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Ice thickness of Dome Fuji region, Antarctica, recorded with the AWI airborne...
This data set contains the ice thickness data as recorded with the AWI airborne radar system (Nixdorf et al., 1999), operated with a 150 MHz pulse of 600 ns duration. Some 20000... -
Ice thickness of Dome Fuji region, Antarctica, recorded with the AWI airborne...
This data set contains the ice thickness data as recorded with the AWI airborne radar system (Nixdorf et al., 1999), operated with a 150 MHz pulse of 600 ns duration. Some 20000... -
Ice thickness of Dome Fuji region, Antarctica, recorded with the AWI airborne...
This data set contains the ice thickness data as recorded with the AWI airborne radar system (Nixdorf et al., 1999), operated with a 150 MHz pulse of 600 ns duration. Some 20000... -
Ice thickness of Dome Fuji region, Antarctica, recorded with the AWI airborne...
This data set contains the ice thickness data as recorded with the AWI airborne radar system (Nixdorf et al., 1999), operated with a 150 MHz pulse of 600 ns duration. Some 20000... -
Ice thickness of Dome Fuji region, Antarctica, recorded with the AWI airborne...
This data set contains the ice thickness data as recorded with the AWI airborne radar system (Nixdorf et al., 1999), operated with a 150 MHz pulse of 600 ns duration. Some 20000... -
Ice thickness of Dome Fuji region, Antarctica, recorded with the AWI airborne...
This data set contains the ice thickness data as recorded with the AWI airborne radar system (Nixdorf et al., 1999), operated with a 150 MHz pulse of 600 ns duration. Some 20000... -
Ice thickness of Dome Fuji region, Antarctica, recorded with the AWI airborne...
This data set contains the ice thickness data as recorded with the AWI airborne radar system (Nixdorf et al., 1999), operated with a 150 MHz pulse of 600 ns duration. Some 20000... -
Ice thickness of Dome Fuji region, Antarctica, recorded with the AWI airborne...
This data set contains the ice thickness data as recorded with the AWI airborne radar system (Nixdorf et al., 1999), operated with a 150 MHz pulse of 600 ns duration. Some 20000... -
Ice thickness of the Oldest Ice Reconnaissance survey, 2016/17, Dome Fuji - B...
This data set contains the ice thickness data as recorded with the AWI airborne radar system (Nixdorf et al., 1999), operated with a 150 MHz pulse of 600 ns duration. Some 20000... -
Ice thickness of the Oldest Ice Reconnaissance survey, 2016/17, Dome Fuji - B...
This data set contains the ice thickness data as recorded with the AWI airborne radar system (Nixdorf et al., 1999), operated with a 150 MHz pulse of 600 ns duration. Some 20000... -
Replication Data for: «Observing electrical fields and neutral winds with EIS...
Programming code for article «Observing electrical fields and neutral winds with EISCAT 3D» Measurements of height dependent electric field (E) and neutral wind (u) are... -
Replication Data for: Observing mesospheric turbulence with specular meteor r...
There are few observational techniques for measuring the distribution of kinetic energy within the mesosphere with a wide range of spatial and temporal scales. This study... -
Replication Data for: Modulation of Polar Mesospheric Summer Echoes (PMSE) wi...
Reproduction data for heating of Polar Mesospheric Summer Echoes measured with EISCAT VHF radar. Included in this dataset are all figures related to the paper in pdf format and... -
Ground-penetrating radar data (50MHz) and internal reflection horizons along ...
The internal stratigraphic structure of ice shelves forms by the interplay of ice dynamics, snow accumulation and basal melt. To infer accumulation and basal melt rates, we... -
Ground-penetrating radar data (50MHz) and internal reflection horizons along ...
The internal stratigraphic structure of ice shelves forms by the interplay of ice dynamics, snow accumulation and basal melt. To infer accumulation and basal melt rates, we... -
Phobos orbital measurement using MARSIS data
This dataset is composed of MARSIS measurements of Phobos's position. It combines the two tables present in Desage et al. (2024) paper on this subject. This data can be used as... -
Internal reflection horizons of ice shelves and ice rises in eastern Dronning...
Ice shelves regulate ice flow from the Antarctic ice sheet towards the ocean and their evolution depends on spatiotemporal patterns of surface accumulation, basal melt, and ice... -
Internal reflection horizons of ice shelves and ice rises in eastern Dronning...
Ice shelves regulate ice flow from the Antarctic ice sheet towards the ocean and their evolution depends on spatiotemporal patterns of surface accumulation, basal melt, and ice... -
Internal reflection horizons of ice shelves and ice rises in eastern Dronning...
Ice shelves regulate ice flow from the Antarctic ice sheet towards the ocean and their evolution depends on spatiotemporal patterns of surface accumulation, basal melt, and ice... -
Internal reflection horizons of ice shelves and ice rises in eastern Dronning...
Ice shelves regulate ice flow from the Antarctic ice sheet towards the ocean and their evolution depends on spatiotemporal patterns of surface accumulation, basal melt, and ice...
