Processed line aeromagnetic data over the Institute and Moller region (2010/11 season)

During the 2010/2011 Antarctic field season a collaborative NERC AFI (Antarctic Funding Initiative) project studying the basal boundary conditions of the Institute & Moller ice streams, West Antarctica, collected ~25,000 km of new high quality aeromagnetic data. Data were acquired using scintrex...

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Main Authors: Ferraccioli, Fausto, Jordan, Tom, Ross, Neil, Corr, Hugh, Leat, Philip, Bingham, Rob, Rippin, David, Le Brocq, Anne, Siegert, Martin
Format: Dataset
Language:English
Published: UK Polar Data Centre, Natural Environment Research Council, UK Research & Innovation 2020
Subjects:
Online Access:https://dx.doi.org/10.5285/03c3180b-97ef-4923-86e1-7ac9eab99497
https://data.bas.ac.uk/full-record.php?id=GB/NERC/BAS/PDC/01267
id ftdatacite:10.5285/03c3180b-97ef-4923-86e1-7ac9eab99497
record_format openpolar
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic "EARTH SCIENCE","SOLID EARTH","GEOMAGNETISM","MAGNETIC FIELD","MAGNETIC ANOMALIES"
Aerogeophysical
Aeromagnetics
Antarctic
spellingShingle "EARTH SCIENCE","SOLID EARTH","GEOMAGNETISM","MAGNETIC FIELD","MAGNETIC ANOMALIES"
Aerogeophysical
Aeromagnetics
Antarctic
Ferraccioli, Fausto
Jordan, Tom
Ross, Neil
Corr, Hugh
Leat, Philip
Bingham, Rob
Rippin, David
Le Brocq, Anne
Siegert, Martin
Processed line aeromagnetic data over the Institute and Moller region (2010/11 season)
topic_facet "EARTH SCIENCE","SOLID EARTH","GEOMAGNETISM","MAGNETIC FIELD","MAGNETIC ANOMALIES"
Aerogeophysical
Aeromagnetics
Antarctic
description During the 2010/2011 Antarctic field season a collaborative NERC AFI (Antarctic Funding Initiative) project studying the basal boundary conditions of the Institute & Moller ice streams, West Antarctica, collected ~25,000 km of new high quality aeromagnetic data. Data were acquired using scintrex cesium magnetometers mounted on the BAS aerogeophysical equiped Twin Otter. Data are provided as XYZ ASCII line data. Data were collected as part of the UK Natural Environment Research Council AFI grant NE/G013071/1. : IMAFI aeromagnetic data and details of survey design and location are presented in (Jordan et al., 2012). The dataset available here includes all channels from raw through to levelled, and draped products. Channel naming follows SCAR/ADMAP2 data release protocols. Key data processing steps are described below. Magnetic data channels and processing flow: MagR- Raw magnetic total field intensity data (nT). MagC- Compensated, or low pass filtered magnetic data (nT). Adjustments to compensate for aircraft roll, pitch and yaw were applied. RefField- Geomagnetic reference field value for which the magnetic data has been compensated. IGRF model 2010 as implemented in Geosoft (nT). MagRTC- Compensated magnetic value adjusted for Tip tanks (where used) and geomagnetic reference field values. MagRTC= MagR- RefField (nT). BCorr- Low pass filtered (60 minute) magnetic base station correction. MagBRTC- calculated as MagBRTC= MagRTC- Bcorr (nT). ACorr- Additional low pass filtering (30 fiducial cutoff) to account for any remnant noise in lines. MagF- Final mag value before levelling. (nT) MagL- Statistically levelled mag data. (nT) MagL_Drape Microlevelled data draped to a uniform level of 2100m above the bed topography, using the method of (Pilkington and Thurston, 2001). (nT) MagML- Microlevelled magnetic data following technique of (Ferraccioli et al., 1998). Note tie lines are not included in the microlevelled data channel. (nT) Basic Channels Line_no Line Number Flight ID Sequential flight number x x projected meters * y y projected meters * Lon Longitude WGS 1984, Lat Latitude WGS 1984, Height_WGS1984 Aircraft altitude (meters) in WGS 1984, Date Date of flight in time format e.g. 2006/01/08 Time Time (UTC) of flight e.g. 23:52:42.0 * Projected coordinates (x and y) are in Lambert conic conformal with two standard parallels defined as follows: Latitude of false origin: -82 Longitude of false origin: -14 Latitude of 1st standard parallel -84 Latitude of 2nd standard parallel -80 False easting 2000000 False northing 2000000
format Dataset
author Ferraccioli, Fausto
Jordan, Tom
Ross, Neil
Corr, Hugh
Leat, Philip
Bingham, Rob
Rippin, David
Le Brocq, Anne
Siegert, Martin
author_facet Ferraccioli, Fausto
Jordan, Tom
Ross, Neil
Corr, Hugh
Leat, Philip
Bingham, Rob
Rippin, David
Le Brocq, Anne
Siegert, Martin
author_sort Ferraccioli, Fausto
title Processed line aeromagnetic data over the Institute and Moller region (2010/11 season)
title_short Processed line aeromagnetic data over the Institute and Moller region (2010/11 season)
title_full Processed line aeromagnetic data over the Institute and Moller region (2010/11 season)
title_fullStr Processed line aeromagnetic data over the Institute and Moller region (2010/11 season)
title_full_unstemmed Processed line aeromagnetic data over the Institute and Moller region (2010/11 season)
title_sort processed line aeromagnetic data over the institute and moller region (2010/11 season)
