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Bachelor Thesis
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Stockholm University: Publications (DiVA)
Topic:
Physical Geography
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Naturgeografi
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Northern Sweden
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Document Type:
Bachelor Thesis
Content Provider:
Stockholm University: Publications (DiVA)
Topic:
Physical Geography
AND
Naturgeografi
Open Polar Keyword:
Northern Sweden
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Glacial lakes in the Torneträsk region, northern Sweden, are key to understandi...
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Representativitet av snödjup vid marktemperaturmätningar under snö för permafros...
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En uppdatering av årsringsvidd- och densitetskronologier vid Torneträsk till och...
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Landcover and periglacial landform mapping of a subarctic mountain area in the V...
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Inferring runoff generation processes in a discontinuous permafrost catchment in...
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The effect of snow-cover area change, precipitation and temperature on streamflo...
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Shallow near-surface lapse rates and their connection to glacier meteorology on...
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Multi-method based characterization of calving events at Sálajiegna Glacier - La...
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GIS, tracer test and water balance based hydrological analysis in Tarfala, North...
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Hydrological carbon transport in the Abiskojokka catchment area : The relationsh...
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Glacier front variatons in Sweden: 2015-2022
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Document Type
Bachelor Thesis
Author
Bodeving, Lena
1
Brandel, Malin
1
González Sánchez, Berta
1
Harney, Pawel
1
Houssais, Martin
1
Koivisto, Elias
1
Ploeg, Karlijn
1
Röja, Kristin
1
Schulthess, Martin
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Taveirne, Moon
1
Åkerström, Lisa
1
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Topic
Naturgeografi
Physical Geography
Glacier
2
Torneträsk
2
Acoustic
1
Acoustics
1
BTS
1
Calving
1
Climate change
1
DEM
1
Glacier front variation
1
Glaciers
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Sentinel-2
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Tarfala
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Temperature lapse rate
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Content Provider
Stockholm University: Publications (DiVA)
Geographic location
Tarfala
3
Arctic
2
Storglaciären
2
Torneträsk
2
Abisko
1
Antarctic
1
Glacial Lake
1
Greenland
1
Kring
1
Mårmaglaciären
1
Rautasjaure
1
Sulitelma
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Tärnaån
1
Valda
1
Våta
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Language
English
9
Swedish
2
Open Polar Keyword
Northern Sweden
permafrost
4
Tarfala
3
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Climate change
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1
Antarc*
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Antarctic
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Arktis*
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Fennoscandian
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Greenland
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Norra Sverige
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Subarctic
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Tornedalen
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glacier
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