Mapping tide-water glacier dynamics in East Greenland using Landsat data

Abstract Landsat multispectral scanner and thematic mapper images were co-registered For the Kangerdlugssuaq Fjord region in East Greenland and were used to map glacier drainage-basin areas, changes in the positions of tide-water glacier termini and to estimate surface velocities of the larger tide-...

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Published in:Journal of Glaciology
Main Author: Dwyer, John L.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1995
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000034900
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000034900
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spelling crcambridgeupr:10.1017/s0022143000034900 2024-04-28T08:15:56+00:00 Mapping tide-water glacier dynamics in East Greenland using Landsat data Dwyer, John L. 1995 http://dx.doi.org/10.1017/s0022143000034900 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000034900 en eng Cambridge University Press (CUP) Journal of Glaciology volume 41, issue 139, page 584-595 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1995 crcambridgeupr https://doi.org/10.1017/s0022143000034900 2024-04-09T06:55:10Z Abstract Landsat multispectral scanner and thematic mapper images were co-registered For the Kangerdlugssuaq Fjord region in East Greenland and were used to map glacier drainage-basin areas, changes in the positions of tide-water glacier termini and to estimate surface velocities of the larger tide-water glaciers. Statistics were compiled to document distance and area changes to glacier termini. The methodologies developed in this study are broadly applicable to the investigation of tide-water glaciers in other areas. The number of images available for consecutive years and the accuracy with which images are co-registered are key factors that influence the degree to which regional glacier dynamics can be characterized using remotely sensed data. Three domains of glacier state were interpreted: net increase in terminus area in the southern part of the study area, net loss of terminus area for glaciers in upper Kangerdlugssuaq Fjord and a slight loss of glacier terminus area northward from Ryberg Fjord. Local increases in the concentrations of drifting icebergs in the fjords coincide with the observed extension of glacier termini positions Ice-surface velocity estimates were derived for several glaciers using automated image cross-correlation techniques The velocity determined for Kangerdlugssuaq Gletscher is approximately 5.0 km a −1 and that for Kong Christian IV Gletscher is 0.9 km a −1 . The continuous presence of icebergs and brash ice in front of these glaciers indicates sustained rates of ice-front calving. Article in Journal/Newspaper Christian IV Gletscher East Greenland glacier Greenland Journal of Glaciology Cambridge University Press Journal of Glaciology 41 139 584 595
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Dwyer, John L.
Mapping tide-water glacier dynamics in East Greenland using Landsat data
topic_facet Earth-Surface Processes
description Abstract Landsat multispectral scanner and thematic mapper images were co-registered For the Kangerdlugssuaq Fjord region in East Greenland and were used to map glacier drainage-basin areas, changes in the positions of tide-water glacier termini and to estimate surface velocities of the larger tide-water glaciers. Statistics were compiled to document distance and area changes to glacier termini. The methodologies developed in this study are broadly applicable to the investigation of tide-water glaciers in other areas. The number of images available for consecutive years and the accuracy with which images are co-registered are key factors that influence the degree to which regional glacier dynamics can be characterized using remotely sensed data. Three domains of glacier state were interpreted: net increase in terminus area in the southern part of the study area, net loss of terminus area for glaciers in upper Kangerdlugssuaq Fjord and a slight loss of glacier terminus area northward from Ryberg Fjord. Local increases in the concentrations of drifting icebergs in the fjords coincide with the observed extension of glacier termini positions Ice-surface velocity estimates were derived for several glaciers using automated image cross-correlation techniques The velocity determined for Kangerdlugssuaq Gletscher is approximately 5.0 km a −1 and that for Kong Christian IV Gletscher is 0.9 km a −1 . The continuous presence of icebergs and brash ice in front of these glaciers indicates sustained rates of ice-front calving.
format Article in Journal/Newspaper
author Dwyer, John L.
author_facet Dwyer, John L.
author_sort Dwyer, John L.
title Mapping tide-water glacier dynamics in East Greenland using Landsat data
title_short Mapping tide-water glacier dynamics in East Greenland using Landsat data
title_full Mapping tide-water glacier dynamics in East Greenland using Landsat data
title_fullStr Mapping tide-water glacier dynamics in East Greenland using Landsat data
title_full_unstemmed Mapping tide-water glacier dynamics in East Greenland using Landsat data
title_sort mapping tide-water glacier dynamics in east greenland using landsat data
publisher Cambridge University Press (CUP)
publishDate 1995
url http://dx.doi.org/10.1017/s0022143000034900
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000034900
genre Christian IV Gletscher
East Greenland
glacier
Greenland
Journal of Glaciology
genre_facet Christian IV Gletscher
East Greenland
glacier
Greenland
Journal of Glaciology
op_source Journal of Glaciology
volume 41, issue 139, page 584-595
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000034900
container_title Journal of Glaciology
container_volume 41
container_issue 139
container_start_page 584
op_container_end_page 595
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