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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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 |
_version_ |
1766146737088495616 |