Geoid and sea surface topography derived from ERS-1 altimeter data by the adjoint method

A method for splitting sea surface height measurements from satellite altimetry into geoid undulations and sea surface topography is presented. The method is based on a combination of the information from altimeter data and a dynamic sea surface height model. The model consists of geoid undulations...

Full description

Bibliographic Details
Main Authors: Blinken, Robert, Koch, Karl-Rudolf, 1935-
Format: Article in Journal/Newspaper
Language:unknown
Subjects:
7
550
Online Access:https://kramerius.lib.cas.cz/view/uuid:aefa96a5-b99f-4c91-a3b3-25a4471d0d8f
https://doi.org/10.1023/A:1022080011849
id ftczechacademysc:oai:kramerius.lib.cas.cz:uuid:aefa96a5-b99f-4c91-a3b3-25a4471d0d8f
record_format openpolar
spelling ftczechacademysc:oai:kramerius.lib.cas.cz:uuid:aefa96a5-b99f-4c91-a3b3-25a4471d0d8f 2024-03-17T08:59:15+00:00 Geoid and sea surface topography derived from ERS-1 altimeter data by the adjoint method Blinken, Robert Koch, Karl-Rudolf, 1935- print média svazek https://kramerius.lib.cas.cz/view/uuid:aefa96a5-b99f-4c91-a3b3-25a4471d0d8f https://doi.org/10.1023/A:1022080011849 unknown https://kramerius.lib.cas.cz/view/uuid:aefa96a5-b99f-4c91-a3b3-25a4471d0d8f issn:0039-3169 doi:https://doi.org/10.1023/A:1022080011849 policy:private satelitní altimetrie výška hladiny moře zvlnění geoidu topografie povrchu moří satellite altimetry sea surface heights geoid undulations sea surface topography quasi-geostrophic model adjoint method 7 550 model:article ftczechacademysc https://doi.org/10.1023/A:1022080011849 2024-02-19T22:56:34Z A method for splitting sea surface height measurements from satellite altimetry into geoid undulations and sea surface topography is presented. The method is based on a combination of the information from altimeter data and a dynamic sea surface height model. The model consists of geoid undulations and a quasi-geostrophic model for expressing the sea surface topography. The goal is the estimation of those values of the parameters of the sea surface height model that provide a least-squares fit of the model to the data. The solution is accomplished by the adjoint method which makes use of the adjoint model for computing the gradient of the cost function of the least-squares adjustment and an optimization algorithm for obtaining improved parameters. The estimation is applied to the North Atlantic. ERS-1 altimeter data of the year 1993 are used. The resulting geoid agrees well with the geoid of the EGM96 gravity model. Robert Blinken, Karl-Rudolf Koch. Obsahuje bibliografii Article in Journal/Newspaper North Atlantic Czech Academy of Sciences: dKNAV
institution Open Polar
collection Czech Academy of Sciences: dKNAV
op_collection_id ftczechacademysc
language unknown
topic satelitní altimetrie
výška hladiny moře
zvlnění geoidu
topografie povrchu moří
satellite altimetry
sea surface heights
geoid undulations
sea surface topography
quasi-geostrophic model
adjoint method
7
550
spellingShingle satelitní altimetrie
výška hladiny moře
zvlnění geoidu
topografie povrchu moří
satellite altimetry
sea surface heights
geoid undulations
sea surface topography
quasi-geostrophic model
adjoint method
7
550
Blinken, Robert
Koch, Karl-Rudolf, 1935-
Geoid and sea surface topography derived from ERS-1 altimeter data by the adjoint method
topic_facet satelitní altimetrie
výška hladiny moře
zvlnění geoidu
topografie povrchu moří
satellite altimetry
sea surface heights
geoid undulations
sea surface topography
quasi-geostrophic model
adjoint method
7
550
description A method for splitting sea surface height measurements from satellite altimetry into geoid undulations and sea surface topography is presented. The method is based on a combination of the information from altimeter data and a dynamic sea surface height model. The model consists of geoid undulations and a quasi-geostrophic model for expressing the sea surface topography. The goal is the estimation of those values of the parameters of the sea surface height model that provide a least-squares fit of the model to the data. The solution is accomplished by the adjoint method which makes use of the adjoint model for computing the gradient of the cost function of the least-squares adjustment and an optimization algorithm for obtaining improved parameters. The estimation is applied to the North Atlantic. ERS-1 altimeter data of the year 1993 are used. The resulting geoid agrees well with the geoid of the EGM96 gravity model. Robert Blinken, Karl-Rudolf Koch. Obsahuje bibliografii
format Article in Journal/Newspaper
author Blinken, Robert
Koch, Karl-Rudolf, 1935-
author_facet Blinken, Robert
Koch, Karl-Rudolf, 1935-
author_sort Blinken, Robert
title Geoid and sea surface topography derived from ERS-1 altimeter data by the adjoint method
title_short Geoid and sea surface topography derived from ERS-1 altimeter data by the adjoint method
title_full Geoid and sea surface topography derived from ERS-1 altimeter data by the adjoint method
title_fullStr Geoid and sea surface topography derived from ERS-1 altimeter data by the adjoint method
title_full_unstemmed Geoid and sea surface topography derived from ERS-1 altimeter data by the adjoint method
title_sort geoid and sea surface topography derived from ers-1 altimeter data by the adjoint method
url https://kramerius.lib.cas.cz/view/uuid:aefa96a5-b99f-4c91-a3b3-25a4471d0d8f
https://doi.org/10.1023/A:1022080011849
genre North Atlantic
genre_facet North Atlantic
op_relation https://kramerius.lib.cas.cz/view/uuid:aefa96a5-b99f-4c91-a3b3-25a4471d0d8f
issn:0039-3169
doi:https://doi.org/10.1023/A:1022080011849
op_rights policy:private
op_doi https://doi.org/10.1023/A:1022080011849
_version_ 1793769667400040448