90 ka Antarctic tracers. : Tracer migration from 90-0 ka BP. Tracers are seeded at the surface at 90 ka BP and transported with the ice flow over time. Coloring illustrates absolute tracer elevation.

This video depicts Lagrangian tracer migration from 90-0 ka BP across the Antarctic Ice Sheet. Tracers are seeded at the surface at 90 ka BP and transported with the ice flow over time. Coloring illustrates absolute tracer elevation.

Bibliographic Details
Main Author: Sutter, Johannes
Format: Article in Journal/Newspaper
Language:unknown
Published: Copernicus Publications 2020
Subjects:
Online Access:https://dx.doi.org/10.5446/50125
https://av.tib.eu/media/50125
id ftdatacite:10.5446/50125
record_format openpolar
spelling ftdatacite:10.5446/50125 2023-05-15T13:40:37+02:00 90 ka Antarctic tracers. : Tracer migration from 90-0 ka BP. Tracers are seeded at the surface at 90 ka BP and transported with the ice flow over time. Coloring illustrates absolute tracer elevation. Sutter, Johannes 2020 https://dx.doi.org/10.5446/50125 https://av.tib.eu/media/50125 unknown Copernicus Publications Earth Sciences Antarctica Tracers Experiment/Model Test MediaObject article Audiovisual 2020 ftdatacite https://doi.org/10.5446/50125 2021-11-05T12:55:41Z This video depicts Lagrangian tracer migration from 90-0 ka BP across the Antarctic Ice Sheet. Tracers are seeded at the surface at 90 ka BP and transported with the ice flow over time. Coloring illustrates absolute tracer elevation. Article in Journal/Newspaper Antarc* Antarctic Antarctica Ice Sheet DataCite Metadata Store (German National Library of Science and Technology) Antarctic The Antarctic
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
topic Earth Sciences
Antarctica
Tracers
spellingShingle Earth Sciences
Antarctica
Tracers
Sutter, Johannes
90 ka Antarctic tracers. : Tracer migration from 90-0 ka BP. Tracers are seeded at the surface at 90 ka BP and transported with the ice flow over time. Coloring illustrates absolute tracer elevation.
topic_facet Earth Sciences
Antarctica
Tracers
description This video depicts Lagrangian tracer migration from 90-0 ka BP across the Antarctic Ice Sheet. Tracers are seeded at the surface at 90 ka BP and transported with the ice flow over time. Coloring illustrates absolute tracer elevation.
format Article in Journal/Newspaper
author Sutter, Johannes
author_facet Sutter, Johannes
author_sort Sutter, Johannes
title 90 ka Antarctic tracers. : Tracer migration from 90-0 ka BP. Tracers are seeded at the surface at 90 ka BP and transported with the ice flow over time. Coloring illustrates absolute tracer elevation.
title_short 90 ka Antarctic tracers. : Tracer migration from 90-0 ka BP. Tracers are seeded at the surface at 90 ka BP and transported with the ice flow over time. Coloring illustrates absolute tracer elevation.
title_full 90 ka Antarctic tracers. : Tracer migration from 90-0 ka BP. Tracers are seeded at the surface at 90 ka BP and transported with the ice flow over time. Coloring illustrates absolute tracer elevation.
title_fullStr 90 ka Antarctic tracers. : Tracer migration from 90-0 ka BP. Tracers are seeded at the surface at 90 ka BP and transported with the ice flow over time. Coloring illustrates absolute tracer elevation.
title_full_unstemmed 90 ka Antarctic tracers. : Tracer migration from 90-0 ka BP. Tracers are seeded at the surface at 90 ka BP and transported with the ice flow over time. Coloring illustrates absolute tracer elevation.
title_sort 90 ka antarctic tracers. : tracer migration from 90-0 ka bp. tracers are seeded at the surface at 90 ka bp and transported with the ice flow over time. coloring illustrates absolute tracer elevation.
publisher Copernicus Publications
publishDate 2020
url https://dx.doi.org/10.5446/50125
https://av.tib.eu/media/50125
geographic Antarctic
The Antarctic
geographic_facet Antarctic
The Antarctic
genre Antarc*
Antarctic
Antarctica
Ice Sheet
genre_facet Antarc*
Antarctic
Antarctica
Ice Sheet
op_doi https://doi.org/10.5446/50125
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