Non-Tidal ocean loading correction for the Argentinean-German Geodetic Observatory using an empirical model of storm surge for the Río de la Plata
- Autores
- Oreiro, Fernando Ariel; Wziontek, H.; Fiore, Monica Maria Elisa; D'onofrio, Enrique Eduardo; Brunini, Claudio Antonio
- Año de publicación
- 2017
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- The Argentinean-German Geodetic Observatory is located 13 km from the Río de la Plata, in an area that is frequently affected by storm surges that can vary the level of the river over ±3 m. Water-level information from seven tide gauge stations located in the Río de la Plata are used to calculate every hour an empirical model of water heights (tidal + non-tidal component) and an empirical model of storm surge (non-tidal component) for the period 01/2016?12/2016. Using the SPOTL software, the gravimetric response of the models and the tidal response are calculated, obtaining that for the observatory location, the range of the tidal component (3.6 nm/s2) is only 12% of the range of the non-tidal component (29.4 nm/s2). The gravimetric response of the storm surge model is subtracted from the superconducting gravimeter observations, after applying the traditional corrections, and a reduction of 7% of the RMS is obtained. The wavelet transform is applied to the same series, before and after the non-tidal correction, and a clear decrease in the spectral energy in the periods between 2 and 12 days is identify between the series. Using the same software East, North and Up displacements are calculated, and a range of 3, 2, and 11 mm is obtained, respectively. The residuals obtained after applying the non-tidal correction allow to clearly identify the influence of rain events in the superconducting gravimeter observations, indicating the need of the analysis of this, and others, hydrological and geophysical effects.
Fil: Oreiro, Fernando Ariel. Ministerio de Defensa. Armada Argentina. Servicio de Hidrografía Naval; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad de Buenos Aires. Facultad de Ingeniería. Instituto de Geodesia y Geofísica Aplicadas; Argentina
Fil: Wziontek, H.. Bundesamt fur Kartographie und Geodasie; Alemania
Fil: Fiore, Monica Maria Elisa. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Ministerio de Defensa. Armada Argentina. Servicio de Hidrografía Naval; Argentina. Universidad de Buenos Aires. Facultad de Ingeniería. Instituto de Geodesia y Geofísica Aplicadas; Argentina
Fil: D'onofrio, Enrique Eduardo. Ministerio de Defensa. Armada Argentina. Servicio de Hidrografía Naval; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad de Buenos Aires. Facultad de Ingeniería. Instituto de Geodesia y Geofísica Aplicadas; Argentina
Fil: Brunini, Claudio Antonio. Universidad Nacional de La Plata. Facultad de Ciencias Astronómicas y Geofísicas. Grupo de Geodesia Espacial y Aeronomía; Argentina. Observatorio geodésico argentino-alemán; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina - Materia
-
ARGENTINEAN-GERMAN GEODETIC OBSERVATORY
NON-TIDAL OCEAN LOADING
RÍO DE LA PLATA
STORM SURGE MODEL
SUPERCONDUCTING GRAVIMETER - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
- Repositorio
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/101407
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Non-Tidal ocean loading correction for the Argentinean-German Geodetic Observatory using an empirical model of storm surge for the Río de la PlataOreiro, Fernando ArielWziontek, H.Fiore, Monica Maria ElisaD'onofrio, Enrique EduardoBrunini, Claudio AntonioARGENTINEAN-GERMAN GEODETIC OBSERVATORYNON-TIDAL OCEAN LOADINGRÍO DE LA PLATASTORM SURGE MODELSUPERCONDUCTING GRAVIMETERhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1The Argentinean-German Geodetic Observatory is located 13 km from the Río de la Plata, in an area that is frequently affected by storm surges that can vary the level of the river over ±3 m. Water-level information from seven tide gauge stations located in the Río de la Plata are used to calculate every hour an empirical model