<p>A 1:19,500 map of the Petunibukta region documents the spatial distribution of almost 300 colluvial and alluvial fans (together with their catchments) in the periglacial high-Arctic environment of Svalbard. Fan-shaped landforms were mapped using an orthophoto and digital elevation model generated from 2009 aerial photographs and a 2013 high-resolution satellite image using Geographic Information Systems. Four additional maps at a scale of 1:40,000 provide details about the morphometric characteristics of the studied fans: long- and cross-profiles, slope and aspect. Additionally, parameters such as fan and catchment area, relief, length, width, elevation (the lowest point at the fan toe, apex, and the highest point of the catchment bounda...
Location and climate factors governing morphological features of ice wedge polygons in arctic zone A...
Recent research suggests that Svalbard glaciers have retreated and thinned since the Little Ice Age....
Detailed investigations of the sediment-landform associations being actively created in modern-day p...
A 1:19,500 map of the Petunibukta region documents the spatial distribution of almost 300 colluvial ...
Fan-shaped landforms occur in all climatic regions on Earth. They have been extensively studied in m...
Fan-shaped landforms occur in all climatic regions on Earth. They have been extensively studied in m...
A 1:850 detailed map of the geomorphology of the Dynamisk Creek alluvial fan on Svalbard was produce...
Fan-shaped landforms occur in all climatic regions on Earth. They have been extensively studied in m...
The development and evolution of confined outwash fans in high Arctic regions depend on the rate of ...
<p>A 1:4000 scale map of the terrestrial margins of the foreland of Nordenskiöldbreen depicts a poly...
Abstract: The continental slopes of the pan-Arctic region exhibit a range of morphological expressio...
Erosional and sediment fluxes from Arctic mountains are lower than for temperate mountain ranges due...
Here we present a glacial and periglacial geomorphological map of a ∼6800 km2 region of central Trom...
Periglacial landforms on Earth reflect cold-climate conditions and are intimately related to process...
Climate change is amplified in the Arctic, and establishing baseline data for its current character ...
Location and climate factors governing morphological features of ice wedge polygons in arctic zone A...
Recent research suggests that Svalbard glaciers have retreated and thinned since the Little Ice Age....
Detailed investigations of the sediment-landform associations being actively created in modern-day p...
A 1:19,500 map of the Petunibukta region documents the spatial distribution of almost 300 colluvial ...
Fan-shaped landforms occur in all climatic regions on Earth. They have been extensively studied in m...
Fan-shaped landforms occur in all climatic regions on Earth. They have been extensively studied in m...
A 1:850 detailed map of the geomorphology of the Dynamisk Creek alluvial fan on Svalbard was produce...
Fan-shaped landforms occur in all climatic regions on Earth. They have been extensively studied in m...
The development and evolution of confined outwash fans in high Arctic regions depend on the rate of ...
<p>A 1:4000 scale map of the terrestrial margins of the foreland of Nordenskiöldbreen depicts a poly...
Abstract: The continental slopes of the pan-Arctic region exhibit a range of morphological expressio...
Erosional and sediment fluxes from Arctic mountains are lower than for temperate mountain ranges due...
Here we present a glacial and periglacial geomorphological map of a ∼6800 km2 region of central Trom...
Periglacial landforms on Earth reflect cold-climate conditions and are intimately related to process...
Climate change is amplified in the Arctic, and establishing baseline data for its current character ...
Location and climate factors governing morphological features of ice wedge polygons in arctic zone A...
Recent research suggests that Svalbard glaciers have retreated and thinned since the Little Ice Age....
Detailed investigations of the sediment-landform associations being actively created in modern-day p...