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Koch, Inka; Drews, Reinhard; Muhle, Lea Sophie; Franke, Steven; Jansen, Daniela; Oraschewski, Falk M; Spiegel, Heiko; Višnjević, Vjeran; Matsuoka, Kenichi; Pattyn, Frank; Eisen, Olaf (2023): Internal reflection horizons of ice shelves and ice rises in eastern Dronning Maud Land (East Antarctica) - Bewise 2012 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.950389, In: Koch, I et al. (2023): Internal reflection horizons of ice shelves and ice rises in eastern Dronning Maud Land (East Antarctica) from multisystem radio-echo sounding data [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.950383

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Abstract:
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 dynamics. These processes shape the ice stratigraphy, which can be imaged by radar and digitized in the form of internal reflection horizons (IRHs). Here, we synthesized IRHs from three airborne and ground-based surveys covering three ice rises and shelves in coastal eastern Dronning Maud Land (East Antarctica).
Keyword(s):
Airborne Radar; Antarctica; AWI UWB; Dronning Maud Land; ice rise; Ice shelf; Internal Reflection Horizon; IRH; radar
Funding:
German Research Foundation (DFG), grant/award no. DR 822/3-1: Emmy Noether Program DR 822/3-1
Coverage:
Median Latitude: -70.443651 * Median Longitude: 24.893490 * South-bound Latitude: -70.584578 * West-bound Longitude: 24.530833 * North-bound Latitude: -70.333173 * East-bound Longitude: 25.290865
Date/Time Start: 2012-12-08T00:00:00 * Date/Time End: 2012-12-12T00:00:00
Event(s):
BEWISE20121208 * Latitude Start: -70.460298 * Longitude Start: 24.785650 * Latitude End: -70.333983 * Longitude End: 24.732052 * Date/Time: 2012-12-08T00:00:00 * Location: Antarctica * Campaign: BE:WISE2012 (Be:Wise -The Buttressing Effect: Why ice shelves are essential) * Basis: Princess Elisabeth Station * Method/Device: Radar - Ground-based dipole antenna (GBDA)
BEWISE20121209 * Latitude Start: -70.346592 * Longitude Start: 24.629947 * Latitude End: -70.467075 * Longitude End: 24.629812 * Date/Time: 2012-12-09T00:00:00 * Location: Antarctica * Campaign: BE:WISE2012 (Be:Wise -The Buttressing Effect: Why ice shelves are essential) * Basis: Princess Elisabeth Station * Method/Device: Radar - Ground-based dipole antenna (GBDA)
BEWISE20121210 * Latitude Start: -70.467028 * Longitude Start: 24.629807 * Latitude End: -70.564345 * Longitude End: 24.923898 * Date/Time: 2012-12-10T00:00:00 * Location: Antarctica * Campaign: BE:WISE2012 (Be:Wise -The Buttressing Effect: Why ice shelves are essential) * Basis: Princess Elisabeth Station * Method/Device: Radar - Ground-based dipole antenna (GBDA)
Comment:
Dataset: Internal reflection horizions (IRHS) in the Roi Baudouin Ice Shelf (RBIS)
radar type: Ground-based dipole antennae
frequency: 20 MHz
coordinator: Reinhard Drews
tracing operator(s): Leah Sophie Muhle, Inka Koch
original file names: pp1 (08.12.2022), pp1_L1L2 (09.12.2022), L3L4 (10.12.2022), AlongFlow_CrossValley (11.12.2022), L5east (12.12.2022)
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Notes:
IRHs 1-9 are sorted according to depth with the shallowest layer having the smallest ID number, these IRHs were also verified at cross-points
IRHs 10 - 24 are unique IRHs not nescessarily sorted by depth
IRHs 13-14 were also verified at cross-points
Visual pattern matching has been applied when horizontal gaps occur in IRHs
basal pick is corrected to the first break
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1DATE/TIMEDate/TimeDrews, ReinhardGeocode
2Survey IDSurvey IDDrews, Reinhard
3Profile IDProfile IDDrews, Reinhard
4LONGITUDELongitudeDrews, ReinhardGeocode
