Höjdförändringar på Lomonosovfonna, Svalbard, 1996-2012

The climate changes and the global warming have a great impact on the Arctic environments. This partially depends on that the albedo is getting lower when snow and ice is melting and exposes more and more dark surfaces of the land and sea. This leads to a feedback effect; the melting accelerates bec...

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Bibliographic Details
Main Author: Borg, Linnea
Format: Bachelor Thesis
Language:Swedish
Published: Uppsala universitet, Institutionen för geovetenskaper 2013
Subjects:
Online Access:http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-206198
id ftuppsalauniv:oai:DiVA.org:uu-206198
record_format openpolar
spelling ftuppsalauniv:oai:DiVA.org:uu-206198 2023-05-15T13:11:55+02:00 Höjdförändringar på Lomonosovfonna, Svalbard, 1996-2012 Borg, Linnea 2013 application/pdf http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-206198 swe swe Uppsala universitet, Institutionen för geovetenskaper Självständigt arbete 75 http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-206198 info:eu-repo/semantics/openAccess Earth and Related Environmental Sciences Geovetenskap och miljövetenskap Physical Geography Naturgeografi Student thesis info:eu-repo/semantics/bachelorThesis text 2013 ftuppsalauniv 2023-02-23T21:47:54Z The climate changes and the global warming have a great impact on the Arctic environments. This partially depends on that the albedo is getting lower when snow and ice is melting and exposes more and more dark surfaces of the land and sea. This leads to a feedback effect; the melting accelerates because dark surfaces attract more sun radiation. Because of the heating the glaciers in Arctic retreat. The purpose of this report is to obtain an eventual change in elevation on the glacier Lomonosovfonna that is located on Svalbard by comparing elevation data collected by NASA and GPS data from 1996-2012. The data was processed in ArcGIS and Matlab and the result is a change in elevation during the periods 1996-2012, 1996-2002 and 2002-2012. The result shows an average height decrease of Lomonosovfonna of -0,44 meters per year. When the result is reviewed, one can notice that both an increase and a decrease in height are observed on Lomonosovfonna. On the edge of the glacier, that border to Billefjorden, only a decrease in elevation is noticed. Some differences in elevation is very high in this area, and this can be due to three causes; the highest amount of melting occurs on the edges because of the higher air temperature at low elevation cause high melt, a calving have occurred or the difference is due to that the glacier is steepest in this area and therefore small position errors between measurements can cause big differences. The result also shows that the melting is accelerating, since the average melting of Lomonosovfonna was -0,26 meters per year during the period 1996-2002 and during the period 2002-2012 the melting had increased to -0,54 meters per year. The results are all in line with earlier measurements and reports and also with predictions for the climate. Klimatförändringarna och den globala uppvärmningen slår hårt mot Arktis och områdena där omkring. Detta beror till stor del av att när snö och is smälter så försvinner ljusa ytor och ersätts av mörkt hav och land – albedot sänks. Detta har en ... Bachelor Thesis albedo Arctic Arktis Arktis* Billefjorden glacier Global warming Svalbard Uppsala University: Publications (DiVA) Arctic Billefjorden ENVELOPE(16.417,16.417,78.563,78.563) Lomonosovfonna ENVELOPE(17.663,17.663,78.774,78.774) Svalbard
institution Open Polar
collection Uppsala University: Publications (DiVA)
op_collection_id ftuppsalauniv
language Swedish
topic Earth and Related Environmental Sciences
Geovetenskap och miljövetenskap
Physical Geography
Naturgeografi
spellingShingle Earth and Related Environmental Sciences
Geovetenskap och miljövetenskap
Physical Geography
Naturgeografi
Borg, Linnea
Höjdförändringar på Lomonosovfonna, Svalbard, 1996-2012
topic_facet Earth and Related Environmental Sciences
Geovetenskap och miljövetenskap
Physical Geography
Naturgeografi
description The climate changes and the global warming have a great impact on the Arctic environments. This partially depends on that the albedo is getting lower when snow and ice is melting and exposes more and more dark surfaces of the land and sea. This leads to a feedback effect; the melting accelerates because dark surfaces attract more sun radiation. Because of the heating the glaciers in Arctic retreat. The purpose of this report is to obtain an eventual change in elevation on the glacier Lomonosovfonna that is located on Svalbard by comparing elevation data collected by NASA and GPS data from 1996-2012. The data was processed in ArcGIS and Matlab and the result is a change in elevation during the periods 1996-2012, 1996-2002 and 2002-2012. The result shows an average height decrease of Lomonosovfonna of -0,44 meters per year. When the result is reviewed, one can notice that both an increase and a decrease in height are observed on Lomonosovfonna. On the edge of the glacier, that border to Billefjorden, only a decrease in elevation is noticed. Some differences in elevation is very high in this area, and this can be due to three causes; the highest amount of melting occurs on the edges because of the higher air temperature at low elevation cause high melt, a calving have occurred or the difference is due to that the glacier is steepest in this area and therefore small position errors between measurements can cause big differences. The result also shows that the melting is accelerating, since the average melting of Lomonosovfonna was -0,26 meters per year during the period 1996-2002 and during the period 2002-2012 the melting had increased to -0,54 meters per year. The results are all in line with earlier measurements and reports and also with predictions for the climate. Klimatförändringarna och den globala uppvärmningen slår hårt mot Arktis och områdena där omkring. Detta beror till stor del av att när snö och is smälter så försvinner ljusa ytor och ersätts av mörkt hav och land – albedot sänks. Detta har en ...
format Bachelor Thesis
author Borg, Linnea
author_facet Borg, Linnea
author_sort Borg, Linnea
title Höjdförändringar på Lomonosovfonna, Svalbard, 1996-2012
title_short Höjdförändringar på Lomonosovfonna, Svalbard, 1996-2012
title_full Höjdförändringar på Lomonosovfonna, Svalbard, 1996-2012
title_fullStr Höjdförändringar på Lomonosovfonna, Svalbard, 1996-2012
title_full_unstemmed Höjdförändringar på Lomonosovfonna, Svalbard, 1996-2012
title_sort höjdförändringar på lomonosovfonna, svalbard, 1996-2012
publisher Uppsala universitet, Institutionen för geovetenskaper
publishDate 2013
url http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-206198
long_lat ENVELOPE(16.417,16.417,78.563,78.563)
ENVELOPE(17.663,17.663,78.774,78.774)
geographic Arctic
Billefjorden
Lomonosovfonna
Svalbard
geographic_facet Arctic
Billefjorden
Lomonosovfonna
Svalbard
genre albedo
Arctic
Arktis
Arktis*
Billefjorden
glacier
Global warming
Svalbard
genre_facet albedo
Arctic
Arktis
Arktis*
Billefjorden
glacier
Global warming
Svalbard
op_relation Självständigt arbete
75
http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-206198
op_rights info:eu-repo/semantics/openAccess
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