The geoid: From geodesy to geophysics and from geophysics to geodesy
Abstract The word geoid appeared for the first time in 1873 in a work by Listing, at a time when an increasing number of measurements of meridian arcs were made, in order to determine the figure of the Earth. From that time, the mathematical methods (least squares, inverse methods ...) and the obser...
Ausführliche Beschreibung
Autor*in: |
Amalvict, Martine [verfasserIn] |
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Format: |
Artikel |
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Sprache: |
Englisch |
Erschienen: |
1993 |
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Schlagwörter: |
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Anmerkung: |
© Kluwer Academic Publishers 1993 |
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Übergeordnetes Werk: |
Enthalten in: Surveys in geophysics - Kluwer Academic Publishers, 1986, 14(1993), 4-5 vom: Sept., Seite 477-494 |
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Übergeordnetes Werk: |
volume:14 ; year:1993 ; number:4-5 ; month:09 ; pages:477-494 |
Links: |
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DOI / URN: |
10.1007/BF00690573 |
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Katalog-ID: |
OLC2034984366 |
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10.1007/BF00690573 doi (DE-627)OLC2034984366 (DE-He213)BF00690573-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Amalvict, Martine verfasserin aut The geoid: From geodesy to geophysics and from geophysics to geodesy 1993 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Kluwer Academic Publishers 1993 Abstract The word geoid appeared for the first time in 1873 in a work by Listing, at a time when an increasing number of measurements of meridian arcs were made, in order to determine the figure of the Earth. From that time, the mathematical methods (least squares, inverse methods ...) and the observation and modelling methods (collecting data, precision ...) have made concurrently great progress. Owing to these advances, the geometric method first, and the dynamic method next were developed by geodesy for the computation of the geoid. In particular, the increasing of data brought by satellites since the 60's led to a detailed knowledge of the geoid. The determination of the geoid is, for geodesy, a goal in itself. The geophysical viewpoint is to study the inner structure and the internal dynamics of the Earth, by the interpretation of the shape of the geoid and its anomalies. The two approaches are complementary to one another and react one on the other: from geodesy to geophysics and from geophysics to geodesy. Geophysics Mathematical Method Modelling Method Detailed Knowledge Dynamic Method Boavida, Joaquim aut Enthalten in Surveys in geophysics Kluwer Academic Publishers, 1986 14(1993), 4-5 vom: Sept., Seite 477-494 (DE-627)129582107 (DE-600)232801-X (DE-576)053589092 0169-3298 nnns volume:14 year:1993 number:4-5 month:09 pages:477-494 https://doi.org/10.1007/BF00690573 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-AST GBV_ILN_11 GBV_ILN_22 GBV_ILN_31 GBV_ILN_40 GBV_ILN_47 GBV_ILN_62 GBV_ILN_70 GBV_ILN_601 GBV_ILN_2006 GBV_ILN_4012 GBV_ILN_4035 AR 14 1993 4-5 09 477-494 |
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10.1007/BF00690573 doi (DE-627)OLC2034984366 (DE-He213)BF00690573-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Amalvict, Martine verfasserin aut The geoid: From geodesy to geophysics and from geophysics to geodesy 1993 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Kluwer Academic Publishers 1993 Abstract The word geoid appeared for the first time in 1873 in a work by Listing, at a time when an increasing number of measurements of meridian arcs were made, in order to determine the figure of the Earth. From that time, the mathematical methods (least squares, inverse methods ...) and the observation and modelling methods (collecting data, precision ...) have made concurrently great progress. Owing to these advances, the geometric method first, and the dynamic method next were developed by geodesy for the computation of the geoid. In particular, the increasing of data brought by satellites since the 60's led to a detailed knowledge of the geoid. The determination of the geoid is, for geodesy, a goal