Ice Thickness from Jutulstraumen Glacier recorded with the airborne AWI UWB radar system, Antarctica ...

Focus of this project was to map the disturbances of the radar stratigraphy at the shear margins of the Jutulstraumen, a large outlet glacier in Dronning Maud Land (DML), Antarctica, as well as within its main trunk. This project will help to improve our understanding of the formation processes of s...

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Bibliographic Details
Main Authors: Franke, Steven, Jansen, Daniela, Helm, Veit
Format: Dataset
Language:English
Published: PANGAEA 2020
Subjects:
DML
Online Access:https://dx.doi.org/10.1594/pangaea.911475
https://doi.pangaea.de/10.1594/PANGAEA.911475
id ftdatacite:10.1594/pangaea.911475
record_format openpolar
spelling ftdatacite:10.1594/pangaea.911475 2024-09-30T14:26:49+00:00 Ice Thickness from Jutulstraumen Glacier recorded with the airborne AWI UWB radar system, Antarctica ... Franke, Steven Jansen, Daniela Helm, Veit 2020 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.911475 https://doi.pangaea.de/10.1594/PANGAEA.911475 en eng PANGAEA https://dx.doi.org/10.1002/esp.5203 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 AWI UWB Ice thickness Jutulstraumen radio-echo sounding Event label DATE/TIME Flight number Profile ID Paradigm ID Trace Number LONGITUDE LATITUDE Two-way traveltime Ice thickness, uncertainty POINT DISTANCE from start Aircraft Ice Thickness Radar EMR, MCoRDS P6-215_UWB_2018 POLAR 6 Dataset dataset 2020 ftdatacite https://doi.org/10.1594/pangaea.91147510.1002/esp.5203 2024-09-02T09:14:02Z Focus of this project was to map the disturbances of the radar stratigraphy at the shear margins of the Jutulstraumen, a large outlet glacier in Dronning Maud Land (DML), Antarctica, as well as within its main trunk. This project will help to improve our understanding of the formation processes of such disturbances around shear margins in active ice streams. A better understanding of the process itself will enable to analyse the observed structures in other parts of the ice sheets in terms of their deformation history. For JuRaS the profiles consist of parallel lines directed perpendicular to the flow direction of the main trunk of the Jutulstraumen, as well as profiles across an eastern tributary. Due to our fueling stop in Kohnen Station we were also able to collect a connecting radar line between the location of the EDML ice core to our main survey area, which is useful for referencing and dating reflections in our data and making connections to survey flights conducted in the 1990s, 2000s and later. ... : AWI Flight Campaign: P6-215_UWB_2018Project: JuRaS-2018Region: Antarctica, Dronning Maud Land, Jutulstraumen Ice Stream-Owner / PI: Daniela Jansen (AWI)Email address of the provider:steven.franke@awi.dedaniela.jansen@awi.de-Instrument used: AWI UWB (MCoRDS 5)Firn correction: none appliedVelocity profile: dielectric constant of 3.15 ( c = 1.68914e8 m/s )-Ice Thickness uncertainty:is the RMS of the the sum of the crossover mean of 62 intersections (= 24.7 m)and the error of the dielectric (1%).sqrt( (crossover_mean)^2 + ( (-ice_thickness/2) * 0.01 )^2 )-GPS data was acquired by four NovAtel DL-V3 GPS receivers operating at 20Hz -Level of focusing:focused SAR ... Dataset Antarc* Antarctica DML Dronning Maud Land ice core Jutulstraumen Glacier DataCite Dronning Maud Land Kohnen ENVELOPE(0.000,0.000,-75.000,-75.000) Kohnen Station ENVELOPE(0.000,0.000,-75.000,-75.000) Jutulstraumen ENVELOPE(-1.000,-1.000,-72.000,-72.000) Jutulstraumen Glacier ENVELOPE(-0.500,-0.500,-71.583,-71.583)
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic AWI UWB
Ice thickness
Jutulstraumen
radio-echo sounding
Event label
DATE/TIME
Flight number
Profile ID
Paradigm ID
Trace Number
LONGITUDE
LATITUDE
Two-way traveltime
Ice thickness, uncertainty
POINT DISTANCE from start
Aircraft
Ice Thickness Radar EMR, MCoRDS
P6-215_UWB_2018
POLAR 6
spellingShingle AWI UWB
Ice thickness
Jutulstraumen
radio-echo sounding
Event label
DATE/TIME
Flight number
Profile ID
Paradigm ID
Trace Number
LONGITUDE
LATITUDE
Two-way traveltime
Ice thickness, uncertainty
POINT DISTANCE from start
Aircraft
Ice Thickness Radar EMR, MCoRDS
P6-215_UWB_2018
POLAR 6
Franke, Steven
Jansen, Daniela
Helm, Veit
Ice Thickness from Jutulstraumen Glacier recorded with the airborne AWI UWB radar system, Antarctica ...
