We present a first version of the Svalbard ice-free topography (SVIFT1.0) using a mass conserving approach for mapping glacier ice thickness. SVIFT1.0 is informed by more than 1 million point measurements, totalling more than 8,700 km of thickness profiles. SVIFT1.0 is publicly available and represents the geometric state around the year 2010. Our estimate for the total ice volume is 6,199 km3 , equivalent to 1.5-cm sea level rise. The thickness map suggests that 13% of the glacierized area is grounded below sea level. A complementary map of error estimates comprises uncertainties in the thickness surveys as well as in other input variables. Aggregated error estimates are used to define a likely ice-volume range of 5,200–7,300 km3 . The ice...
As part of ongoing work within the SvalGlac project aimed to obtain a reliable estimate of the total...
Estimating the long-term mass balance of the high-Arctic Svalbard archipelago is difficult due to th...
Satellite remote sensing based on optical or radar instruments has enable us to measure glacier-wide...
We present a first version of the Svalbard ice-free topography (SVIFT1.0) using a mass conserving ap...
International audienceWe present a first version of the Svalbard ice-free topography (SVIFT1.0) using...
The basal topography is largely unknown beneath most glaciers and ice caps, and many attempts have b...
Pedersenbreen is a small valley glacier (ca. 6 km2 in 2009), ending on land, located in north-wester...
We combined ground-based pulsed radar data collected in 2008-2009 with airborne radio-echo sounding ...
In this study, glacier ice thickness distribution and storage volume has been modelled for two glaci...
Svalbard tidewater glaciers are retreating, which will affect fjord circulation and ecosystems when ...
As part of ongoing work within the SvalGlac project aimed to obtain a reliable estimate of the total...
Estimating the long-term mass balance of the high-Arctic Svalbard archipelago is difficult due to th...
Satellite remote sensing based on optical or radar instruments has enable us to measure glacier-wide...
We present a first version of the Svalbard ice-free topography (SVIFT1.0) using a mass conserving ap...
International audienceWe present a first version of the Svalbard ice-free topography (SVIFT1.0) using...
The basal topography is largely unknown beneath most glaciers and ice caps, and many attempts have b...
Pedersenbreen is a small valley glacier (ca. 6 km2 in 2009), ending on land, located in north-wester...
We combined ground-based pulsed radar data collected in 2008-2009 with airborne radio-echo sounding ...
In this study, glacier ice thickness distribution and storage volume has been modelled for two glaci...
Svalbard tidewater glaciers are retreating, which will affect fjord circulation and ecosystems when ...
As part of ongoing work within the SvalGlac project aimed to obtain a reliable estimate of the total...
Estimating the long-term mass balance of the high-Arctic Svalbard archipelago is difficult due to th...
Satellite remote sensing based on optical or radar instruments has enable us to measure glacier-wide...