Collaborative Research: Ice Core Studies Reconstructing Greenland Climate During the Eemian and Beyond

The primary goal of this collaborative project between three institutions is to understand the extent and evolution of the Greenland Ice Sheet (GrIS) during the Eemian period (roughly 130,000 to 115,000 years ago, the last major interglacial period in Earth's history) and the deglaciation immed...

Full description

Bibliographic Details
Main Author: Bender, Michael
Format: Dataset
Language:English
Published: NSF Arctic Data Center 2015
Subjects:
ANS
Online Access:https://dx.doi.org/10.18739/a25x25d26
https://arcticdata.io/catalog/view/doi:10.18739/A25X25D26
id ftdatacite:10.18739/a25x25d26
record_format openpolar
spelling ftdatacite:10.18739/a25x25d26 2023-05-15T15:19:48+02:00 Collaborative Research: Ice Core Studies Reconstructing Greenland Climate During the Eemian and Beyond Bender, Michael 2015 text/xml https://dx.doi.org/10.18739/a25x25d26 https://arcticdata.io/catalog/view/doi:10.18739/A25X25D26 en eng NSF Arctic Data Center ANS dataset Dataset 2015 ftdatacite https://doi.org/10.18739/a25x25d26 2021-11-05T12:55:41Z The primary goal of this collaborative project between three institutions is to understand the extent and evolution of the Greenland Ice Sheet (GrIS) during the Eemian period (roughly 130,000 to 115,000 years ago, the last major interglacial period in Earth's history) and the deglaciation immediately preceding it ("Termination 2"). The GrIS is an important agent influencing sea level, and Arctic and global climate, on multiple timescales. Its dynamics need to be understood in the context of past climate changes, but there is little information available about the footprint, volume, and elevation of the GrIS prior to the last ice age due to the absence of continuous ice core records prior to 123,000 years ago. During the Eemian, the GrIS was perhaps half its present size, contributing on the order of 3 m to "excess" sea level rise. Characterizing the evolution of the GrIS during glacial termination 2 and the Eemian would improve our understanding of its dynamics, and enhance our ability to make projections of sea level rise during the coming centuries. Older ice does exist at the bottoms of previously drilled ice cores, but the extraction of age and climate information from this older ice is hampered by the fact that it is stratigraphically disturbed and, in many cases, contaminated with soil or bedrock material. These investigators propose several novel methods to date this disturbed and/or "dirty" ice and to extract information on climate and ice sheet extent. The investigators will combine their new measurements and other available data to develop a more complete history of the GrIS during termination 2 and the Eemian. They will work with ice sheet modelers to investigate the constraints that the Eemian data provide for the models and improve their predictive capability. These efforts have the potential to improve our ability to predict the contribution of the GrIS to sea-level rise in the coming decades to centuries. Educational and outreach activities include the training of two graduate students, inclusion of this research in summer teacher enrichment programs, a lecture series for graduate students and postdocs, and communication of the results through the news media. PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH Blunier, T., M. L. Bender, B. Barnett, and J. C. Von Fisher. "Planetary fertility during the past 400 ka based on the triple isotope composition of O2 in trapped gases from the Vostok ice core," Climate of the Past, v.8, 2012, p. 1509. Rubino, M., D. M. Etheridge, C. M. Trudinger, C. E. Allison, M. O. Battle, R. L. Langenfelds, L. P. Steele, M. Curran, M. Bender, J. W. C. White, T. M. Jenk, T. Blunier, and R. J. Francey. "Rubino, M., D. M. Etheridge, C. M. Trudinger, C. E. Allison, M. O. Battle, R. L. Langenfelds, L. P. Steele, M. Curran, M. Bender, J. W. C. White, T. M. Jenk, T. Blunier, and R. J. Francey," Journal of Geophysical Research-Atmospheres, v.118, 2013, p. doi:10.10. Dataset Arctic Greenland ice core Ice Sheet DataCite Metadata Store (German National Library of Science and Technology) Arctic Greenland Steele ENVELOPE(-60.710,-60.710,-70.980,-70.980)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic ANS
