<?xml version="1.0" encoding="UTF-8"?><!--*** Generated from internal PANGAEA metadata schema by dif.xslt ***--><DIF xsi:schemaLocation="http://gcmd.gsfc.nasa.gov/Aboutus/xml/dif/ http://gcmd.gsfc.nasa.gov/Aboutus/xml/dif/dif_v9.4.xsd" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns="http://gcmd.gsfc.nasa.gov/Aboutus/xml/dif/">
<Entry_ID>PANGAEA_968088</Entry_ID>
<Entry_Title>GEM-2 ice and platelet total thickness measurements for transect AFIN_ATKA_20221206</Entry_Title>
<Data_Set_Citation>
<Dataset_Creator>Neudert, Mara; Arndt, Stefanie</Dataset_Creator>
<Dataset_Title>GEM-2 ice and platelet total thickness measurements for transect AFIN_ATKA_20221206</Dataset_Title>
<Dataset_Release_Date>2025-03-21</Dataset_Release_Date>
<Dataset_Publisher>PANGAEA</Dataset_Publisher>
<Data_Presentation_Form>Dataset</Data_Presentation_Form>
<Online_Resource>https://doi.pangaea.de/10.1594/PANGAEA.968088</Online_Resource>
</Data_Set_Citation>
<Personnel>
<Role>Investigator</Role>
<First_Name>Mara</First_Name>
<Last_Name>Neudert</Last_Name>
<Email>mneudert@awi.de</Email>
</Personnel>
<Discipline>
<Discipline_Name>Earth Science</Discipline_Name>
</Discipline>
<Parameters>
<Detailed_Variable>LATITUDE</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>LONGITUDE</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>DATE/TIME</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Distance</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Signal strength</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Sea ice and snow thickness</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Sea ice and snow conductivity</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Sub-ice platelet-layer conductivity</Detailed_Variable>
</Parameters>
<Parameters>
<Detailed_Variable>Sub-ice platelet-layer thickness</Detailed_Variable>
</Parameters>
<ISO_Topic_Category>geoscientificInformation</ISO_Topic_Category>
<Keyword>AFIN</Keyword>
<Keyword>AFIN_ATKA_20221206</Keyword>
<Keyword>ANT-Land_2022_AFIN</Keyword>
<Keyword>Atka Bay</Keyword>
<Keyword>DFG-SPP1158</Keyword>
<Keyword>Ground-based Electromagnetic Induction Sounding Device</Keyword>
<Keyword>Sea ice</Keyword>
<Keyword>Sub-ice platelet layer</Keyword>
<Sensor_Name>
<Long_Name>Ground-based Electromagnetic Induction Sounding Device</Long_Name>
</Sensor_Name>
<Sensor_Name>
<Long_Name>Multi-frequncy inversion, modified framework of the EMagPy (McLachlan et al., 2020)</Long_Name>
</Sensor_Name>
<Source_Name>
<Long_Name>NEUMAYER III</Long_Name>
</Source_Name>
<Temporal_Coverage>
<Start_Date>2022-12-06</Start_Date>
<Stop_Date>2022-12-06</Stop_Date>
</Temporal_Coverage>
<Data_Set_Progress>Complete</Data_Set_Progress>
<Spatial_Coverage>
<Southernmost_Latitude>-70.68372962</Southernmost_Latitude>
<Northernmost_Latitude>-70.55233888</Northernmost_Latitude>
<Westernmost_Longitude>-8.136683260999973</Westernmost_Longitude>
<Easternmost_Longitude>-7.8238966700000105</Easternmost_Longitude>
</Spatial_Coverage>
<Project>
<Short_Name>AFIN</Short_Name>
<Long_Name>Antarctic Fast Ice Network</Long_Name>
</Project>
<Project>
<Short_Name>SPP1158</Short_Name>
<Long_Name>Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas</Long_Name>
</Project>
<Project>
<Short_Name>AWI_SeaIce</Short_Name>
<Long_Name>Sea Ice Physics @ AWI</Long_Name>
</Project>
<Access_Constraints>unrestricted</Access_Constraints>
<Use_Constraints>CC-BY-4.0: Creative Commons Attribution 4.0 International</Use_Constraints>
<Data_Set_Language>English</Data_Set_Language>
<Data_Center>
<Data_Center_Name>
<Short_Name>PANGAEA</Short_Name>
<Long_Name>Data Publisher for Earth &amp; Environmental Science</Long_Name>
</Data_Center_Name>
<Data_Center_URL>https://www.pangaea.de/</Data_Center_URL>
<Personnel>
<Role>Data Center Contact</Role>
<First_Name>Michael</First_Name>
<Last_Name>Diepenbroek</Last_Name>
<Email>info@pangaea.de</Email>
<Contact_Address>
<Address>Leobener Str.</Address>
<City>Bremen</City>
<Province_or_State>Bremen</Province_or_State>
<Postal_Code>28359</Postal_Code>
<Country>Germany</Country>
</Contact_Address>
</Personnel>
</Data_Center>
<Distribution>
<Distribution_Media>online</Distribution_Media>
<Distribution_Size>1137375 data points</Distribution_Size>
<Distribution_Format>text/tab-separated-values</Distribution_Format>
</Distribution>
<Reference>Hunkeler, Priska A; Hendricks, Stefan; Hoppmann, Mario; Farquharson, Colin G; Kalscheuer, Thomas; Grab, Melchior; Kaufmann, Manuela S; Rabenstein, Lasse; Gerdes, Rüdiger (2016): Improved 1D inversions for sea ice thickness and conductivity from electromagnetic induction data: Inclusion of nonlinearities caused by passive bucking. Geophysics, 81(1), WA45-WA58, https://doi.org/10.1190/geo2015-0130.1</Reference>