of water heights (tidal + non-tidal component) and an empirical model of storm surge (non-tidal component) for the period 01/2016?12/2016. Using the SPOTL software, the gravimetric response of the models and the tidal response are calculated, obtaining that for the observatory location, the range of the tidal component (3.6 nm/s2) is only 12% of the range of the non-tidal component (29.4 nm/s2). The gravimetric response of the storm surge model is subtracted from the superconducting gravimeter observations, after applying the traditional corrections, and a reduction of 7% of the RMS is obtained. The wavelet transform is applied to the same series, before and after the non-tidal correction, and a clear decrease in the spectral energy in the periods between 2 and 12 days is identify between the series. Using the same software East, North and Up displacements are calculated, and a range of 3, 2, and 11 mm is obtained, respectively. The residuals obtained after applying the non-tidal correction allow to clearly identify the influence of rain events in the superconducting gravimeter observations, indicating the need of the analysis of this, and others, hydrological and geophysical effects.Fil: Oreiro, Fernando Ariel. Ministerio de Defensa. Armada Argentina. Servicio de Hidrografía Naval; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad de Buenos Aires. Facultad de Ingeniería. Instituto de Geodesia y Geofísica Aplicadas; ArgentinaFil: Wziontek, H.. Bundesamt fur Kartographie und Geodasie; AlemaniaFil: Fiore, Monica Maria Elisa. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Ministerio de Defensa. Armada Argentina. Servicio de Hidrografía Naval; Argentina. Universidad de Buenos Aires. Facultad de Ingeniería. Instituto de Geodesia y Geofísica Aplicadas; ArgentinaFil: D'onofrio, Enrique Eduardo. Ministerio de Defensa. Armada Argentina. Servicio de Hidrografía Naval; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad de Buenos Aires. Facultad de Ingeniería. Instituto de Geodesia y Geofísica Aplicadas; ArgentinaFil: Brunini, Claudio Antonio. Universidad Nacional de La Plata. Facultad de Ciencias Astronómicas y Geofísicas. Grupo de Geodesia Espacial y Aeronomía; Argentina. Observatorio geodésico argentino-alemán; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaBirkhauser Verlag Ag2017-08-29info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/101407Oreiro, Fernando Ariel; Wziontek, H.; Fiore, Monica Maria Elisa; D'onofrio, Enrique Eduardo; Brunini, Claudio Antonio; Non-Tidal ocean loading correction for the Argentinean-German Geodetic Observatory using an empirical model of storm surge for the Río de la Plata; Birkhauser Verlag Ag; Pure And Applied Geophysics; 175; 5; 29-8-2017; 1739-17530033-4553CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/http://link.springer.com/10.1007/s00024-017-1651-6info:eu-repo/semantics/altIdentifier/doi/10.1007/s00024-017-1651-6info:eu-repo/semantics/altIdentifier/url/https://link.springer.com/article/10.1007%2Fs00024-017-1651-6info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T09:34:21Zoai:ri.conicet.gov.ar:11336/101407instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-29 09:34:21.472CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
dc.title.none.fl_str_mv |
Non-Tidal ocean loading correction for the Argentinean-German Geodetic Observatory using an empirical model of storm surge for the Río de la Plata |
title |
Non-Tidal ocean loading correction for the Argentinean-German Geodetic Observatory using an empirical model of storm surge for the Río de la Plata |
spellingShingle |
Non-Tidal ocean loading correction for the Argentinean-German Geodetic Observatory using an empirical model of storm surge for the Río de la Plata Oreiro, Fernando Ariel ARGENTINEAN-GERMAN GEODETIC OBSERVATORY NON-TIDAL OCEAN LOADING RÍO DE LA PLATA STORM SURGE MODEL SUPERCONDUCTING GRAVIMETER |
title_short |
Non-Tidal ocean loading correction for the Argentinean-German Geodetic Observatory using an empirical model of storm surge for the Río de la Plata |
title_full |
