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Increased Ice Thinning over Svalbard measured by ICESat/ICESat-2 Laser Altimetry
We used spaceborne laser altimetry data from the ICESat and ICESat-2 missions to obtain ice elevation and mass change rates between 2003-2008 and 2019 over Svalbard. Elevation... -
Locations, outlines and ICESat-2 tracks of active lakes at the onset of the J...
We analysed a 6 year time series of displacement maps from Sentinel-1 SAR interferometry in the upstream region of Dronning Maud Lands Jutulstraumen Glacier (Antarctica). Our... -
Optical attenuation coefficients of glacier ice from 350-700 nm and raw irrad...
Optical attenuation coefficients of glacier ice from 350-700 nm were estimated from in-ice solar irradiance measured over the spectral range 350-900 nm and 12-124 cm depth... -
(Table A3) Raw irradiance values of glacier ice layer B (53-124 cm depth) fro...
This dataset contains the raw irradiance values that can be used to compute transmittance and attenuation coefficient, and are not interpolated or filtered, so the user can... -
(Table A3) Raw irradiance values of glacier ice layer A (12-77 cm depth) from...
This dataset contains the raw irradiance values that can be used to compute transmittance and attenuation coefficient, and are not interpolated or filtered, so the user can... -
(Table A2) Optical attenuation coefficients of glacier ice layer A (12-77 cm ...
Formal estimates of attenuation coefficient for Layer A, interpolated to 1 nm resolution using a convolution (Savitsky-Golay) filter, and reported for the useable range of... -
(Table A1) Optical attenuation coefficients of glacier ice layer B (53-124 cm...
Formal estimates of attenuation coefficient for Layer A, interpolated to 1 nm resolution using a convolution (Savitsky-Golay) filter, and reported for the useable range of...