<Reference>Hunkeler, Priska A; Hoppmann, Mario; Hendricks, Stefan; Kalscheuer, Thomas; Gerdes, Rüdiger (2016): A glimpse beneath Antarctic landfast sea ice: platelet-layer volume from multi-frequency electromagnetic induction sounding. Geophysical Research Letters, 43(1), 222-231, https://doi.org/10.1002/2015GL065074</Reference>
<Reference>McLachlan, Paul; Blanchy, Guillaume; Binley, Andrew (2021): EMagPy: Open-source standalone software for processing, forward modeling and inversion of electromagnetic induction data. Computers &amp; Geosciences, 146, 104561, https://doi.org/10.1016/j.cageo.2020.104561</Reference>
<Summary>The snow+ice thickness (distance from the snow surface to the consolidated ice-platelet ice interface) and the underlying platelet ice thickness was measured by the electromagnetic induction (EM) method. On all transects, we used a multi-frequency EM instrument sensor (GEM-2 by Geophex Ltd) towed on a small sled behind a snowmobile (Hunkeler et al, 2016b). The instrument includes a real-time data processing unit including a GPS receiver which communicates with a pocket PC that is operates the sensor and records the EM and GPS data streams. The GEM-2 is a multi-frequency sensor that can transmit multiple configurable frequencies in the kHz range simultaneously. The sensor setup during AFIN used 5 frequencies with an approximately logarithmic spacing throughout the frequency range of the sensor (1.53, 5.31, 18.33, 63.03, and 93.09 kHz). The transect measurements are based on a sensor calibration, where the GEM-2 was placed in a zero-conductivity environment on the ice shelf before and after each transect to correct for signal offsets in instrument drift. The snow+ice and platelet ice thickness and conductivity retrieval of the calibrated GEM-2 surveys data was done by multi-frequncy inversion in the modified framework of the EMagPy (McLachlan et al., 2020) accounting for the bucking coil bias (Hunkeler at al., 2016a). To validate the retrieved thicknesses, we used the snow depth, ice thickness and platelet ice thickness from the drill hole measurements coincident with the GEM-2 transects. The coincident drill hole data can be found here: doi:10.1594/PANGAEA.968459. For more details we refer to the paper by Neudert et al, 2024: Improved sub-Ice Platelet Layer Mapping with multi-frequency EM Induction Sounding, in review at Journal of Applied Geophysics, Elsevier. ** For all details see the full metadata description at "https://doi.pangaea.de/10.1594/PANGAEA.968088"!</Summary>
<Related_URL>
<URL>http://en.wikipedia.org/wiki/ISO_6709</URL>
<Description>LATITUDE</Description>
</Related_URL>
<Related_URL>
<URL>http://en.wikipedia.org/wiki/ISO_6709</URL>
<Description>LONGITUDE</Description>
</Related_URL>
<Related_URL>
<URL>http://en.wikipedia.org/wiki/ISO_8601</URL>
<Description>DATE/TIME</Description>
</Related_URL>
<Related_URL>
<URL>https://doi.org/10.1002/2015GL065074</URL>
<Description>A glimpse beneath Antarctic landfast sea ice: platelet-layer volume from multi-frequency electromagnetic induction sounding</Description>
</Related_URL>
<Related_URL>
<URL>https://doi.org/10.1016/j.cageo.2020.104561</URL>
<Description>EMagPy: Open-source standalone software for processing, forward modeling and inversion of electromagnetic induction data</Description>
</Related_URL>
<Related_URL>
<URL>https://doi.org/10.1190/geo2015-0130.1</URL>
<Description>Improved 1D inversions for sea ice thickness and conductivity from electromagnetic induction data: Inclusion of nonlinearities caused by passive bucking</Description>
</Related_URL>
<Related_URL>
<URL>https://doi.org/10.17815/jlsrf-2-152</URL>
<Description>NEUMAYER III</Description>
</Related_URL>
<Related_URL>
<URL>https://gepris.dfg.de/project/5472008</URL>
<Description>SPP1158</Description>
</Related_URL>
<Related_URL>
<URL>https://www.awi.de/en/science/climate-sciences/sea-ice-physics/projects/afin-antarctic-fast-ice-network.html</URL>
<Description>AFIN</Description>
</Related_URL>
<Related_URL>
<URL>https://www.awi.de/en/science/climate-sciences/sea-ice-physics.html</URL>
<Description>AWI_SeaIce</Description>
</Related_URL>
<Parent_DIF>PANGAEA_968041</Parent_DIF>
<Metadata_Name>DIF</Metadata_Name>
<Metadata_Version>9.4</Metadata_Version>
<DIF_Creation_Date>2025-03-21</DIF_Creation_Date>
<Last_DIF_Revision_Date>2026-07-14</Last_DIF_Revision_Date>
</DIF>
