Mapping the geoid for Iberia and the Macaronesian Islands using multisensor gravity data and the GRACE geopotential model

Abstract A new gravimetric geoid model (ICAGM07) has been determined for the North-East Atlantic Ocean, Iberia, and the Macaronesian Islands using multi-sensor gravity data and a GRACE derived Earth geopotential model. A high resolution gravity model, determined using least squares optimal interpola...

Full description

Bibliographic Details
Published in:Journal of Geodynamics
Language:English
Published: Elsevier 2010
Subjects:
Online Access:http://hdl.handle.net/2262/43478
https://doi.org/10.1016/j.jog.2009.03.001
id fttrinitycoll:oai:tara.tcd.ie:2262/43478
record_format openpolar
spelling fttrinitycoll:oai:tara.tcd.ie:2262/43478 2023-05-15T17:36:11+02:00 Mapping the geoid for Iberia and the Macaronesian Islands using multisensor gravity data and the GRACE geopotential model 2010-12-14T18:55:46Z http://hdl.handle.net/2262/43478 https://doi.org/10.1016/j.jog.2009.03.001 en eng Elsevier 02643707 (ISSN) S0264-3707(09)00037-4 (PII) S0264-3707(09)00037-4 (publisherID) http://hdl.handle.net/2262/43478 Journal of Geodynamics 48 1 6 doi:10.1016/j.jog.2009.03.001 2009 18 months Geoid Gravity Height unification North Atlantic Iberia 2010 fttrinitycoll https://doi.org/10.1016/j.jog.2009.03.001 2020-02-16T13:49:44Z Abstract A new gravimetric geoid model (ICAGM07) has been determined for the North-East Atlantic Ocean, Iberia, and the Macaronesian Islands using multi-sensor gravity data and a GRACE derived Earth geopotential model. A high resolution gravity model, determined using least squares optimal interpolation of marine, land, and satellite derived gravity anomalies, was used to resolve the medium and short wavelengths of the geoid. Long wavelengths of the geoid were provided by the GRACE derived Earth geopotential model. The topographic effects were computed in the spectral domain using a high resolution (100 m) digital terrain model derived from SRTM mission data and cartographic charts. The remove-restore technique was used to compute the geoid model on a 1.5 arc minute grid, and the residual geoid height was computed using spherical FFT and a modified Stokes? kernel. The effects of different Earth tide models on the geoid were computed and analyzed. Comparison over the sea with an oceanographic geoid determined from CLS01 MSSH and Rio05 MDT yield a relative accuracy of 8cm, with larger differences close to the shoreline. Over land, comparisons with 1646 GPS/levelling marks indicate an overall precision of 8-10cm and relative vertical datum offsets of up to 2 m. This new geoid model represents a significant improvement over existing geoid models, with a homogeneous relative accuracy of 8-10cm over both marine and land areas, and exposes the inaccuracies of local vertical datums as references for studies of vertical deformation. correspondance: Corresponding author. (Catal?o, J.) jcfernandes@fc.ul.pt (Catal?o, J.) sevilla@mat.ucm.es (Sevilla, M.J.) University of Lisbon--> , Faculty of Sciences--> , IDL--> , LATTEX--> , Lisbon--> - (Catal?o, J.) University of Lisbon--> , Faculty of Sciences--> , IDL--> , LATTEX--> , Lisbon--> - PORTUGAL (Catal?o, J.) Instituto de Astronomia y Geodesia--> , UCM-CSIC--> , Madrid--> - (Sevilla, M.J.) PORTUGAL Received: 2008-07-31 Revised: 2009-03-23 Accepted: 2009-03-23 Other/Unknown Material North Atlantic North East Atlantic The University of Dublin, Trinity College: TARA (Trinity's Access to Research Archive) Journal of Geodynamics 48 1 6 15
institution Open Polar
collection The University of Dublin, Trinity College: TARA (Trinity's Access to Research Archive)
op_collection_id fttrinitycoll
language English
topic Geoid
Gravity
Height unification