5LATITUDELatitudeDrews, ReinhardGeocode – aquisition date
6Polar stereographic projection, XPolar stereo XmDrews, Reinhardproject 71 south (EPSG:3031)
7Polar stereographic projection, YPolar stereo YmDrews, Reinhardproject 71 south (EPSG:3031)
8Trace NumberTraceDrews, Reinhardof the radar transect along-track
9Pick Date/TimePick DateDrews, Reinharddate the IRHs were last picked or edited
10Two-way traveltime to ice baseTWT ice basesDrews, ReinhardRadar - Ground-based dipole antenna (GBDA)to the ice base in seconds from the surface
11Two-way traveltime to internal reflection horizonTWT IRHsDrews, ReinhardRadar - Ground-based dipole antenna (GBDA)IRH_01
12Two-way traveltime to internal reflection horizonTWT IRHsDrews, ReinhardRadar - Ground-based dipole antenna (GBDA)IRH_02
13Two-way traveltime to internal reflection horizonTWT IRHsDrews, ReinhardRadar - Ground-based dipole antenna (GBDA)IRH_03
14Two-way traveltime to internal reflection horizonTWT IRHsDrews, ReinhardRadar - Ground-based dipole antenna (GBDA)IRH_04
15Two-way traveltime to internal reflection horizonTWT IRHsDrews, ReinhardRadar - Ground-based dipole antenna (GBDA)IRH_05
16Two-way traveltime to internal reflection horizonTWT IRHsDrews, ReinhardRadar - Ground-based dipole antenna (GBDA)IRH_06
17Two-way traveltime to internal reflection horizonTWT IRHsDrews, ReinhardRadar - Ground-based dipole antenna (GBDA)IRH_07
18Two-way traveltime to internal reflection horizonTWT IRHsDrews, ReinhardRadar - Ground-based dipole antenna (GBDA)IRH_08
19Two-way traveltime to internal reflection horizonTWT IRHsDrews, ReinhardRadar - Ground-based dipole antenna (GBDA)IRH_09
20Two-way traveltime to internal reflection horizonTWT IRHsDrews, ReinhardRadar - Ground-based dipole antenna (GBDA)IRH_10
21Two-way traveltime to internal reflection horizonTWT IRHsDrews, ReinhardRadar - Ground-based dipole antenna (GBDA)IRH_11
22Two-way traveltime to internal reflection horizonTWT IRHsDrews, ReinhardRadar - Ground-based dipole antenna (GBDA)IRH_12
23Two-way traveltime to internal reflection horizonTWT IRHsDrews, ReinhardRadar - Ground-based dipole antenna (GBDA)IRH_13
24Two-way traveltime to internal reflection horizonTWT IRHsDrews, ReinhardRadar - Ground-based dipole antenna (GBDA)IRH_14
25Two-way traveltime to internal reflection horizonTWT IRHsDrews, ReinhardRadar - Ground-based dipole antenna (GBDA)IRH_15
26Two-way traveltime to internal reflection horizonTWT IRHsDrews, ReinhardRadar - Ground-based dipole antenna (GBDA)IRH_16
27Two-way traveltime to internal reflection horizonTWT IRHsDrews, ReinhardRadar - Ground-based dipole antenna (GBDA)IRH_17
28Two-way traveltime to internal reflection horizonTWT IRHsDrews, ReinhardRadar - Ground-based dipole antenna (GBDA)IRH_18
29Two-way traveltime to internal reflection horizonTWT IRHsDrews, ReinhardRadar - Ground-based dipole antenna (GBDA)IRH_19
30Two-way traveltime to internal reflection horizonTWT IRHsDrews, ReinhardRadar - Ground-based dipole antenna (GBDA)IRH_20
31Two-way traveltime to internal reflection horizonTWT IRHsDrews, ReinhardRadar - Ground-based dipole antenna (GBDA)IRH_21
32Two-way traveltime to internal reflection horizonTWT IRHsDrews, ReinhardRadar - Ground-based dipole antenna (GBDA)IRH_22
33Two-way traveltime to internal reflection horizonTWT IRHsDrews, ReinhardRadar - Ground-based dipole antenna (GBDA)IRH_23
34Two-way traveltime to internal reflection horizonTWT IRHsDrews, ReinhardRadar - Ground-based dipole antenna (GBDA)IRH_24
Change history:
2024-08-05T04:51:17 – Unit of Polar stereographic projection changed from "km" to "m".
Status:
Curation Level: Enhanced curation (CurationLevelC)
Size:
485890 data points

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