Rescue of the historical sea level record of Marseille (France) from 1885 to 1988 and its extension back to 1849–1851

Abstract This paper describes the historical sea level data that we have rescued from a tide gauge, especially devised originally for geodesy. This gauge was installed in Marseille in 1884 with the primary objective of defining the origin of the height system in France. Hourly values for 1885–1988 h...
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Autor*in:	Wöppelmann, G. [verfasserIn] Marcos, M. Coulomb, A. Martín Míguez, B. Bonnetain, P. Boucher, C. Gravelle, M. Simon, B. Tiphaneau, P.

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2014

Schlagwörter:	Tide gauge Levelling Sea level History of geodesy Marseille

Anmerkung:	© The Author(s) 2014

Übergeordnetes Werk:	Enthalten in: Journal of geodesy - Berlin : Springer, 1995, 88(2014), 9 vom: 08. Juni, Seite 869-885
Übergeordnetes Werk:	volume:88 ; year:2014 ; number:9 ; day:08 ; month:06 ; pages:869-885

Links:	Volltext

DOI / URN:	10.1007/s00190-014-0728-6

Katalog-ID:	SPR001590316

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520			\|a Abstract This paper describes the historical sea level data that we have rescued from a tide gauge, especially devised originally for geodesy. This gauge was installed in Marseille in 1884 with the primary objective of defining the origin of the height system in France. Hourly values for 1885–1988 have been digitized from the original tidal charts. They are supplemented by hourly values from an older tide gauge record (1849–1851) that was rediscovered during a survey in 2009. Both recovered data sets have been critically edited for errors and their reliability assessed. The hourly values are thoroughly analysed for the first time after their original recording. A consistent high-frequency time series is reported, increasing notably the length of one of the few European sea level records in the Mediterranean Sea spanning more than one hundred years. Changes in sea levels are examined, and previous results revisited with the extended time series. The rate of relative sea level change for the period 1849–2012 is estimated to have been %$1.08\pm 0.04%$ mm/year at Marseille, a value that is slightly lower but in close agreement with the longest time series of Brest over the common period (%$1.26\pm 0.04%$ mm/year). The data from a permanent global positioning system station installed on the roof of the solid tide gauge building suggests a remarkable stability of the ground (%$-0.04\pm 0.25%$ mm/year) since 1998, confirming the choice made by our predecessor geodesists in the nineteenth century regarding this site selection.
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700	1		\|a Martín Míguez, B. \|4 aut
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700	1		\|a Boucher, C. \|4 aut
700	1		\|a Gravelle, M. \|4 aut
700	1		\|a Simon, B. \|4 aut
700	1		\|a Tiphaneau, P. \|4 aut
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allfields	10.1007/s00190-014-0728-6 doi (DE-627)SPR001590316 (SPR)s00190-014-0728-6-e DE-627 ger DE-627 rakwb eng Wöppelmann, G. verfasserin aut Rescue of the historical sea level record of Marseille (France) from 1885 to 1988 and its extension back to 1849–1851 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s) 2014 Abstract This paper describes the historical sea level data that we have rescued from a tide gauge, especially devised originally for geodesy. This gauge was installed in Marseille in 1884 with the primary objective of defining the origin of the height system in France. Hourly values for 1885–1988 have been digitized from the original tidal charts. They are supplemented by hourly values from an older tide gauge record (1849–1851) that was rediscovered during a survey in 2009. Both recovered data sets have been critically edited for errors and their reliability assessed. The hourly values are thoroughly analysed for the first time after their original recording. A consistent high-frequency time series is reported, increasing notably the length of one of the few European sea level records in the Mediterranean Sea spanning more than one hundred years. Changes in sea levels are examined, and previous results revisited with the extended time series. The rate of relative sea level change for the period 1849–2012 is estimated to have been %$1.08\pm 0.04%$ mm/year at Marseille, a value that is slightly lower but in close agreement with the longest time series of Brest over the common period (%$1.26\pm 0.04%$ mm/year). The data from a permanent global positioning system station installed on the roof of the solid tide gauge building suggests a remarkable stability of the ground (%$-0.04\pm 0.25%$ mm/year) since 1998, confirming the choice made by our predecessor geodesists in the nineteenth century regarding this site selection. Tide gauge (dpeaa)DE-He213 Levelling (dpeaa)DE-He213 Sea level (dpeaa)DE-He213 History of geodesy (dpeaa)DE-He213 Marseille (dpeaa)DE-He213 Marcos, M. aut Coulomb, A. aut Martín Míguez, B. aut Bonnetain, P. aut Boucher, C. aut Gravelle, M. aut Simon, B. aut Tiphaneau, P. aut Enthalten in Journal of geodesy Berlin : Springer, 1995 88(2014), 9 vom: 08. Juni, Seite 869-885 (DE-627)271175389 (DE-600)1478938-3 1432-1394 nnns volume:88 year:2014 number:9 day:08 month:06 pages:869-885 https://dx.doi.org/10.1007/s00190-014-0728-6 kostenfrei Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 88 2014 9 08 06 869-885