North Atlantic
Iberia
spellingShingle Geoid
Gravity
Height unification
North Atlantic
Iberia
Mapping the geoid for Iberia and the Macaronesian Islands using multisensor gravity data and the GRACE geopotential model
topic_facet Geoid
Gravity
Height unification
North Atlantic
Iberia
description Abstract A new gravimetric geoid model (ICAGM07) has been determined for the North-East Atlantic Ocean, Iberia, and the Macaronesian Islands using multi-sensor gravity data and a GRACE derived Earth geopotential model. A high resolution gravity model, determined using least squares optimal interpolation of marine, land, and satellite derived gravity anomalies, was used to resolve the medium and short wavelengths of the geoid. Long wavelengths of the geoid were provided by the GRACE derived Earth geopotential model. The topographic effects were computed in the spectral domain using a high resolution (100 m) digital terrain model derived from SRTM mission data and cartographic charts. The remove-restore technique was used to compute the geoid model on a 1.5 arc minute grid, and the residual geoid height was computed using spherical FFT and a modified Stokes? kernel. The effects of different Earth tide models on the geoid were computed and analyzed. Comparison over the sea with an oceanographic geoid determined from CLS01 MSSH and Rio05 MDT yield a relative accuracy of 8cm, with larger differences close to the shoreline. Over land, comparisons with 1646 GPS/levelling marks indicate an overall precision of 8-10cm and relative vertical datum offsets of up to 2 m. This new geoid model represents a significant improvement over existing geoid models, with a homogeneous relative accuracy of 8-10cm over both marine and land areas, and exposes the inaccuracies of local vertical datums as references for studies of vertical deformation. correspondance: Corresponding author. (Catal?o, J.) jcfernandes@fc.ul.pt (Catal?o, J.) sevilla@mat.ucm.es (Sevilla, M.J.) University of Lisbon--> , Faculty of Sciences--> , IDL--> , LATTEX--> , Lisbon--> - (Catal?o, J.) University of Lisbon--> , Faculty of Sciences--> , IDL--> , LATTEX--> , Lisbon--> - PORTUGAL (Catal?o, J.) Instituto de Astronomia y Geodesia--> , UCM-CSIC--> , Madrid--> - (Sevilla, M.J.) PORTUGAL Received: 2008-07-31 Revised: 2009-03-23 Accepted: 2009-03-23
title Mapping the geoid for Iberia and the Macaronesian Islands using multisensor gravity data and the GRACE geopotential model
title_short Mapping the geoid for Iberia and the Macaronesian Islands using multisensor gravity data and the GRACE geopotential model
title_full Mapping the geoid for Iberia and the Macaronesian Islands using multisensor gravity data and the GRACE geopotential model
title_fullStr Mapping the geoid for Iberia and the Macaronesian Islands using multisensor gravity data and the GRACE geopotential model
title_full_unstemmed Mapping the geoid for Iberia and the Macaronesian Islands using multisensor gravity data and the GRACE geopotential model
title_sort mapping the geoid for iberia and the macaronesian islands using multisensor gravity data and the grace geopotential model
publisher Elsevier
publishDate 2010
url http://hdl.handle.net/2262/43478
https://doi.org/10.1016/j.jog.2009.03.001
genre North Atlantic
North East Atlantic
genre_facet North Atlantic
North East Atlantic
op_relation 02643707 (ISSN)
S0264-3707(09)00037-4 (PII)
S0264-3707(09)00037-4 (publisherID)
http://hdl.handle.net/2262/43478
Journal of Geodynamics
48
1
6
doi:10.1016/j.jog.2009.03.001
op_rights 2009
18 months
op_doi https://doi.org/10.1016/j.jog.2009.03.001
container_title Journal of Geodynamics
container_volume 48
container_issue 1
container_start_page 6
op_container_end_page 15
_version_ 1766135579612807168