topic_facet AWI UWB
Ice thickness
Jutulstraumen
radio-echo sounding
Event label
DATE/TIME
Flight number
Profile ID
Paradigm ID
Trace Number
LONGITUDE
LATITUDE
Two-way traveltime
Ice thickness, uncertainty
POINT DISTANCE from start
Aircraft
Ice Thickness Radar EMR, MCoRDS
P6-215_UWB_2018
POLAR 6
description Focus of this project was to map the disturbances of the radar stratigraphy at the shear margins of the Jutulstraumen, a large outlet glacier in Dronning Maud Land (DML), Antarctica, as well as within its main trunk. This project will help to improve our understanding of the formation processes of such disturbances around shear margins in active ice streams. A better understanding of the process itself will enable to analyse the observed structures in other parts of the ice sheets in terms of their deformation history. For JuRaS the profiles consist of parallel lines directed perpendicular to the flow direction of the main trunk of the Jutulstraumen, as well as profiles across an eastern tributary. Due to our fueling stop in Kohnen Station we were also able to collect a connecting radar line between the location of the EDML ice core to our main survey area, which is useful for referencing and dating reflections in our data and making connections to survey flights conducted in the 1990s, 2000s and later. ... : AWI Flight Campaign: P6-215_UWB_2018Project: JuRaS-2018Region: Antarctica, Dronning Maud Land, Jutulstraumen Ice Stream-Owner / PI: Daniela Jansen (AWI)Email address of the provider:steven.franke@awi.dedaniela.jansen@awi.de-Instrument used: AWI UWB (MCoRDS 5)Firn correction: none appliedVelocity profile: dielectric constant of 3.15 ( c = 1.68914e8 m/s )-Ice Thickness uncertainty:is the RMS of the the sum of the crossover mean of 62 intersections (= 24.7 m)and the error of the dielectric (1%).sqrt( (crossover_mean)^2 + ( (-ice_thickness/2) * 0.01 )^2 )-GPS data was acquired by four NovAtel DL-V3 GPS receivers operating at 20Hz -Level of focusing:focused SAR ...
format Dataset
author Franke, Steven
Jansen, Daniela
Helm, Veit
author_facet Franke, Steven
Jansen, Daniela
Helm, Veit
author_sort Franke, Steven
title Ice Thickness from Jutulstraumen Glacier recorded with the airborne AWI UWB radar system, Antarctica ...
title_short Ice Thickness from Jutulstraumen Glacier recorded with the airborne AWI UWB radar system, Antarctica ...
title_full Ice Thickness from Jutulstraumen Glacier recorded with the airborne AWI UWB radar system, Antarctica ...
title_fullStr Ice Thickness from Jutulstraumen Glacier recorded with the airborne AWI UWB radar system, Antarctica ...
title_full_unstemmed Ice Thickness from Jutulstraumen Glacier recorded with the airborne AWI UWB radar system, Antarctica ...
title_sort ice thickness from jutulstraumen glacier recorded with the airborne awi uwb radar system, antarctica ...
publisher PANGAEA
publishDate 2020
url https://dx.doi.org/10.1594/pangaea.911475
https://doi.pangaea.de/10.1594/PANGAEA.911475
long_lat ENVELOPE(0.000,0.000,-75.000,-75.000)
ENVELOPE(0.000,0.000,-75.000,-75.000)
ENVELOPE(-1.000,-1.000,-72.000,-72.000)
ENVELOPE(-0.500,-0.500,-71.583,-71.583)
geographic Dronning Maud Land
Kohnen
Kohnen Station
Jutulstraumen
Jutulstraumen Glacier
geographic_facet Dronning Maud Land
Kohnen
Kohnen Station
Jutulstraumen
Jutulstraumen Glacier
genre Antarc*
Antarctica
DML
Dronning Maud Land
ice core
Jutulstraumen Glacier
genre_facet Antarc*
Antarctica
DML
Dronning Maud Land
ice core
Jutulstraumen Glacier
op_relation https://dx.doi.org/10.1002/esp.5203
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_doi https://doi.org/10.1594/pangaea.91147510.1002/esp.5203
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