Water stable isotope record of ice cores NGRIP I and II ...
A high resolution (0.05 m) water isotopic record (d18O) is available from the NorthGRIP ice core. In this study we look into the water isotope diffusion history as estimated by the spectral characteristics of the d18O time series covering the last 16,000 years. The diffusion of water vapor in the po...
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Online Access: | https://dx.doi.org/10.1594/pangaea.886044 https://doi.pangaea.de/10.1594/PANGAEA.886044 |
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ftdatacite:10.1594/pangaea.886044 2024-04-28T08:19:40+00:00 Water stable isotope record of ice cores NGRIP I and II ... Gkinis, Vasileios Simonsen, Sebastian B Buchardt, Susanne L White, James W C Vinther, Bo Møllesøe 2018 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.886044 https://doi.pangaea.de/10.1594/PANGAEA.886044 en eng PANGAEA https://dx.doi.org/10.1016/j.epsl.2014.08.022 Creative Commons Attribution Non Commercial No Derivatives 3.0 Unported https://creativecommons.org/licenses/by-nc-nd/3.0/legalcode cc-by-nc-nd-3.0 DEPTH, ice/snow δ18O, water Ice drill NGRIP Sampling/drilling ice Greenland Ice Core Projects GRIP/GISP/NGRIP North Greenland Ice Core Project NGRIP dataset Supplementary Dataset Dataset 2018 ftdatacite https://doi.org/10.1594/pangaea.88604410.1016/j.epsl.2014.08.022 2024-04-02T11:42:33Z A high resolution (0.05 m) water isotopic record (d18O) is available from the NorthGRIP ice core. In this study we look into the water isotope diffusion history as estimated by the spectral characteristics of the d18O time series covering the last 16,000 years. The diffusion of water vapor in the porous medium of the firn pack attenuates the initial isotopic signal, predominantly having an impact on the high frequency components of the power spectrum. Higher temperatures induce higher rates of smoothing and thus the signal can be used as a firn paleothermometer. We use a water isotope diffusion model coupled to a steady-state densification model in order to infer the temperature signal from the site, assuming the accumulation and strain rate history as estimated using the GICC05 layer counted chronology and a Dansgaard-Johnsen ice flow model. The temperature reconstruction accurately captures the timing and magnitude of the Bølling-Allerød and Younger Dryas transitions. A Holocene climatic optimum is seen ... : The overlapping NGRIP I and II core sampled with a 5 cm resolution an measured on an IRMS. Even though the depth is identical, it is not expected that the age is completely identical. ... Dataset GISP Greenland Greenland ice core Greenland Ice core Project GRIP ice core NGRIP North Greenland North Greenland Ice Core Project DataCite Metadata Store (German National Library of Science and Technology) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
DEPTH, ice/snow δ18O, water Ice drill NGRIP Sampling/drilling ice Greenland Ice Core Projects GRIP/GISP/NGRIP North Greenland Ice Core Project NGRIP |
spellingShingle |
DEPTH, ice/snow δ18O, water Ice drill NGRIP Sampling/drilling ice Greenland Ice Core Projects GRIP/GISP/NGRIP North Greenland Ice Core Project NGRIP Gkinis, Vasileios Simonsen, Sebastian B Buchardt, Susanne L White, James W C Vinther, Bo Møllesøe Water stable isotope record of ice cores NGRIP I and II ... |
topic_facet |
DEPTH, ice/snow δ18O, water Ice drill NGRIP Sampling/drilling ice Greenland Ice Core Projects GRIP/GISP/NGRIP North Greenland Ice Core Project NGRIP |
description |
A high resolution (0.05 m) water isotopic record (d18O) is available from the NorthGRIP ice core. In this study we look into the water isotope diffusion history as estimated by the spectral characteristics of the d18O time series covering the last 16,000 years. The diffusion of water vapor in the porous medium of the firn pack attenuates the initial isotopic signal, predominantly having an impact on the high frequency components of the power spectrum. Higher temperatures induce higher rates of smoothing and thus the signal can be used as a firn paleothermometer. We use a water isotope diffusion model coupled to a steady-state densification model in order to infer the temperature signal from the site, assuming the accumulation and strain rate history as estimated using the GICC05 layer counted chronology and a Dansgaard-Johnsen ice flow model. The temperature reconstruction accurately captures the timing and magnitude of the Bølling-Allerød and Younger Dryas transitions. A Holocene climatic optimum is seen ... : The overlapping NGRIP I and II core sampled with a 5 cm resolution an measured on an IRMS. Even though the depth is identical, it is not expected that the age is completely identical. ... |
format |
Dataset |
author |
Gkinis, Vasileios Simonsen, Sebastian B Buchardt, Susanne L White, James W C Vinther, Bo Møllesøe |
author_facet |
Gkinis, Vasileios Simonsen, Sebastian B Buchardt, Susanne L White, James W C Vinther, Bo Møllesøe |
author_sort |
Gkinis, Vasileios |
title |
Water stable isotope record of ice cores NGRIP I and II ... |
title_short |
Water stable isotope record of ice cores NGRIP I and II ... |
title_full |
Water stable isotope record of ice cores NGRIP I and II ... |
title_fullStr |
Water stable isotope record of ice cores NGRIP I and II ... |
title_full_unstemmed |
Water stable isotope record of ice cores NGRIP I and II ... |
title_sort |
water stable isotope record of ice cores ngrip i and ii ... |
publisher |
PANGAEA |
publishDate |
2018 |
url |
https://dx.doi.org/10.1594/pangaea.886044 https://doi.pangaea.de/10.1594/PANGAEA.886044 |
genre |
GISP Greenland Greenland ice core Greenland Ice core Project GRIP ice core NGRIP North Greenland North Greenland Ice Core Project |
genre_facet |
GISP Greenland Greenland ice core Greenland Ice core Project GRIP ice core NGRIP North Greenland North Greenland Ice Core Project |
op_relation |
https://dx.doi.org/10.1016/j.epsl.2014.08.022 |
op_rights |
Creative Commons Attribution Non Commercial No Derivatives 3.0 Unported https://creativecommons.org/licenses/by-nc-nd/3.0/legalcode cc-by-nc-nd-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.88604410.1016/j.epsl.2014.08.022 |
_version_ |
1797583047031259136 |