Non-Tidal ocean loading correction for the Argentinean-German Geodetic Observatory using an empirical model of storm surge for the Río de la Plata |
title_fullStr |
Non-Tidal ocean loading correction for the Argentinean-German Geodetic Observatory using an empirical model of storm surge for the Río de la Plata |
title_full_unstemmed |
Non-Tidal ocean loading correction for the Argentinean-German Geodetic Observatory using an empirical model of storm surge for the Río de la Plata |
title_sort |
Non-Tidal ocean loading correction for the Argentinean-German Geodetic Observatory using an empirical model of storm surge for the Río de la Plata |
dc.creator.none.fl_str_mv |
Oreiro, Fernando Ariel Wziontek, H. Fiore, Monica Maria Elisa D'onofrio, Enrique Eduardo Brunini, Claudio Antonio |
author |
Oreiro, Fernando Ariel |
author_facet |
Oreiro, Fernando Ariel Wziontek, H. Fiore, Monica Maria Elisa D'onofrio, Enrique Eduardo Brunini, Claudio Antonio |
author_role |
author |
author2 |
Wziontek, H. Fiore, Monica Maria Elisa D'onofrio, Enrique Eduardo Brunini, Claudio Antonio |
author2_role |
author author author author |
dc.subject.none.fl_str_mv |
ARGENTINEAN-GERMAN GEODETIC OBSERVATORY NON-TIDAL OCEAN LOADING RÍO DE LA PLATA STORM SURGE MODEL SUPERCONDUCTING GRAVIMETER |
topic |
ARGENTINEAN-GERMAN GEODETIC OBSERVATORY NON-TIDAL OCEAN LOADING RÍO DE LA PLATA STORM SURGE MODEL SUPERCONDUCTING GRAVIMETER |
purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
dc.description.none.fl_txt_mv |
The Argentinean-German Geodetic Observatory is located 13 km from the Río de la Plata, in an area that is frequently affected by storm surges that can vary the level of the river over ±3 m. Water-level information from seven tide gauge stations located in the Río de la Plata are used to calculate every hour an empirical model of water heights (tidal + non-tidal component) and an empirical model of storm surge (non-tidal component) for the period 01/2016?12/2016. Using the SPOTL software, the gravimetric response of the models and the tidal response are calculated, obtaining that for the observatory location, the range of the tidal component (3.6 nm/s2) is only 12% of the range of the non-tidal component (29.4 nm/s2). The gravimetric response of the storm surge model is subtracted from the superconducting gravimeter observations, after applying the traditional corrections, and a reduction of 7% of the RMS is obtained. The wavelet transform is applied to the same series, before and after the non-tidal correction, and a clear decrease in the spectral energy in the periods between 2 and 12 days is identify between the series. Using the same software East, North and Up displacements are calculated, and a range of 3, 2, and 11 mm is obtained, respectively. The residuals obtained after applying the non-tidal correction allow to clearly identify the influence of rain events in the superconducting gravimeter observations, indicating the need of the analysis of this, and others, hydrological and geophysical effects. Fil: Oreiro, Fernando Ariel. Ministerio de Defensa. Armada Argentina. Servicio de Hidrografía Naval; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad de Buenos Aires. Facultad de Ingeniería. Instituto de Geodesia y Geofísica Aplicadas; Argentina Fil: Wziontek, H.. Bundesamt fur Kartographie und Geodasie; Alemania Fil: Fiore, Monica Maria Elisa. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Ministerio de Defensa. Armada Argentina. Servicio de Hidrografía Naval; Argentina. Universidad de Buenos Aires. Facultad de Ingeniería. Instituto de Geodesia y Geofísica Aplicadas; Argentina Fil: D'onofrio, Enrique Eduardo. Ministerio de Defensa. Armada Argentina. Servicio de Hidrografía Naval; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad de Buenos Aires. Facultad de Ingeniería. Instituto de Geodesia y Geofísica Aplicadas; Argentina Fil: Brunini, Claudio Antonio. Universidad Nacional de La Plata. Facultad de Ciencias Astronómicas y Geofísicas. Grupo de Geodesia Espacial y Aeronomía; Argentina. Observatorio geodésico argentino-alemán; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina |
