An Intensive Observation of Calving at Helheim Glacier, East Greenland

Calving of glacial ice into the ocean from the Greenland Ice Sheet is an important component of global sea level rise. The calving process itself is relatively poorly observed, understood, and modeled; as such, it represents a bottleneck in improving future global sea level estimates in climate mode...

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Published in:Oceanography
Main Authors: Holland, David M., Voytenko, Denis, Christianson, Knut, Dixon, Timothy H., Mei, M. Jeffrey, Parizek, Byron R., Vaňková, Irena, Walker, Ryan T., Walter, Jacob I., Nicholls, Keith, Holland, Denise
Format: Text
Language:English
Published: 2016
Subjects:
Online Access:http://www.ncbi.nlm.nih.gov/pmc/articles/PMC7430530/
https://doi.org/10.5670/oceanog.2016.98
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spelling ftpubmed:oai:pubmedcentral.nih.gov:7430530 2023-05-15T16:03:36+02:00 An Intensive Observation of Calving at Helheim Glacier, East Greenland Holland, David M. Voytenko, Denis Christianson, Knut Dixon, Timothy H. Mei, M. Jeffrey Parizek, Byron R. Vaňková, Irena Walker, Ryan T. Walter, Jacob I. Nicholls, Keith Holland, Denise 2016-12-11 http://www.ncbi.nlm.nih.gov/pmc/articles/PMC7430530/ https://doi.org/10.5670/oceanog.2016.98 en eng http://www.ncbi.nlm.nih.gov/pmc/articles/PMC7430530/ http://dx.doi.org/10.5670/oceanog.2016.98 Oceanography (Wash D C) Article Text 2016 ftpubmed https://doi.org/10.5670/oceanog.2016.98 2020-08-23T00:35:12Z Calving of glacial ice into the ocean from the Greenland Ice Sheet is an important component of global sea level rise. The calving process itself is relatively poorly observed, understood, and modeled; as such, it represents a bottleneck in improving future global sea level estimates in climate models. We organized a pilot project to observe the calving process at Helheim Glacier in East Greenland in an effort to better understand it. During an intensive one-week survey, we deployed a suite of instrumentation including a terrestrial radar interferometer, GPS receivers, seismometers, tsunameters, and an automated weather station. This effort captured a calving process and measured various glaciological, oceanographic, and atmospheric parameters before, during, and after the event. One outcome of our observations is evidence that the calving process actually consists of a number of discrete events, spread out over time, in this instance over at least two days. This time span has implications for models of the process. Realistic projections of future global sea level will depend on accurate parametrization of calving, which will require more sustained observations. Text East Greenland glacier Greenland Ice Sheet PubMed Central (PMC) Greenland Oceanography 29 4 46 61
institution Open Polar
collection PubMed Central (PMC)
op_collection_id ftpubmed
language English
topic Article
spellingShingle Article
Holland, David M.
Voytenko, Denis
Christianson, Knut
Dixon, Timothy H.
Mei, M. Jeffrey
Parizek, Byron R.
Vaňková, Irena
Walker, Ryan T.
Walter, Jacob I.
Nicholls, Keith
Holland, Denise
An Intensive Observation of Calving at Helheim Glacier, East Greenland
topic_facet Article
description Calving of glacial ice into the ocean from the Greenland Ice Sheet is an important component of global sea level rise. The calving process itself is relatively poorly observed, understood, and modeled; as such, it represents a bottleneck in improving future global sea level estimates in climate models. We organized a pilot project to observe the calving process at Helheim Glacier in East Greenland in an effort to better understand it. During an intensive one-week survey, we deployed a suite of instrumentation including a terrestrial radar interferometer, GPS receivers, seismometers, tsunameters, and an automated weather station. This effort captured a calving process and measured various glaciological, oceanographic, and atmospheric parameters before, during, and after the event. One outcome of our observations is evidence that the calving process actually consists of a number of discrete events, spread out over time, in this instance over at least two days. This time span has implications for models of the process. Realistic projections of future global sea level will depend on accurate parametrization of calving, which will require more sustained observations.
format Text
author Holland, David M.
Voytenko, Denis
Christianson, Knut
Dixon, Timothy H.
Mei, M. Jeffrey
Parizek, Byron R.
Vaňková, Irena
Walker, Ryan T.
Walter, Jacob I.
Nicholls, Keith
Holland, Denise
author_facet Holland, David M.
Voytenko, Denis
Christianson, Knut
Dixon, Timothy H.
Mei, M. Jeffrey
Parizek, Byron R.
Vaňková, Irena
Walker, Ryan T.
Walter, Jacob I.
Nicholls, Keith
Holland, Denise
author_sort Holland, David M.
title An Intensive Observation of Calving at Helheim Glacier, East Greenland
title_short An Intensive Observation of Calving at Helheim Glacier, East Greenland
title_full An Intensive Observation of Calving at Helheim Glacier, East Greenland
title_fullStr An Intensive Observation of Calving at Helheim Glacier, East Greenland
title_full_unstemmed An Intensive Observation of Calving at Helheim Glacier, East Greenland
title_sort intensive observation of calving at helheim glacier, east greenland
publishDate 2016
url http://www.ncbi.nlm.nih.gov/pmc/articles/PMC7430530/
https://doi.org/10.5670/oceanog.2016.98
geographic Greenland
geographic_facet Greenland
genre East Greenland
glacier
Greenland
Ice Sheet
genre_facet East Greenland
glacier
Greenland
Ice Sheet
op_source Oceanography (Wash D C)
op_relation http://www.ncbi.nlm.nih.gov/pmc/articles/PMC7430530/
http://dx.doi.org/10.5670/oceanog.2016.98
op_doi https://doi.org/10.5670/oceanog.2016.98
container_title Oceanography
container_volume 29
container_issue 4
container_start_page 46
op_container_end_page 61
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