spellingShingle ANS
Bender, Michael
Collaborative Research: Ice Core Studies Reconstructing Greenland Climate During the Eemian and Beyond
topic_facet ANS
description The primary goal of this collaborative project between three institutions is to understand the extent and evolution of the Greenland Ice Sheet (GrIS) during the Eemian period (roughly 130,000 to 115,000 years ago, the last major interglacial period in Earth's history) and the deglaciation immediately preceding it ("Termination 2"). The GrIS is an important agent influencing sea level, and Arctic and global climate, on multiple timescales. Its dynamics need to be understood in the context of past climate changes, but there is little information available about the footprint, volume, and elevation of the GrIS prior to the last ice age due to the absence of continuous ice core records prior to 123,000 years ago. During the Eemian, the GrIS was perhaps half its present size, contributing on the order of 3 m to "excess" sea level rise. Characterizing the evolution of the GrIS during glacial termination 2 and the Eemian would improve our understanding of its dynamics, and enhance our ability to make projections of sea level rise during the coming centuries. Older ice does exist at the bottoms of previously drilled ice cores, but the extraction of age and climate information from this older ice is hampered by the fact that it is stratigraphically disturbed and, in many cases, contaminated with soil or bedrock material. These investigators propose several novel methods to date this disturbed and/or "dirty" ice and to extract information on climate and ice sheet extent. The investigators will combine their new measurements and other available data to develop a more complete history of the GrIS during termination 2 and the Eemian. They will work with ice sheet modelers to investigate the constraints that the Eemian data provide for the models and improve their predictive capability. These efforts have the potential to improve our ability to predict the contribution of the GrIS to sea-level rise in the coming decades to centuries. Educational and outreach activities include the training of two graduate students, inclusion of this research in summer teacher enrichment programs, a lecture series for graduate students and postdocs, and communication of the results through the news media. PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH Blunier, T., M. L. Bender, B. Barnett, and J. C. Von Fisher. "Planetary fertility during the past 400 ka based on the triple isotope composition of O2 in trapped gases from the Vostok ice core," Climate of the Past, v.8, 2012, p. 1509. Rubino, M., D. M. Etheridge, C. M. Trudinger, C. E. Allison, M. O. Battle, R. L. Langenfelds, L. P. Steele, M. Curran, M. Bender, J. W. C. White, T. M. Jenk, T. Blunier, and R. J. Francey. "Rubino, M., D. M. Etheridge, C. M. Trudinger, C. E. Allison, M. O. Battle, R. L. Langenfelds, L. P. Steele, M. Curran, M. Bender, J. W. C. White, T. M. Jenk, T. Blunier, and R. J. Francey," Journal of Geophysical Research-Atmospheres, v.118, 2013, p. doi:10.10.
format Dataset
author Bender, Michael
author_facet Bender, Michael
author_sort Bender, Michael
title Collaborative Research: Ice Core Studies Reconstructing Greenland Climate During the Eemian and Beyond
title_short Collaborative Research: Ice Core Studies Reconstructing Greenland Climate During the Eemian and Beyond
title_full Collaborative Research: Ice Core Studies Reconstructing Greenland Climate During the Eemian and Beyond
title_fullStr Collaborative Research: Ice Core Studies Reconstructing Greenland Climate During the Eemian and Beyond
title_full_unstemmed Collaborative Research: Ice Core Studies Reconstructing Greenland Climate During the Eemian and Beyond
title_sort collaborative research: ice core studies reconstructing greenland climate during the eemian and beyond
publisher NSF Arctic Data Center
publishDate 2015
url https://dx.doi.org/10.18739/a25x25d26
https://arcticdata.io/catalog/view/doi:10.18739/A25X25D26
long_lat ENVELOPE(-60.710,-60.710,-70.980,-70.980)
geographic Arctic
Greenland
Steele
geographic_facet Arctic
Greenland
Steele
genre Arctic
Greenland
ice core
Ice Sheet
genre_facet Arctic
Greenland
ice core
Ice Sheet
op_doi https://doi.org/10.18739/a25x25d26
_version_ 1766350005303508992