1_The Influence of Orbital Forcing on 10Be Deposition in Greenland Over the Glacial Period.docx |
title_full_unstemmed |
DataSheet1_The Influence of Orbital Forcing on 10Be Deposition in Greenland Over the Glacial Period.docx |
title_sort |
datasheet1_the influence of orbital forcing on 10be deposition in greenland over the glacial period.docx |
publishDate |
2021 |
url |
https://doi.org/10.3389/feart.2021.743640.s001 https://figshare.com/articles/dataset/DataSheet1_The_Influence_of_Orbital_Forcing_on_10Be_Deposition_in_Greenland_Over_the_Glacial_Period_docx/16621282 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Greenland Greenland ice cores GRIP ice core |
genre_facet |
Greenland Greenland ice cores GRIP ice core |
op_relation |
doi:10.3389/feart.2021.743640.s001 https://figshare.com/articles/dataset/DataSheet1_The_Influence_of_Orbital_Forcing_on_10Be_Deposition_in_Greenland_Over_the_Glacial_Period_docx/16621282 |
op_rights |
CC BY 4.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.3389/feart.2021.743640.s001 |
_version_ |
1766015180208078848 |