_version_ 1867171344855072768
author Zuhr, Alexandra
Franke, Steven
Steinhage, Daniel
Helm, Veit
author_facet Zuhr, Alexandra
Franke, Steven
Steinhage, Daniel
Helm, Veit
collection Datos científicos de ciencias marinas y ambientales
contents 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 the 2023/24 season using the AWI ultra-wideband radar system in wideband mode (150–520 MHz). Information from firn core B52 are used for dating the IRHs, which span the period from 1209 to 2024. Surface mass balance is derived from each IRH for the mass per time between two consecutive IRHs.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_983768
institution PANGAEA
language en
publishDate 2026
publisher PANGAEA
record_format pangaea
spellingShingle Internal Reflection Horizons (IRHs) in western Dronning Maud Land, East Antarctica, from airborne radar surveys (IRH age = 0.047 ka)
Zuhr, Alexandra
Franke, Steven
Steinhage, Daniel
Helm, Veit
AC; Airborne Radar; Aircraft; AWI UWB; Depth of internal reflection horizon, below ice surface; Depth of internal reflection horizon, below ice surface, in water equivalents; Dronning Maud Land; East Antarctic plateau; Flight 15; Flight 16; Flight 7; Instrument; Internal Reflection Horizon; Internal reflection horizon, age; Internal reflection horizon, age, uncertainty; LATITUDE; LONGITUDE; P6_244_ANT_23_24_2311290701; P6_244_ANT_23_24_2312111501; P6_244_ANT_23_24_2312111602; P6-244_ANT_23_24; Paradigm ID; POLAR 6; Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas; Profile ID; Radar product; radio-echo sounding; Reference Elevation Model of Antarctica (REMA, Howat et al. 2019); Season; SPP1158; Surface elevation; Surface Mass Balance; Surface mass balance, in water equivalent; Surface mass balance, lower uncertainty limit; Surface mass balance, upper uncertainty limit; Trace Number; Two-way traveltime to internal reflection horizon
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 the 2023/24 season using the AWI ultra-wideband radar system in wideband mode (150–520 MHz). Information from firn core B52 are used for dating the IRHs, which span the period from 1209 to 2024. Surface mass balance is derived from each IRH for the mass per time between two consecutive IRHs.
title Internal Reflection Horizons (IRHs) in western Dronning Maud Land, East Antarctica, from airborne radar surveys (IRH age = 0.047 ka)
topic AC; Airborne Radar; Aircraft; AWI UWB; Depth of internal reflection horizon, below ice surface; Depth of internal reflection horizon, below ice surface, in water equivalents; Dronning Maud Land; East Antarctic plateau; Flight 15; Flight 16; Flight 7; Instrument; Internal Reflection Horizon; Internal reflection horizon, age; Internal reflection horizon, age, uncertainty; LATITUDE; LONGITUDE; P6_244_ANT_23_24_2311290701; P6_244_ANT_23_24_2312111501; P6_244_ANT_23_24_2312111602; P6-244_ANT_23_24; Paradigm ID; POLAR 6; Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas; Profile ID; Radar product; radio-echo sounding; Reference Elevation Model of Antarctica (REMA, Howat et al. 2019); Season; SPP1158; Surface elevation; Surface Mass Balance; Surface mass balance, in water equivalent; Surface mass balance, lower uncertainty limit; Surface mass balance, upper uncertainty limit; Trace Number; Two-way traveltime to internal reflection horizon
url https://doi.org/10.1594/PANGAEA.983768