Radium, water isotopes, and salinity on the East Siberian Sea slope - NABOS 2018

Radium isotopes (radium-228 and radium-226), water isotopes (oxygen-18 and deuterium), and salinity were measured on the slope of the East Siberian Sea in coordination with the 2018 Nansen and Amundsen Basins Observational System (NABOS) expedition. Radium is continuously produced at ocean boundarie...

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Main Authors: Lauren Kipp, Matthew Charette
Format: Dataset
Language:unknown
Published: Arctic Data Center 2023
Subjects:
Online Access:https://doi.org/10.18739/A2FB4WN6B
id dataone:doi:10.18739/A2FB4WN6B
record_format openpolar
spelling dataone:doi:10.18739/A2FB4WN6B 2024-06-03T18:46:38+00:00 Radium, water isotopes, and salinity on the East Siberian Sea slope - NABOS 2018 Lauren Kipp Matthew Charette East Siberian Sea ENVELOPE(148.0,169.0,81.0,75.0) BEGINDATE: 2018-09-07T00:00:00Z ENDDATE: 2018-09-17T00:00:00Z 2023-01-01T00:00:00Z https://doi.org/10.18739/A2FB4WN6B unknown Arctic Data Center NABOS radium water isotopes East Siberian Sea Dataset 2023 dataone:urn:node:ARCTIC https://doi.org/10.18739/A2FB4WN6B 2024-06-03T18:19:30Z Radium isotopes (radium-228 and radium-226), water isotopes (oxygen-18 and deuterium), and salinity were measured on the slope of the East Siberian Sea in coordination with the 2018 Nansen and Amundsen Basins Observational System (NABOS) expedition. Radium is continuously produced at ocean boundaries and is soluble in seawater, thus it serves as an analogue for similarly sourced sediment-derived materials. Because the Eastern Arctic shelves are the origin of the Transpolar Drift, monitoring the radium levels in this region improves our understanding of potential climate-driven changes on the transport of shelf-derived materials offshore. Dataset Arctic East Siberian Sea Arctic Data Center (via DataONE) Arctic East Siberian Sea ENVELOPE(166.000,166.000,74.000,74.000) ENVELOPE(148.0,169.0,81.0,75.0)
institution Open Polar
collection Arctic Data Center (via DataONE)
op_collection_id dataone:urn:node:ARCTIC
language unknown
topic NABOS
radium
water isotopes
East Siberian Sea
spellingShingle NABOS
radium
water isotopes
East Siberian Sea
Lauren Kipp
Matthew Charette
Radium, water isotopes, and salinity on the East Siberian Sea slope - NABOS 2018
topic_facet NABOS
radium
water isotopes
East Siberian Sea
description Radium isotopes (radium-228 and radium-226), water isotopes (oxygen-18 and deuterium), and salinity were measured on the slope of the East Siberian Sea in coordination with the 2018 Nansen and Amundsen Basins Observational System (NABOS) expedition. Radium is continuously produced at ocean boundaries and is soluble in seawater, thus it serves as an analogue for similarly sourced sediment-derived materials. Because the Eastern Arctic shelves are the origin of the Transpolar Drift, monitoring the radium levels in this region improves our understanding of potential climate-driven changes on the transport of shelf-derived materials offshore.
format Dataset
author Lauren Kipp
Matthew Charette
author_facet Lauren Kipp
Matthew Charette
author_sort Lauren Kipp
title Radium, water isotopes, and salinity on the East Siberian Sea slope - NABOS 2018
title_short Radium, water isotopes, and salinity on the East Siberian Sea slope - NABOS 2018
title_full Radium, water isotopes, and salinity on the East Siberian Sea slope - NABOS 2018
title_fullStr Radium, water isotopes, and salinity on the East Siberian Sea slope - NABOS 2018
title_full_unstemmed Radium, water isotopes, and salinity on the East Siberian Sea slope - NABOS 2018
title_sort radium, water isotopes, and salinity on the east siberian sea slope - nabos 2018
publisher Arctic Data Center
publishDate 2023
url https://doi.org/10.18739/A2FB4WN6B
op_coverage East Siberian Sea
ENVELOPE(148.0,169.0,81.0,75.0)
BEGINDATE: 2018-09-07T00:00:00Z ENDDATE: 2018-09-17T00:00:00Z
long_lat ENVELOPE(166.000,166.000,74.000,74.000)
ENVELOPE(148.0,169.0,81.0,75.0)
geographic Arctic
East Siberian Sea
geographic_facet Arctic
East Siberian Sea
genre Arctic
East Siberian Sea
genre_facet Arctic
East Siberian Sea
op_doi https://doi.org/10.18739/A2FB4WN6B
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