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author Franke, Steven
Helm, Veit
Hames, Oceane
Haas, Christian
author_facet Franke, Steven
Helm, Veit
Hames, Oceane
Haas, Christian
collection Datos científicos de ciencias marinas y ambientales
contents 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 AWI ultra-wideband microwave radar (UWBM) during the Antarctic season of 2022/23 (December 5th, 2022). The profiles extend across Atka Bay's snow-covered landfast sea ice in western Dronning Maud Land, East Antarctica. UWBM data was acquired to study snow drifts around icebergs and their radar signatures with a quad-polarized high-resolution radar system. The snow depth is defined as the snow between the snow-ice interface or the snow-flooded snow (slush or brine-wetted snow) interface.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_987055
institution PANGAEA
language en
publishDate 2025
publisher PANGAEA
record_format pangaea
spellingShingle Snow depth and snow-base backscatter intensity from AWI's airborne UWBM quad-polarized radar over Atka Bay (December 2022; ANTSI Project)
Franke, Steven
Helm, Veit
Hames, Oceane
Haas, Christian
AC; Aircraft; Antarctic Ice Sheet; ANTSI, MEP, Kottas-Aero; Atka Bay; AWI_SeaIce; AWI UWBM; Backscatter intensity ratio, snow-base interface, HH/VH; Backscatter intensity ratio, snow-base interface, VV/HV; Cryosphere; Dronning Maud Land; Echo backscatter; Event label; landfast sea ice; LATITUDE; LONGITUDE; P5_238_ANTSI_2022_2212051101; P5-238_ANTSI_2022; Polar 5; POLAR 5; Profile ID; radio-echo sounding; Sea ice; Sea Ice Physics @ AWI; snow depth; Snow depth; Trace Number
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 AWI ultra-wideband microwave radar (UWBM) during the Antarctic season of 2022/23 (December 5th, 2022). The profiles extend across Atka Bay's snow-covered landfast sea ice in western Dronning Maud Land, East Antarctica. UWBM data was acquired to study snow drifts around icebergs and their radar signatures with a quad-polarized high-resolution radar system. The snow depth is defined as the snow between the snow-ice interface or the snow-flooded snow (slush or brine-wetted snow) interface.
title Snow depth and snow-base backscatter intensity from AWI's airborne UWBM quad-polarized radar over Atka Bay (December 2022; ANTSI Project)
topic AC; Aircraft; Antarctic Ice Sheet; ANTSI, MEP, Kottas-Aero; Atka Bay; AWI_SeaIce; AWI UWBM; Backscatter intensity ratio, snow-base interface, HH/VH; Backscatter intensity ratio, snow-base interface, VV/HV; Cryosphere; Dronning Maud Land; Echo backscatter; Event label; landfast sea ice; LATITUDE; LONGITUDE; P5_238_ANTSI_2022_2212051101; P5-238_ANTSI_2022; Polar 5; POLAR 5; Profile ID; radio-echo sounding; Sea ice; Sea Ice Physics @ AWI; snow depth; Snow depth; Trace Number
url https://doi.org/10.1594/PANGAEA.987055