A DEM of the 2010 surface topography of Storglaciären, Sweden

During the summer of 2010 the surface elevation of Storglaciären in northern Sweden was measured using high-precision GNSS and reflectorless Total Station surveys. The DEM created from these data contain less noise than those created from orthophotographic methods over snow covered glaciers and is t...

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Main Author: Andrew Mercer
Format: Article in Journal/Newspaper
Language:unknown
Subjects:
Online Access:http://hdl.handle.net/10.1080/17445647.2015.1131754
id ftrepec:oai:RePEc:taf:tjomxx:v:12:y:2016:i:5:p:1112-1118
record_format openpolar
spelling ftrepec:oai:RePEc:taf:tjomxx:v:12:y:2016:i:5:p:1112-1118 2023-05-15T17:44:30+02:00 A DEM of the 2010 surface topography of Storglaciären, Sweden Andrew Mercer http://hdl.handle.net/10.1080/17445647.2015.1131754 unknown http://hdl.handle.net/10.1080/17445647.2015.1131754 article ftrepec 2020-12-04T13:41:49Z During the summer of 2010 the surface elevation of Storglaciären in northern Sweden was measured using high-precision GNSS and reflectorless Total Station surveys. The DEM created from these data contain less noise than those created from orthophotographic methods over snow covered glaciers and is therefore smoother, with fewer erroneous features in the data. The principal, though not sole, intended use for the DEM is in the calculation of surface mass balance, which has influenced decisions on what constitutes a functional part of a glacier, leading to the exclusion of features such as snow aprons and perennial ice above the bergschrund. Other peripheral features have changed since the previous, aerial survey from 1999 leading to a reduction in size of approximately 0.17 km2. Article in Journal/Newspaper Northern Sweden RePEc (Research Papers in Economics) Storglaciären ENVELOPE(18.560,18.560,67.904,67.904)
institution Open Polar
collection RePEc (Research Papers in Economics)
op_collection_id ftrepec
language unknown
description During the summer of 2010 the surface elevation of Storglaciären in northern Sweden was measured using high-precision GNSS and reflectorless Total Station surveys. The DEM created from these data contain less noise than those created from orthophotographic methods over snow covered glaciers and is therefore smoother, with fewer erroneous features in the data. The principal, though not sole, intended use for the DEM is in the calculation of surface mass balance, which has influenced decisions on what constitutes a functional part of a glacier, leading to the exclusion of features such as snow aprons and perennial ice above the bergschrund. Other peripheral features have changed since the previous, aerial survey from 1999 leading to a reduction in size of approximately 0.17 km2.
format Article in Journal/Newspaper
author Andrew Mercer
spellingShingle Andrew Mercer
A DEM of the 2010 surface topography of Storglaciären, Sweden
author_facet Andrew Mercer
author_sort Andrew Mercer
title A DEM of the 2010 surface topography of Storglaciären, Sweden
title_short A DEM of the 2010 surface topography of Storglaciären, Sweden
title_full A DEM of the 2010 surface topography of Storglaciären, Sweden
title_fullStr A DEM of the 2010 surface topography of Storglaciären, Sweden
title_full_unstemmed A DEM of the 2010 surface topography of Storglaciären, Sweden
title_sort dem of the 2010 surface topography of storglaciären, sweden
url http://hdl.handle.net/10.1080/17445647.2015.1131754
long_lat ENVELOPE(18.560,18.560,67.904,67.904)
geographic Storglaciären
geographic_facet Storglaciären
genre Northern Sweden
genre_facet Northern Sweden
op_relation http://hdl.handle.net/10.1080/17445647.2015.1131754
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