Dye 3 trapped gas isotopic analyses covering abrupt warming episodes during last glacial period
Gas analyses were measured to reconstruct the 15Nitrogen/14Nitrogen (d15N) anomaly associated with the abrupt warming episodes better known as the Dansgaard-Oeschger (DO) events. In addition to the d15N analyses, we measured the elemental composition of Oxygen, Nitrogen and Argon in order to assess...
Main Author: | |
---|---|
Format: | Dataset |
Language: | unknown |
Published: |
Arctic Data Center
2022
|
Subjects: | |
Online Access: | https://doi.org/10.18739/A21N7XN9Q |
id |
dataone:doi:10.18739/A21N7XN9Q |
---|---|
record_format |
openpolar |
spelling |
dataone:doi:10.18739/A21N7XN9Q 2024-11-03T19:44:45+00:00 Dye 3 trapped gas isotopic analyses covering abrupt warming episodes during last glacial period Todd Sowers Dye 3 core was drilled in S. Greenland ENVELOPE(-44.0,-43.0,66.0,65.0) BEGINDATE: 2019-01-01T00:00:00Z ENDDATE: 2022-01-01T00:00:00Z 2022-01-01T00:00:00Z https://doi.org/10.18739/A21N7XN9Q unknown Arctic Data Center temperature Dataset 2022 dataone:urn:node:ARCTIC https://doi.org/10.18739/A21N7XN9Q 2024-11-03T19:17:37Z Gas analyses were measured to reconstruct the 15Nitrogen/14Nitrogen (d15N) anomaly associated with the abrupt warming episodes better known as the Dansgaard-Oeschger (DO) events. In addition to the d15N analyses, we measured the elemental composition of Oxygen, Nitrogen and Argon in order to assess the magnitude of gas loss from the core which was drilled in 1981. The Dye 3 d15N data exhibit larger excursions than d15N data from any other ice core (Greenland or Antarctica). Taken at face value, larger d15N excursions imply larger abrupt temperature increases during the warming phases of the DO events. Dataset Antarc* Antarctica Dye 3 Dye-3 Greenland ice core Arctic Data Center (via DataONE) Greenland ENVELOPE(-44.0,-43.0,66.0,65.0) |
institution |
Open Polar |
collection |
Arctic Data Center (via DataONE) |
op_collection_id |
dataone:urn:node:ARCTIC |
language |
unknown |
topic |
temperature |
spellingShingle |
temperature Todd Sowers Dye 3 trapped gas isotopic analyses covering abrupt warming episodes during last glacial period |
topic_facet |
temperature |
description |
Gas analyses were measured to reconstruct the 15Nitrogen/14Nitrogen (d15N) anomaly associated with the abrupt warming episodes better known as the Dansgaard-Oeschger (DO) events. In addition to the d15N analyses, we measured the elemental composition of Oxygen, Nitrogen and Argon in order to assess the magnitude of gas loss from the core which was drilled in 1981. The Dye 3 d15N data exhibit larger excursions than d15N data from any other ice core (Greenland or Antarctica). Taken at face value, larger d15N excursions imply larger abrupt temperature increases during the warming phases of the DO events. |
format |
Dataset |
author |
Todd Sowers |
author_facet |
Todd Sowers |
author_sort |
Todd Sowers |
title |
Dye 3 trapped gas isotopic analyses covering abrupt warming episodes during last glacial period |
title_short |
Dye 3 trapped gas isotopic analyses covering abrupt warming episodes during last glacial period |
title_full |
Dye 3 trapped gas isotopic analyses covering abrupt warming episodes during last glacial period |
title_fullStr |
Dye 3 trapped gas isotopic analyses covering abrupt warming episodes during last glacial period |
title_full_unstemmed |
Dye 3 trapped gas isotopic analyses covering abrupt warming episodes during last glacial period |
title_sort |
dye 3 trapped gas isotopic analyses covering abrupt warming episodes during last glacial period |
publisher |
Arctic Data Center |
publishDate |
2022 |
url |
https://doi.org/10.18739/A21N7XN9Q |
op_coverage |
Dye 3 core was drilled in S. Greenland ENVELOPE(-44.0,-43.0,66.0,65.0) BEGINDATE: 2019-01-01T00:00:00Z ENDDATE: 2022-01-01T00:00:00Z |
long_lat |
ENVELOPE(-44.0,-43.0,66.0,65.0) |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Antarc* Antarctica Dye 3 Dye-3 Greenland ice core |
genre_facet |
Antarc* Antarctica Dye 3 Dye-3 Greenland ice core |
op_doi |
https://doi.org/10.18739/A21N7XN9Q |
_version_ |
1814735217354604544 |