Updated OCTAS geoid in the northern North Atlantic- OCTAS07
Abstract. A new gravimetric geoid (OCTAS07v2) is generated using Stokes ’ formula with gravity data as input. As local gravity data, a combination of land gravity data, new and old airborne gravity data, and adjusted marine gravity data has been used. All ma-rine gravity data has been error screened...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.562.1308 2023-05-15T17:30:24+02:00 Updated OCTAS geoid in the northern North Atlantic- OCTAS07 O. C. D. Omang A. Hunegnaw D. Solheim D. I. Lysaker K. Ghazavi H. Nahav The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.562.1308 http://www.geology.osu.edu/~jekeli.1/iag-commission2/IUGG2007_files/reviewed_papers/Omang_etal_11997_final.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.562.1308 http://www.geology.osu.edu/~jekeli.1/iag-commission2/IUGG2007_files/reviewed_papers/Omang_etal_11997_final.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.geology.osu.edu/~jekeli.1/iag-commission2/IUGG2007_files/reviewed_papers/Omang_etal_11997_final.pdf Geoid MDT MSSH Adjusted Marine Gravity Data New Airborne Gravity Data text ftciteseerx 2016-01-08T12:05:32Z Abstract. A new gravimetric geoid (OCTAS07v2) is generated using Stokes ’ formula with gravity data as input. As local gravity data, a combination of land gravity data, new and old airborne gravity data, and adjusted marine gravity data has been used. All ma-rine gravity data has been error screened and quality assured by removing dubious data and adjusting the data when necessary. Voids in the gravity data distri-bution were patched with gravity data from satellite altimetry. The OCTAS07v2 geoid was estimated using the remove-compute-restore technique. The long-wave-length signal of the local gravity data was reduced using a Wong-Gore modified Stokes ’ function. The long-wavelength part was represented by a global grav-ity field model based on GRACE data. The OCTAS07v2 geoid model was combined with the OCTAS07 MSS model to create a synthetic Mean Dynamic Topography (MDT) model. In compari-son with the OCCAM MDT, our new synthetic MDT model gave a std. dev. of the residuals of 11 cm. A comparison to the main northern North Atlantic cur-rents show many similar features. Text North Atlantic Unknown Grav ENVELOPE(12.125,12.125,67.516,67.516) |
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Open Polar |
collection |
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op_collection_id |
ftciteseerx |
language |
English |
topic |
Geoid MDT MSSH Adjusted Marine Gravity Data New Airborne Gravity Data |
spellingShingle |
Geoid MDT MSSH Adjusted Marine Gravity Data New Airborne Gravity Data O. C. D. Omang A. Hunegnaw D. Solheim D. I. Lysaker K. Ghazavi H. Nahav Updated OCTAS geoid in the northern North Atlantic- OCTAS07 |
topic_facet |
Geoid MDT MSSH Adjusted Marine Gravity Data New Airborne Gravity Data |
description |
Abstract. A new gravimetric geoid (OCTAS07v2) is generated using Stokes ’ formula with gravity data as input. As local gravity data, a combination of land gravity data, new and old airborne gravity data, and adjusted marine gravity data has been used. All ma-rine gravity data has been error screened and quality assured by removing dubious data and adjusting the data when necessary. Voids in the gravity data distri-bution were patched with gravity data from satellite altimetry. The OCTAS07v2 geoid was estimated using the remove-compute-restore technique. The long-wave-length signal of the local gravity data was reduced using a Wong-Gore modified Stokes ’ function. The long-wavelength part was represented by a global grav-ity field model based on GRACE data. The OCTAS07v2 geoid model was combined with the OCTAS07 MSS model to create a synthetic Mean Dynamic Topography (MDT) model. In compari-son with the OCCAM MDT, our new synthetic MDT model gave a std. dev. of the residuals of 11 cm. A comparison to the main northern North Atlantic cur-rents show many similar features. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
O. C. D. Omang A. Hunegnaw D. Solheim D. I. Lysaker K. Ghazavi H. Nahav |
author_facet |
O. C. D. Omang A. Hunegnaw D. Solheim D. I. Lysaker K. Ghazavi H. Nahav |
author_sort |
O. C. D. Omang |
title |
Updated OCTAS geoid in the northern North Atlantic- OCTAS07 |
title_short |
Updated OCTAS geoid in the northern North Atlantic- OCTAS07 |
title_full |
Updated OCTAS geoid in the northern North Atlantic- OCTAS07 |
title_fullStr |
Updated OCTAS geoid in the northern North Atlantic- OCTAS07 |
title_full_unstemmed |
Updated OCTAS geoid in the northern North Atlantic- OCTAS07 |
title_sort |
updated octas geoid in the northern north atlantic- octas07 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.562.1308 http://www.geology.osu.edu/~jekeli.1/iag-commission2/IUGG2007_files/reviewed_papers/Omang_etal_11997_final.pdf |
long_lat |
ENVELOPE(12.125,12.125,67.516,67.516) |
geographic |
Grav |
geographic_facet |
Grav |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
http://www.geology.osu.edu/~jekeli.1/iag-commission2/IUGG2007_files/reviewed_papers/Omang_etal_11997_final.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.562.1308 http://www.geology.osu.edu/~jekeli.1/iag-commission2/IUGG2007_files/reviewed_papers/Omang_etal_11997_final.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766126783929778176 |