This paper examines the relationship between reflectance and physical characteristics of the snow cover in the Arctic. Field data were acquired for different snow and ice surfaces during a survey carried out at Ny-Ålesund, Svalbard, in spring 1998. In each measurement reflectance in the spectral range 350 - 2500 nm, snow data (including temperature, grain size and shape, density and water content), surface layer morphology, and vertical profile of the snow pack were recorded detailed analysis of reflectance based on the physical was performed. Field reflectance data were also re-sampled at the spectral intervals of Landsat TM to compare the ability of identifying different snow targets at discrete wavelength intervals. This analysis shows t...
Remote-sensing is an adequate tool for monitoring polar ice-sheets. In visible and infrared spectral...
International audienceThe optical-equivalent snow grain size affects the reflectivity of snow surfac...
International audienceArctic snow cover dynamics exhibit strong changes in terms of extent and durat...
The dataset holds measurements of reflected sunlight spectrum from snow and different snow free targ...
International audienceThe albedo of snow is determined in part by the size and shape of snow crystal...
The snow cover plays an important role not only for the whole climate system but also for tourism an...
The snow-covered ice sheets of Antarctica and Greenland reflect most of the incoming solar radiation...
In order to investigate influences on the reflectance of snow covered Arctic sea ice, a discrete ord...
The produced dataset (in csv format) contains snow spectral albedo as measured the field activity ca...
The significance of the polar regions for the Earth’s climate system and their observed amplified re...
The Arctic sea-ice surface albedo is observed by ground-based, airborne, and satellite instruments. ...
The broadband albedo of surface snow is determined both by the near-surface profile of the physical ...
The dataset contains laboratory spectral reflectance (350-2500 nm) measurements of natural snow samp...
A ground truth study was performed on first year fast ice in Kongsfjorden, Svalbard, during spring 1...
Thesis (Ph.D.)--University of Washington, 2017-03Snow cover is important for Earth’s surface energy ...
Remote-sensing is an adequate tool for monitoring polar ice-sheets. In visible and infrared spectral...
International audienceThe optical-equivalent snow grain size affects the reflectivity of snow surfac...
International audienceArctic snow cover dynamics exhibit strong changes in terms of extent and durat...
The dataset holds measurements of reflected sunlight spectrum from snow and different snow free targ...
International audienceThe albedo of snow is determined in part by the size and shape of snow crystal...
The snow cover plays an important role not only for the whole climate system but also for tourism an...
The snow-covered ice sheets of Antarctica and Greenland reflect most of the incoming solar radiation...
In order to investigate influences on the reflectance of snow covered Arctic sea ice, a discrete ord...
The produced dataset (in csv format) contains snow spectral albedo as measured the field activity ca...
The significance of the polar regions for the Earth’s climate system and their observed amplified re...
The Arctic sea-ice surface albedo is observed by ground-based, airborne, and satellite instruments. ...
The broadband albedo of surface snow is determined both by the near-surface profile of the physical ...
The dataset contains laboratory spectral reflectance (350-2500 nm) measurements of natural snow samp...
A ground truth study was performed on first year fast ice in Kongsfjorden, Svalbard, during spring 1...
Thesis (Ph.D.)--University of Washington, 2017-03Snow cover is important for Earth’s surface energy ...
Remote-sensing is an adequate tool for monitoring polar ice-sheets. In visible and infrared spectral...
International audienceThe optical-equivalent snow grain size affects the reflectivity of snow surfac...
International audienceArctic snow cover dynamics exhibit strong changes in terms of extent and durat...