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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Main Authors: Holland, Denise, Walter, Jacob I., Dixon, Timothy H., Parizek, Byron R., Mei, M. Jeffrey, Nicholls, Keith, Christianson, Knut, Vankova, Irena, Walker, Ryan T., Holland, David M., Voytenko, Denis
Format: Other/Unknown Material
Language:unknown
Published: 2016
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Online Access:http://hdl.handle.net/2060/20170003150
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record_format openpolar
spelling ftnasantrs:oai:casi.ntrs.nasa.gov:20170003150 2023-05-15T16:03:37+02:00 An Intensive Observation of Calving at Helheim Glacier, East Greenland Holland, Denise Walter, Jacob I. Dixon, Timothy H. Parizek, Byron R. Mei, M. Jeffrey Nicholls, Keith Christianson, Knut Vankova, Irena Walker, Ryan T. Holland, David M. Voytenko, Denis Unclassified, Unlimited, Publicly available December 2016 application/pdf http://hdl.handle.net/2060/20170003150 unknown Document ID: 20170003150 http://hdl.handle.net/2060/20170003150 Copyright, Public use permitted CASI Oceanography GSFC-E-DAA-TN40840 Oceanography (ISSN 1042-8275); 29; 4; 46-61 2016 ftnasantrs 2019-07-20T23:36:39Z 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, global positioning system (GPS) receivers, seismometers, tsunameters, and an automated weather station. We were fortunate to capture a calving process and to measure 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 an accurate parametrization of calving, and we argue that more sustained observations will be required to reach this objective. Other/Unknown Material East Greenland glacier Greenland Ice Sheet NASA Technical Reports Server (NTRS) Greenland
institution Open Polar
collection NASA Technical Reports Server (NTRS)
op_collection_id ftnasantrs
language unknown
topic Oceanography
spellingShingle Oceanography
Holland, Denise
Walter, Jacob I.
Dixon, Timothy H.
Parizek, Byron R.
Mei, M. Jeffrey
Nicholls, Keith
Christianson, Knut
Vankova, Irena
Walker, Ryan T.
Holland, David M.
Voytenko, Denis
An Intensive Observation of Calving at Helheim Glacier, East Greenland
topic_facet Oceanography
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, global positioning system (GPS) receivers, seismometers, tsunameters, and an automated weather station. We were fortunate to capture a calving process and to measure 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 an accurate parametrization of calving, and we argue that more sustained observations will be required to reach this objective.
format Other/Unknown Material
author Holland, Denise
Walter, Jacob I.
Dixon, Timothy H.
Parizek, Byron R.
Mei, M. Jeffrey
Nicholls, Keith
Christianson, Knut
Vankova, Irena
Walker, Ryan T.
Holland, David M.
Voytenko, Denis
author_facet Holland, Denise
Walter, Jacob I.
Dixon, Timothy H.
Parizek, Byron R.
Mei, M. Jeffrey
Nicholls, Keith
Christianson, Knut
Vankova, Irena
Walker, Ryan T.
Holland, David M.
Voytenko, Denis
author_sort Holland, Denise
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://hdl.handle.net/2060/20170003150
op_coverage Unclassified, Unlimited, Publicly available
geographic Greenland
geographic_facet Greenland
genre East Greenland
glacier
Greenland
Ice Sheet
genre_facet East Greenland
glacier
Greenland
Ice Sheet
op_source CASI
op_relation Document ID: 20170003150
http://hdl.handle.net/2060/20170003150
op_rights Copyright, Public use permitted
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