publisher UK Polar Data Centre, Natural Environment Research Council, UK Research & Innovation
publishDate 2020
url https://dx.doi.org/10.5285/03c3180b-97ef-4923-86e1-7ac9eab99497
https://data.bas.ac.uk/full-record.php?id=GB/NERC/BAS/PDC/01267
long_lat ENVELOPE(-97.500,-97.500,-71.833,-71.833)
geographic Antarctic
West Antarctica
Thurston
geographic_facet Antarctic
West Antarctica
Thurston
genre Antarc*
Antarctic
Antarctica
West Antarctica
genre_facet Antarc*
Antarctic
Antarctica
West Antarctica
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op_rights Open Government Licence V3.0
http://www.nationalarchives.gov.uk/doc/open-government-licence/version/3
op_doi https://doi.org/10.5285/03c3180b-97ef-4923-86e1-7ac9eab99497
https://doi.org/10.5285/7946c497-72fc-41cb-a9b2-bf9980efe156
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spelling ftdatacite:10.5285/03c3180b-97ef-4923-86e1-7ac9eab99497 2023-05-15T13:37:36+02:00 Processed line aeromagnetic data over the Institute and Moller region (2010/11 season) Ferraccioli, Fausto Jordan, Tom Ross, Neil Corr, Hugh Leat, Philip Bingham, Rob Rippin, David Le Brocq, Anne Siegert, Martin 2020 text/plain https://dx.doi.org/10.5285/03c3180b-97ef-4923-86e1-7ac9eab99497 https://data.bas.ac.uk/full-record.php?id=GB/NERC/BAS/PDC/01267 en eng UK Polar Data Centre, Natural Environment Research Council, UK Research & Innovation https://dx.doi.org/10.5285/7946c497-72fc-41cb-a9b2-bf9980efe156 https://dx.doi.org/10.5285/bc55df03-cac4-4384-bfa7-57b65d969b48 https://dx.doi.org/10.1016/j.tecto.2012.09.010 https://dx.doi.org/10.1038/ngeo1468 https://dx.doi.org/10.1046/j.1365-2478.1998.00080.x https://dx.doi.org/10.1071/eg01095 https://dx.doi.org/10.1130/b30794.1 Open Government Licence V3.0 http://www.nationalarchives.gov.uk/doc/open-government-licence/version/3 "EARTH SCIENCE","SOLID EARTH","GEOMAGNETISM","MAGNETIC FIELD","MAGNETIC ANOMALIES" Aerogeophysical Aeromagnetics Antarctic dataset Aerogeophysical,Aeromagnetics,Antarctic Dataset 2020 ftdatacite https://doi.org/10.5285/03c3180b-97ef-4923-86e1-7ac9eab99497 https://doi.org/10.5285/7946c497-72fc-41cb-a9b2-bf9980efe156 https://doi.org/10.5285/bc55df03-cac4-4384-bfa7-57b65d969b48 https://doi.org/10.1016/j.tecto.2012.09.010 https://doi.org/10.1 2021-11-05T12:55:41Z During the 2010/2011 Antarctic field season a collaborative NERC AFI (Antarctic Funding Initiative) project studying the basal boundary conditions of the Institute & Moller ice streams, West Antarctica, collected ~25,000 km of new high quality aeromagnetic data. Data were acquired using scintrex cesium magnetometers mounted on the BAS aerogeophysical equiped Twin Otter. Data are provided as XYZ ASCII line data. Data were collected as part of the UK Natural Environment Research Council AFI grant NE/G013071/1. : IMAFI aeromagnetic data and details of survey design and location are presented in (Jordan et al., 2012). The dataset available here includes all channels from raw through to levelled, and draped products. Channel naming follows SCAR/ADMAP2 data release protocols. Key data processing steps are described below. Magnetic data channels and processing flow: MagR- Raw magnetic total field intensity data (nT). MagC- Compensated, or low pass filtered magnetic data (nT). Adjustments to compensate for aircraft roll, pitch and yaw were applied. RefField- Geomagnetic reference field value for which the magnetic data has been compensated. IGRF model 2010 as implemented in Geosoft (nT). MagRTC- Compensated magnetic value adjusted for Tip tanks (where used) and geomagnetic reference field values. MagRTC= MagR- RefField (nT). BCorr- Low pass filtered (60 minute) magnetic base station correction. MagBRTC- calculated as MagBRTC= MagRTC- Bcorr (nT). ACorr- Additional low pass filtering (30 fiducial cutoff) to account for any remnant noise in lines. MagF- Final mag value before levelling. (nT) MagL- Statistically levelled mag data. (nT) MagL_Drape Microlevelled data draped to a uniform level of 2100m above the bed topography, using the method of (Pilkington and Thurston, 2001). (nT) MagML- Microlevelled magnetic data following technique of (Ferraccioli et al., 1998). Note tie lines are not included in the microlevelled data channel. (nT) Basic Channels Line_no Line Number Flight ID Sequential flight number x x projected meters * y y projected meters * Lon Longitude WGS 1984, Lat Latitude WGS 1984, Height_WGS1984 Aircraft altitude (meters) in WGS 1984, Date Date of flight in time format e.g. 2006/01/08 Time Time (UTC) of flight e.g. 23:52:42.0 * Projected coordinates (x and y) are in Lambert conic conformal with two standard parallels defined as follows: Latitude of false origin: -82 Longitude of false origin: -14 Latitude of 1st standard parallel -84 Latitude of 2nd standard parallel -80 False easting 2000000 False northing 2000000 Dataset Antarc* Antarctic Antarctica West Antarctica DataCite Metadata Store (German National Library of Science and Technology) Antarctic West Antarctica Thurston ENVELOPE(-97.500,-97.500,-71.833,-71.833)