Dataset - B2FIND

Bathymetric model beneath Nivl and Lazarev ice shelves, and across Astrid Rid...

Attached data comprise a bathymetric model of central Dronning Maud Land, including the seabed beneath the Nivl Ice Shelf and the Lazarev Ice Shelf, as well as the offshore...

Bathymetric model beneath Nivl and Lazarev ice shelves, and across Astrid Ridge

Attached data comprise a bathymetric model of central Dronning Maud Land, including the seabed beneath the Nivl Ice Shelf and the Lazarev Ice Shelf, as well as the offshore...

Modeled bathymetry beneath Roi Baudouin and Borchgrevink ice shelves, East An...

The lack of consistent and reliable estimates of the bathymetry beneath the Roi Baudouin and Borchgrevink ice shelves of Dronning Maud Land is addressed by inverting airborne...

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...

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...

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...

GEA IV 2013-15 radar ice thickness in eastern Dronning Maud Land

Ice thickness from radar data over eastern Dronning Maud Land, with geographical coordinates and dates of acquisition in 2013, 2014, and 2015. Airborne acquisition was completed...

Stable water isotopologues of arrays of high resolution 1 m snow cores from a...

A set of 1 m firn profiles was sampled in December 2018 across a traverse of ~ 100 km near Kohnen Station to quantify stratigraphic noise in high resolution isotope records. At...

5km-scale isotopic (δ18O) variability of the top-meter between locations B50 ...

Intermediate-scale (5 kilometers) isotopic composition of the top-meter of the snowpack around Kohnen station, Dronning-Maud Land, East-Antarctica. The snow was sampled with the...

100m-scale isotopic (δ18O) variability of the top-meter at location B52, East...

Small-scale (100 meter) isotopic composition of the top-meter of the snowpack around Kohnen station, Droning-Maud Land, East-Antarctica. The snow was sampled with the dual-tube...