description |
The Argentinean-German Geodetic Observatory is located 13 km from the Río de la Plata, in an area that is frequently affected by storm surges that can vary the level of the river over ±3 m. Water-level information from seven tide gauge stations located in the Río de la Plata are used to calculate every hour an empirical model of water heights (tidal + non-tidal component) and an empirical model of storm surge (non-tidal component) for the period 01/2016?12/2016. Using the SPOTL software, the gravimetric response of the models and the tidal response are calculated, obtaining that for the observatory location, the range of the tidal component (3.6 nm/s2) is only 12% of the range of the non-tidal component (29.4 nm/s2). The gravimetric response of the storm surge model is subtracted from the superconducting gravimeter observations, after applying the traditional corrections, and a reduction of 7% of the RMS is obtained. The wavelet transform is applied to the same series, before and after the non-tidal correction, and a clear decrease in the spectral energy in the periods between 2 and 12 days is identify between the series. Using the same software East, North and Up displacements are calculated, and a range of 3, 2, and 11 mm is obtained, respectively. The residuals obtained after applying the non-tidal correction allow to clearly identify the influence of rain events in the superconducting gravimeter observations, indicating the need of the analysis of this, and others, hydrological and geophysical effects. |
publishDate |
2017 |
dc.date.none.fl_str_mv |
2017-08-29 |
dc.type.none.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion http://purl.org/coar/resource_type/c_6501 info:ar-repo/semantics/articulo |
format |
article |
status_str |
publishedVersion |
dc.identifier.none.fl_str_mv |
http://hdl.handle.net/11336/101407 Oreiro, Fernando Ariel; Wziontek, H.; Fiore, Monica Maria Elisa; D'onofrio, Enrique Eduardo; Brunini, Claudio Antonio; Non-Tidal ocean loading correction for the Argentinean-German Geodetic Observatory using an empirical model of storm surge for the Río de la Plata; Birkhauser Verlag Ag; Pure And Applied Geophysics; 175; 5; 29-8-2017; 1739-1753 0033-4553 CONICET Digital CONICET |
url |
http://hdl.handle.net/11336/101407 |
identifier_str_mv |
Oreiro, Fernando Ariel; Wziontek, H.; Fiore, Monica Maria Elisa; D'onofrio, Enrique Eduardo; Brunini, Claudio Antonio; Non-Tidal ocean loading correction for the Argentinean-German Geodetic Observatory using an empirical model of storm surge for the Río de la Plata; Birkhauser Verlag Ag; Pure And Applied Geophysics; 175; 5; 29-8-2017; 1739-1753 0033-4553 CONICET Digital CONICET |
dc.language.none.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
info:eu-repo/semantics/altIdentifier/url/http://link.springer.com/10.1007/s00024-017-1651-6 info:eu-repo/semantics/altIdentifier/doi/10.1007/s00024-017-1651-6 info:eu-repo/semantics/altIdentifier/url/https://link.springer.com/article/10.1007%2Fs00024-017-1651-6 |
dc.rights.none.fl_str_mv |
info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
eu_rights_str_mv |
openAccess |
rights_invalid_str_mv |
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
dc.format.none.fl_str_mv |
application/pdf application/pdf application/pdf application/pdf application/pdf |
dc.publisher.none.fl_str_mv |
Birkhauser Verlag Ag |
publisher.none.fl_str_mv |
Birkhauser Verlag Ag |
dc.source.none.fl_str_mv |
reponame:CONICET Digital (CONICET) instname:Consejo Nacional de Investigaciones Científicas y Técnicas |
reponame_str |
CONICET Digital (CONICET) |
collection |
CONICET Digital (CONICET) |
instname_str |
Consejo Nacional de Investigaciones Científicas y Técnicas |
repository.name.fl_str_mv |
CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas |
repository.mail.fl_str_mv |
dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar |
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1844613062305251328 |
score |
13.070432 |