New Antarctic gravity anomaly grid for enhanced geodetic and geophysical studies in Antarctica

Gravity surveying is challenging in Antarctica because of its hostile environment and inaccessibility. Nevertheless, many ground-based, airborne, and shipborne gravity campaigns have been completed by the geophysical and geodetic communities since the 1980s. We present the first modern Antarctic-wid...

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Main Authors: Scheinert, Mirko, Ferracioli, Fausto, Schwabe, Joachim, Bell, Robin E., Studinger, Michael, Damaske, Detlef, Jokat, Wilfried, Aleshkova, Nadja, Jordan, Tom, Blankenship, Donald, Damiani, Theresa, Young, Duncan, Cochran, James R., Richter, Tom
Format: Article in Journal/Newspaper
Language:English
Published: 2016
Subjects:
Online Access:https://doi.org/10.7916/d8-fykv-aq24
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spelling ftcolumbiauniv:oai:academiccommons.columbia.edu:10.7916/d8-fykv-aq24 2023-05-15T13:53:34+02:00 New Antarctic gravity anomaly grid for enhanced geodetic and geophysical studies in Antarctica Scheinert, Mirko Ferracioli, Fausto Schwabe, Joachim Bell, Robin E. Studinger, Michael Damaske, Detlef Jokat, Wilfried Aleshkova, Nadja Jordan, Tom Blankenship, Donald Damiani, Theresa Young, Duncan Cochran, James R. Richter, Tom 2016 https://doi.org/10.7916/d8-fykv-aq24 English eng https://doi.org/10.7916/d8-fykv-aq24 Geophysics Geodesy Gravity--Measurement Gravity anomalies Articles 2016 ftcolumbiauniv https://doi.org/10.7916/d8-fykv-aq24 2019-07-06T22:19:53Z Gravity surveying is challenging in Antarctica because of its hostile environment and inaccessibility. Nevertheless, many ground-based, airborne, and shipborne gravity campaigns have been completed by the geophysical and geodetic communities since the 1980s. We present the first modern Antarctic-wide gravity data compilation derived from 13 million data points covering an area of 10 million km2, which corresponds to 73% coverage of the continent. The remove-compute-restore technique was applied for gridding, which facilitated leveling of the different gravity data sets with respect to an Earth gravity model derived from satellite data alone. The resulting free-air and Bouguer gravity anomaly grids of 10 km resolution are publicly available. These grids will enable new high-resolution combined Earth gravity models to be derived and represent a major step forward toward solving the geodetic polar data gap problem. They provide a new tool to investigate continental-scale lithospheric structure and geological evolution of Antarctica. Article in Journal/Newspaper Antarc* Antarctic Antarctica Columbia University: Academic Commons Antarctic
institution Open Polar
collection Columbia University: Academic Commons
op_collection_id ftcolumbiauniv
language English
topic Geophysics
Geodesy
Gravity--Measurement
Gravity anomalies
spellingShingle Geophysics
Geodesy
Gravity--Measurement
Gravity anomalies
Scheinert, Mirko
Ferracioli, Fausto
Schwabe, Joachim
Bell, Robin E.
Studinger, Michael
Damaske, Detlef
Jokat, Wilfried
Aleshkova, Nadja
Jordan, Tom
Blankenship, Donald
Damiani, Theresa
Young, Duncan
Cochran, James R.
Richter, Tom
New Antarctic gravity anomaly grid for enhanced geodetic and geophysical studies in Antarctica
topic_facet Geophysics
Geodesy
Gravity--Measurement
Gravity anomalies
description Gravity surveying is challenging in Antarctica because of its hostile environment and inaccessibility. Nevertheless, many ground-based, airborne, and shipborne gravity campaigns have been completed by the geophysical and geodetic communities since the 1980s. We present the first modern Antarctic-wide gravity data compilation derived from 13 million data points covering an area of 10 million km2, which corresponds to 73% coverage of the continent. The remove-compute-restore technique was applied for gridding, which facilitated leveling of the different gravity data sets with respect to an Earth gravity model derived from satellite data alone. The resulting free-air and Bouguer gravity anomaly grids of 10 km resolution are publicly available. These grids will enable new high-resolution combined Earth gravity models to be derived and represent a major step forward toward solving the geodetic polar data gap problem. They provide a new tool to investigate continental-scale lithospheric structure and geological evolution of Antarctica.
format Article in Journal/Newspaper
author Scheinert, Mirko
Ferracioli, Fausto
Schwabe, Joachim
Bell, Robin E.
Studinger, Michael
Damaske, Detlef
Jokat, Wilfried
Aleshkova, Nadja
Jordan, Tom
Blankenship, Donald
Damiani, Theresa
Young, Duncan
Cochran, James R.
Richter, Tom
author_facet Scheinert, Mirko
Ferracioli, Fausto
Schwabe, Joachim
Bell, Robin E.
Studinger, Michael
Damaske, Detlef
Jokat, Wilfried
Aleshkova, Nadja
Jordan, Tom
Blankenship, Donald
Damiani, Theresa
Young, Duncan
Cochran, James R.
Richter, Tom
author_sort Scheinert, Mirko
title New Antarctic gravity anomaly grid for enhanced geodetic and geophysical studies in Antarctica
title_short New Antarctic gravity anomaly grid for enhanced geodetic and geophysical studies in Antarctica
title_full New Antarctic gravity anomaly grid for enhanced geodetic and geophysical studies in Antarctica
title_fullStr New Antarctic gravity anomaly grid for enhanced geodetic and geophysical studies in Antarctica
title_full_unstemmed New Antarctic gravity anomaly grid for enhanced geodetic and geophysical studies in Antarctica
title_sort new antarctic gravity anomaly grid for enhanced geodetic and geophysical studies in antarctica
publishDate 2016
url https://doi.org/10.7916/d8-fykv-aq24
geographic Antarctic
geographic_facet Antarctic
genre Antarc*
Antarctic
Antarctica
genre_facet Antarc*
Antarctic
Antarctica
op_relation https://doi.org/10.7916/d8-fykv-aq24
op_doi https://doi.org/10.7916/d8-fykv-aq24
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