Evolution of supra-glacial lakes across the Greenland Ice Sheet

We used 268 cloud-free Moderate-resolution Imaging Spectroradiometer (MODIS) images spanning the melt seasons 2003 and 2005-2007 to study the seasonal evolution of supra-glacial lakes in three different regions of the Greenland ice sheet. Lake area estimates were obtained by developing an automated...

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Bibliographic Details
Main Author: Sundal, Aud
Other Authors: Shepherd, Andrew, Nienow, Pete
Format: Master Thesis
Language:English
Published: 2008
Subjects:
Online Access:http://hdl.handle.net/1842/2454
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author Sundal, Aud
author2 Shepherd, Andrew
Nienow, Pete
author_facet Sundal, Aud
author_sort Sundal, Aud
collection Edinburgh Research Archive (ERA - University of Edinburgh)
description We used 268 cloud-free Moderate-resolution Imaging Spectroradiometer (MODIS) images spanning the melt seasons 2003 and 2005-2007 to study the seasonal evolution of supra-glacial lakes in three different regions of the Greenland ice sheet. Lake area estimates were obtained by developing an automated classification method for their identification based on 250 m resolution MODIS surface reflectance data. Widespread supra-glacial lake formation and drainage are observed across the ice sheet, with a 2-3 weeks delay in the evolution of total supra-glacial lake area in the northern areas compared to the south-west. The onset of lake growth varies by up to one month inter-annually, and lakes form and drain at progressively higher altitudes during the melt season. The annual peak in total lake area is positively correlated with modelled annual runoff across all study areas, suggesting that local runoff governs seasonal variations in total supra-glacial lake area. Our results indicate that, in a future warmer climate (Meehl et al 2007), Greenland supra-glacial lakes can be expected to form at higher altitudes and over a longer time period than is presently the case, expanding the area and time period over which connections between the ice sheet surface and base may be established (Das et al 2008) and thereby potentially increasing ice sheet discharge (Zwally et al 2002).
format Master Thesis
genre Greenland
Ice Sheet
genre_facet Greenland
Ice Sheet
geographic Glacial Lake
Greenland
geographic_facet Glacial Lake
Greenland
id ftunivedinburgh:oai:era.ed.ac.uk:1842/2454
institution Open Polar
language English
long_lat ENVELOPE(-129.463,-129.463,58.259,58.259)
op_collection_id ftunivedinburgh
op_relation http://hdl.handle.net/1842/2454
publishDate 2008
record_format openpolar
spelling ftunivedinburgh:oai:era.ed.ac.uk:1842/2454 2025-04-27T14:29:46+00:00 Evolution of supra-glacial lakes across the Greenland Ice Sheet Sundal, Aud Shepherd, Andrew Nienow, Pete 05/12/2008 24573 bytes 1757653 bytes 326455 bytes application/pdf http://hdl.handle.net/1842/2454 en eng http://hdl.handle.net/1842/2454 MODIS supra-glacial lakes Greenland image classification GIS MSc Geographical Information Science Thesis or Dissertation Masters MSc Master of Science 2008 ftunivedinburgh 2025-04-01T03:41:08Z We used 268 cloud-free Moderate-resolution Imaging Spectroradiometer (MODIS) images spanning the melt seasons 2003 and 2005-2007 to study the seasonal evolution of supra-glacial lakes in three different regions of the Greenland ice sheet. Lake area estimates were obtained by developing an automated classification method for their identification based on 250 m resolution MODIS surface reflectance data. Widespread supra-glacial lake formation and drainage are observed across the ice sheet, with a 2-3 weeks delay in the evolution of total supra-glacial lake area in the northern areas compared to the south-west. The onset of lake growth varies by up to one month inter-annually, and lakes form and drain at progressively higher altitudes during the melt season. The annual peak in total lake area is positively correlated with modelled annual runoff across all study areas, suggesting that local runoff governs seasonal variations in total supra-glacial lake area. Our results indicate that, in a future warmer climate (Meehl et al 2007), Greenland supra-glacial lakes can be expected to form at higher altitudes and over a longer time period than is presently the case, expanding the area and time period over which connections between the ice sheet surface and base may be established (Das et al 2008) and thereby potentially increasing ice sheet discharge (Zwally et al 2002). Master Thesis Greenland Ice Sheet Edinburgh Research Archive (ERA - University of Edinburgh) Glacial Lake ENVELOPE(-129.463,-129.463,58.259,58.259) Greenland
spellingShingle MODIS
supra-glacial lakes
Greenland
image classification
GIS
MSc Geographical Information Science
Sundal, Aud
Evolution of supra-glacial lakes across the Greenland Ice Sheet
title Evolution of supra-glacial lakes across the Greenland Ice Sheet
title_full Evolution of supra-glacial lakes across the Greenland Ice Sheet
title_fullStr Evolution of supra-glacial lakes across the Greenland Ice Sheet
title_full_unstemmed Evolution of supra-glacial lakes across the Greenland Ice Sheet
title_short Evolution of supra-glacial lakes across the Greenland Ice Sheet
title_sort evolution of supra-glacial lakes across the greenland ice sheet
topic MODIS
supra-glacial lakes
Greenland
image classification
GIS
MSc Geographical Information Science
topic_facet MODIS
supra-glacial lakes
Greenland
image classification
GIS
MSc Geographical Information Science
url http://hdl.handle.net/1842/2454