The NUNAtak Ice Thinning (NUNAIT) Calculator for Cosmonuclide Elevation Profiles

Cosmogenic nuclides are widely used to constrain the landscape history of glaciated areas. At nunataks in continental polar regions with extremely arid conditions, cosmogenic nuclides are often the only method available to date the ice thinning history of the glacier. However, the amount of cosmogen...

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Main Author: Ángel Rodés
Format: Article
Language:English
Published: MDPI AG 2021-08-01
Series:Geosciences
Subjects:
Online Access:https://www.mdpi.com/2076-3263/11/9/362
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author Ángel Rodés
author_facet Ángel Rodés
author_sort Ángel Rodés
collection DOAJ
description Cosmogenic nuclides are widely used to constrain the landscape history of glaciated areas. At nunataks in continental polar regions with extremely arid conditions, cosmogenic nuclides are often the only method available to date the ice thinning history of the glacier. However, the amount of cosmogenic isotopes accumulated at the surface of nunataks depends not only on the length of time that rock has been exposed since the last deglaciation but also on the full history of the surface, including muon production under ice, exposure during previous interglacials, subaerial weathering rate, glacial erosion rate, and uplift rate of the nunatak. The NUNAtak Ice Thinning model (NUNAIT) simulates the cosmonuclide accumulation on vertical profiles, fitting the aforementioned parameters to a set of multi-isotope apparent ages from samples taken at different elevations over the ice-sheet surface. The NUNAIT calculator is an easy-to-use tool that constrains parameters that describe the geological history of a nunatak from a set of surface exposure ages.
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spelling doaj.art-288ff447b36441a08d7aa5d2c00d7fa62023-11-22T13:15:47ZengMDPI AGGeosciences2076-32632021-08-0111936210.3390/geosciences11090362The NUNAtak Ice Thinning (NUNAIT) Calculator for Cosmonuclide Elevation ProfilesÁngel Rodés0Scottish Universities Environmental Research Centre, University of Glasgow, East Kilbride G75 0QF, UKCosmogenic nuclides are widely used to constrain the landscape history of glaciated areas. At nunataks in continental polar regions with extremely arid conditions, cosmogenic nuclides are often the only method available to date the ice thinning history of the glacier. However, the amount of cosmogenic isotopes accumulated at the surface of nunataks depends not only on the length of time that rock has been exposed since the last deglaciation but also on the full history of the surface, including muon production under ice, exposure during previous interglacials, subaerial weathering rate, glacial erosion rate, and uplift rate of the nunatak. The NUNAtak Ice Thinning model (NUNAIT) simulates the cosmonuclide accumulation on vertical profiles, fitting the aforementioned parameters to a set of multi-isotope apparent ages from samples taken at different elevations over the ice-sheet surface. The NUNAIT calculator is an easy-to-use tool that constrains parameters that describe the geological history of a nunatak from a set of surface exposure ages.https://www.mdpi.com/2076-3263/11/9/362nunatakcosmonuclides<sup>10</sup>Be<sup>26</sup>Al<sup>21</sup>Ne<sup>3</sup>He
spellingShingle Ángel Rodés
The NUNAtak Ice Thinning (NUNAIT) Calculator for Cosmonuclide Elevation Profiles
Geosciences
nunatak
cosmonuclides
<sup>10</sup>Be
<sup>26</sup>Al
<sup>21</sup>Ne
<sup>3</sup>He
title The NUNAtak Ice Thinning (NUNAIT) Calculator for Cosmonuclide Elevation Profiles
title_full The NUNAtak Ice Thinning (NUNAIT) Calculator for Cosmonuclide Elevation Profiles
title_fullStr The NUNAtak Ice Thinning (NUNAIT) Calculator for Cosmonuclide Elevation Profiles
title_full_unstemmed The NUNAtak Ice Thinning (NUNAIT) Calculator for Cosmonuclide Elevation Profiles
title_short The NUNAtak Ice Thinning (NUNAIT) Calculator for Cosmonuclide Elevation Profiles
title_sort nunatak ice thinning nunait calculator for cosmonuclide elevation profiles
topic nunatak
cosmonuclides
<sup>10</sup>Be
<sup>26</sup>Al
<sup>21</sup>Ne
<sup>3</sup>He
url https://www.mdpi.com/2076-3263/11/9/362
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