in itself. The geophysical viewpoint is to study the inner structure and the internal dynamics of the Earth, by the interpretation of the shape of the geoid and its anomalies. The two approaches are complementary to one another and react one on the other: from geodesy to geophysics and from geophysics to geodesy. Geophysics Mathematical Method Modelling Method Detailed Knowledge Dynamic Method Boavida, Joaquim aut Enthalten in Surveys in geophysics Kluwer Academic Publishers, 1986 14(1993), 4-5 vom: Sept., Seite 477-494 (DE-627)129582107 (DE-600)232801-X (DE-576)053589092 0169-3298 nnns volume:14 year:1993 number:4-5 month:09 pages:477-494 https://doi.org/10.1007/BF00690573 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-AST GBV_ILN_11 GBV_ILN_22 GBV_ILN_31 GBV_ILN_40 GBV_ILN_47 GBV_ILN_62 GBV_ILN_70 GBV_ILN_601 GBV_ILN_2006 GBV_ILN_4012 GBV_ILN_4035 AR 14 1993 4-5 09 477-494 |
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10.1007/BF00690573 doi (DE-627)OLC2034984366 (DE-He213)BF00690573-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Amalvict, Martine verfasserin aut The geoid: From geodesy to geophysics and from geophysics to geodesy 1993 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Kluwer Academic Publishers 1993 Abstract The word geoid appeared for the first time in 1873 in a work by Listing, at a time when an increasing number of measurements of meridian arcs were made, in order to determine the figure of the Earth. From that time, the mathematical methods (least squares, inverse methods ...) and the observation and modelling methods (collecting data, precision ...) have made concurrently great progress. Owing to these advances, the geometric method first, and the dynamic method next were developed by geodesy for the computation of the geoid. In particular, the increasing of data brought by satellites since the 60's led to a detailed knowledge of the geoid. The determination of the geoid is, for geodesy, a goal in itself. The geophysical viewpoint is to study the inner structure and the internal dynamics of the Earth, by the interpretation of the shape of the geoid and its anomalies. The two approaches are complementary to one another and react one on the other: from geodesy to geophysics and from geophysics to geodesy. Geophysics Mathematical Method Modelling Method Detailed Knowledge Dynamic Method Boavida, Joaquim aut Enthalten in Surveys in geophysics Kluwer Academic Publishers, 1986 14(1993), 4-5 vom: Sept., Seite 477-494 (DE-627)129582107 (DE-600)232801-X (DE-576)053589092 0169-3298 nnns volume:14 year:1993 number:4-5 month:09 pages:477-494 https://doi.org/10.1007/BF00690573 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-AST GBV_ILN_11 GBV_ILN_22 GBV_ILN_31 GBV_ILN_40 GBV_ILN_47 GBV_ILN_62 GBV_ILN_70 GBV_ILN_601 GBV_ILN_2006 GBV_ILN_4012 GBV_ILN_4035 AR 14 1993 4-5 09 477-494 |
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10.1007/BF00690573 doi (DE-627)OLC2034984366 (DE-He213)BF00690573-p DE-627 ger DE-627 rakwb eng 550 VZ 16,13 ssgn Amalvict, Martine verfasserin aut The geoid: From geodesy to geophysics and from geophysics to geodesy 1993 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Kluwer Academic Publishers 1993 Abstract The word geoid appeared for the first time in 1873 in a work by Listing, at a time when an increasing number of measurements of meridian arcs were made, in order to determine the figure of the Earth. From that time, the mathematical methods (least squares, inverse methods ...) and the observation and modelling methods (collecting data, precision ...) have made concurrently great progress. Owing to these advances, the geometric method first, and the dynamic method next were developed by geodesy for the computation of the geoid. In particular, the increasing of data brought by satellites since the 60's led to a detailed knowledge of the geoid. The determination of the geoid is, for geodesy, a goal in itself. The geophysical viewpoint is to study the inner structure and the internal dynamics of the Earth, by the interpretation of the shape of the geoid and its anomalies. The two approaches are complementary to one another and react one on the other: from geodesy to geophysics and from geophysics to geodesy. Geophysics Mathematical Method Modelling Method Detailed Knowledge Dynamic Method Boavida, Joaquim aut Enthalten in Surveys in geophysics Kluwer Academic Publishers, 1986 14(1993), 4-5 vom: Sept., Seite 477-494 (DE-627)129582107 (DE-600)232801-X (DE-576)053589092 0169-3298 nnns volume:14 year:1993 number:4-5 month:09 pages:477-494 https://doi.org/10.1007/BF00690573 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-AST GBV_ILN_11 GBV_ILN_22 GBV_ILN_31 GBV_ILN_40 GBV_ILN_47 GBV_ILN_62 GBV_ILN_70 GBV_ILN_601 GBV_ILN_2006 GBV_ILN_4012 GBV_ILN_4035 AR 14 1993 4-5 09 477-494 |
