(Table 1) Basin area, average late-summer speedup, number of sinks and runoff of West Greenland Ice Sheet catchments ...

We use interferometric synthetic aperture radar observations recorded in a land-terminating sector of western Greenland to characterise the ice sheet surface hydrology and to quantify spatial variations in the seasonality of ice sheet flow. Our data reveal a non-uniform pattern of late-summer ice sp...

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Bibliographic Details
Main Authors: Palmer, Steven J, Shepherd, Andrew, Nienow, Peter, Joughin, Ian
Format: Dataset
Language:English
Published: PANGAEA 2011
Subjects:
IPY
Online Access:https://dx.doi.org/10.1594/pangaea.817850
https://doi.pangaea.de/10.1594/PANGAEA.817850
id ftdatacite:10.1594/pangaea.817850
record_format openpolar
spelling ftdatacite:10.1594/pangaea.817850 2024-09-15T18:07:45+00:00 (Table 1) Basin area, average late-summer speedup, number of sinks and runoff of West Greenland Ice Sheet catchments ... Palmer, Steven J Shepherd, Andrew Nienow, Peter Joughin, Ian 2011 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.817850 https://doi.pangaea.de/10.1594/PANGAEA.817850 en eng PANGAEA https://dx.doi.org/10.1016/j.epsl.2010.12.037 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Event label Latitude of event Longitude of event Name Area Percentage Number Runoff Satellite remote sensing International Polar Year 2007-2008 IPY dataset Supplementary Dataset Dataset 2011 ftdatacite https://doi.org/10.1594/pangaea.81785010.1016/j.epsl.2010.12.037 2024-08-01T11:01:20Z We use interferometric synthetic aperture radar observations recorded in a land-terminating sector of western Greenland to characterise the ice sheet surface hydrology and to quantify spatial variations in the seasonality of ice sheet flow. Our data reveal a non-uniform pattern of late-summer ice speedup that, in places, extends over 100 km inland. We show that the degree of late-summer speedup is positively correlated with modelled runoff within the 10 glacier catchments of our survey, and that the pattern of late-summer speedup follows that of water routed at the ice sheet surface. In late-summer, ice within the largest catchment flows on average 48% faster than during winter, whereas changes in smaller catchments are less pronounced. Our observations show that the routing of seasonal runoff at the ice sheet surface plays an important role in shaping the magnitude and extent of seasonal ice sheet speedup. ... : Positions of catchments approximate. Data extracted in the frame of a joint ICSTI/PANGAEA IPY effort, see http://doi.pangaea.de/10.1594/PANGAEA.150150 ... Dataset glacier Greenland Ice Sheet International Polar Year IPY DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Event label
Latitude of event
Longitude of event
Name
Area
Percentage
Number
Runoff
Satellite remote sensing
International Polar Year 2007-2008 IPY
spellingShingle Event label
Latitude of event
Longitude of event
Name
Area
Percentage
Number
Runoff
Satellite remote sensing
International Polar Year 2007-2008 IPY
Palmer, Steven J
Shepherd, Andrew
Nienow, Peter
Joughin, Ian
(Table 1) Basin area, average late-summer speedup, number of sinks and runoff of West Greenland Ice Sheet catchments ...
topic_facet Event label
Latitude of event
Longitude of event
Name
Area
Percentage
Number
Runoff
Satellite remote sensing
International Polar Year 2007-2008 IPY
description We use interferometric synthetic aperture radar observations recorded in a land-terminating sector of western Greenland to characterise the ice sheet surface hydrology and to quantify spatial variations in the seasonality of ice sheet flow. Our data reveal a non-uniform pattern of late-summer ice speedup that, in places, extends over 100 km inland. We show that the degree of late-summer speedup is positively correlated with modelled runoff within the 10 glacier catchments of our survey, and that the pattern of late-summer speedup follows that of water routed at the ice sheet surface. In late-summer, ice within the largest catchment flows on average 48% faster than during winter, whereas changes in smaller catchments are less pronounced. Our observations show that the routing of seasonal runoff at the ice sheet surface plays an important role in shaping the magnitude and extent of seasonal ice sheet speedup. ... : Positions of catchments approximate. Data extracted in the frame of a joint ICSTI/PANGAEA IPY effort, see http://doi.pangaea.de/10.1594/PANGAEA.150150 ...
format Dataset
author Palmer, Steven J
Shepherd, Andrew
Nienow, Peter
Joughin, Ian
author_facet Palmer, Steven J
Shepherd, Andrew
Nienow, Peter
Joughin, Ian
author_sort Palmer, Steven J
title (Table 1) Basin area, average late-summer speedup, number of sinks and runoff of West Greenland Ice Sheet catchments ...
title_short (Table 1) Basin area, average late-summer speedup, number of sinks and runoff of West Greenland Ice Sheet catchments ...
title_full (Table 1) Basin area, average late-summer speedup, number of sinks and runoff of West Greenland Ice Sheet catchments ...
title_fullStr (Table 1) Basin area, average late-summer speedup, number of sinks and runoff of West Greenland Ice Sheet catchments ...
title_full_unstemmed (Table 1) Basin area, average late-summer speedup, number of sinks and runoff of West Greenland Ice Sheet catchments ...
title_sort (table 1) basin area, average late-summer speedup, number of sinks and runoff of west greenland ice sheet catchments ...
publisher PANGAEA
publishDate 2011
url https://dx.doi.org/10.1594/pangaea.817850
https://doi.pangaea.de/10.1594/PANGAEA.817850
genre glacier
Greenland
Ice Sheet
International Polar Year
IPY
genre_facet glacier
Greenland
Ice Sheet
International Polar Year
IPY
op_relation https://dx.doi.org/10.1016/j.epsl.2010.12.037
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.81785010.1016/j.epsl.2010.12.037
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