Dataset - B2FIND

Snow depth and snow-base backscatter intensity from AWI's airborne UWBM quad-...

This dataset contains snow depth and snow-base backscatter intensity for four polarizations (HH, VH, VV, HV) derived from airborne radar data acquired using the quad-polarized...

Internal Reflection Horizons (IRHs) in western Dronning Maud Land, East Antar...

We present five internal reflection horizons (IRHs) derived from airborne radar data in western Dronning Maud Land on the East Antarctic Plateau. The data were collected during...

Internal Reflection Horizons (IRHs) in western Dronning Maud Land, East Antar...

We present five internal reflection horizons (IRHs) derived from airborne radar data in western Dronning Maud Land on the East Antarctic Plateau. The data were collected during...

Internal Reflection Horizons (IRHs) in western Dronning Maud Land, East Antar...

We present five internal reflection horizons (IRHs) derived from airborne radar data in western Dronning Maud Land on the East Antarctic Plateau. The data were collected during...

Internal Reflection Horizons (IRHs) in western Dronning Maud Land, East Antar...

We present five internal reflection horizons (IRHs) derived from airborne radar data in western Dronning Maud Land on the East Antarctic Plateau. The data were collected during...

Internal Reflection Horizons (IRHs) in western Dronning Maud Land, East Antar...

We present five internal reflection horizons (IRHs) derived from airborne radar data in western Dronning Maud Land on the East Antarctic Plateau. The data were collected during...

Ice Thickness from downstream of the EastGRIP ice core site, North East Green...

This project aims to acquire airborne data with AWI's UWB (ultrawideband) ice-penetrating radar to extend the knowledge of detailed subglacial topography downstream of the...

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...

Locations and thickness of sediment-laden basal ice zones at Jutulstraumen Gl...

Understanding the material properties and physical conditions of basal ice is crucial for a comprehensive understanding of Antarctic ice-sheet dynamics. Yet, direct data are...

Ice thickness from the coast of Dronning Maud Land (Antarctica), recorded 201...

Ice thickness from the coast of Dronning Maud Land (Antarctica), recorded 2018/19 with the AWI UWB radar systemThis project aims to acquire airborne data with AWI's UWB...