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the geoid: from geodesy to geophysics and from geophysics to geodesy |
title_auth |
The geoid: From geodesy to geophysics and from geophysics to geodesy |
abstract |
Abstract The word geoid appeared for the first time in 1873 in a work by Listing, at a time when an increasing number of measurements of meridian arcs were made, in order to determine the figure of the Earth. From that time, the mathematical methods (least squares, inverse methods ...) and the observation and modelling methods (collecting data, precision ...) have made concurrently great progress. Owing to these advances, the geometric method first, and the dynamic method next were developed by geodesy for the computation of the geoid. In particular, the increasing of data brought by satellites since the 60's led to a detailed knowledge of the geoid. The determination of the geoid is, for geodesy, a goal in itself. The geophysical viewpoint is to study the inner structure and the internal dynamics of the Earth, by the interpretation of the shape of the geoid and its anomalies. The two approaches are complementary to one another and react one on the other: from geodesy to geophysics and from geophysics to geodesy. © Kluwer Academic Publishers 1993 |
abstractGer |
Abstract The word geoid appeared for the first time in 1873 in a work by Listing, at a time when an increasing number of measurements of meridian arcs were made, in order to determine the figure of the Earth. From that time, the mathematical methods (least squares, inverse methods ...) and the observation and modelling methods (collecting data, precision ...) have made concurrently great progress. Owing to these advances, the geometric method first, and the dynamic method next were developed by geodesy for the computation of the geoid. In particular, the increasing of data brought by satellites since the 60's led to a detailed knowledge of the geoid. The determination of the geoid is, for geodesy, a goal in itself. The geophysical viewpoint is to study the inner structure and the internal dynamics of the Earth, by the interpretation of the shape of the geoid and its anomalies. The two approaches are complementary to one another and react one on the other: from geodesy to geophysics and from geophysics to geodesy. © Kluwer Academic Publishers 1993 |
abstract_unstemmed |
Abstract The word geoid appeared for the first time in 1873 in a work by Listing, at a time when an increasing number of measurements of meridian arcs were made, in order to determine the figure of the Earth. From that time, the mathematical methods (least squares, inverse methods ...) and the observation and modelling methods (collecting data, precision ...) have made concurrently great progress. Owing to these advances, the geometric method first, and the dynamic method next were developed by geodesy for the computation of the geoid. In particular, the increasing of data brought by satellites since the 60's led to a detailed knowledge of the geoid. The determination of the geoid is, for geodesy, a goal in itself. The geophysical viewpoint is to study the inner structure and the internal dynamics of the Earth, by the interpretation of the shape of the geoid and its anomalies. The two approaches are complementary to one another and react one on the other: from geodesy to geophysics and from geophysics to geodesy. © Kluwer Academic Publishers 1993 |
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container_issue |
4-5 |
title_short |
The geoid: From geodesy to geophysics and from geophysics to geodesy |
url |
https://doi.org/10.1007/BF00690573 |
remote_bool |
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Boavida, Joaquim |
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up_date |
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