spelling	10.1007/s00190-014-0728-6 doi (DE-627)SPR001590316 (SPR)s00190-014-0728-6-e DE-627 ger DE-627 rakwb eng Wöppelmann, G. verfasserin aut Rescue of the historical sea level record of Marseille (France) from 1885 to 1988 and its extension back to 1849–1851 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s) 2014 Abstract This paper describes the historical sea level data that we have rescued from a tide gauge, especially devised originally for geodesy. This gauge was installed in Marseille in 1884 with the primary objective of defining the origin of the height system in France. Hourly values for 1885–1988 have been digitized from the original tidal charts. They are supplemented by hourly values from an older tide gauge record (1849–1851) that was rediscovered during a survey in 2009. Both recovered data sets have been critically edited for errors and their reliability assessed. The hourly values are thoroughly analysed for the first time after their original recording. A consistent high-frequency time series is reported, increasing notably the length of one of the few European sea level records in the Mediterranean Sea spanning more than one hundred years. Changes in sea levels are examined, and previous results revisited with the extended time series. The rate of relative sea level change for the period 1849–2012 is estimated to have been %$1.08\pm 0.04%$ mm/year at Marseille, a value that is slightly lower but in close agreement with the longest time series of Brest over the common period (%$1.26\pm 0.04%$ mm/year). The data from a permanent global positioning system station installed on the roof of the solid tide gauge building suggests a remarkable stability of the ground (%$-0.04\pm 0.25%$ mm/year) since 1998, confirming the choice made by our predecessor geodesists in the nineteenth century regarding this site selection. Tide gauge (dpeaa)DE-He213 Levelling (dpeaa)DE-He213 Sea level (dpeaa)DE-He213 History of geodesy (dpeaa)DE-He213 Marseille (dpeaa)DE-He213 Marcos, M. aut Coulomb, A. aut Martín Míguez, B. aut Bonnetain, P. aut Boucher, C. aut Gravelle, M. aut Simon, B. aut Tiphaneau, P. aut Enthalten in Journal of geodesy Berlin : Springer, 1995 88(2014), 9 vom: 08. Juni, Seite 869-885 (DE-627)271175389 (DE-600)1478938-3 1432-1394 nnns volume:88 year:2014 number:9 day:08 month:06 pages:869-885 https://dx.doi.org/10.1007/s00190-014-0728-6 kostenfrei Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 88 2014 9 08 06 869-885
allfields_unstemmed	10.1007/s00190-014-0728-6 doi (DE-627)SPR001590316 (SPR)s00190-014-0728-6-e DE-627 ger DE-627 rakwb eng Wöppelmann, G. verfasserin aut Rescue of the historical sea level record of Marseille (France) from 1885 to 1988 and its extension back to 1849–1851 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s) 2014 Abstract This paper describes the historical sea level data that we have rescued from a tide gauge, especially devised originally for geodesy. This gauge was installed in Marseille in 1884 with the primary objective of defining the origin of the height system in France. Hourly values for 1885–1988 have been digitized from the original tidal charts. They are supplemented by hourly values from an older tide gauge record (1849–1851) that was rediscovered during a survey in 2009. Both recovered data sets have been critically edited for errors and their reliability assessed. The hourly values are thoroughly analysed for the first time after their original recording. A consistent high-frequency time series is reported, increasing notably the length of one of the few European sea level records in the Mediterranean Sea spanning more than one hundred years. Changes in sea levels are examined, and previous results revisited with the extended time series. The rate of relative sea level change for the period 1849–2012 is estimated to have been %$1.08\pm 0.04%$ mm/year at Marseille, a value that is slightly lower but in close agreement with the longest time series of Brest over the common period (%$1.26\pm 0.04%$ mm/year). The data from a permanent global positioning system station installed on the roof of the solid tide gauge building suggests a remarkable stability of the ground (%$-0.04\pm 0.25%$ mm/year) since 1998, confirming the choice made by our predecessor geodesists in the nineteenth century regarding this site selection. Tide gauge (dpeaa)DE-He213 Levelling (dpeaa)DE-He213 Sea level (dpeaa)DE-He213 History of geodesy (dpeaa)DE-He213 Marseille (dpeaa)DE-He213 Marcos, M. aut Coulomb, A. aut Martín Míguez, B. aut Bonnetain, P. aut Boucher, C. aut Gravelle, M. aut Simon, B. aut Tiphaneau, P. aut Enthalten in Journal of geodesy Berlin : Springer, 1995 88(2014), 9 vom: 08. Juni, Seite 869-885 (DE-627)271175389 (DE-600)1478938-3 1432-1394 nnns volume:88 year:2014 number:9 day:08 month:06 pages:869-885 https://dx.doi.org/10.1007/s00190-014-0728-6 kostenfrei Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 88 2014 9 08 06 869-885
allfieldsGer	10.1007/s00190-014-0728-6 doi (DE-627)SPR001590316 (SPR)s00190-014-0728-6-e DE-627 ger DE-627 rakwb eng Wöppelmann, G. verfasserin aut Rescue of the historical sea level record of Marseille (France) from 1885 to 1988 and its extension back to 1849–1851 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s) 2014 Abstract This paper describes the historical sea level data that we have rescued from a tide gauge, especially devised originally for geodesy. This gauge was installed in Marseille in 1884 with the primary objective of defining the origin of the height system in France. Hourly values for 1885–1988 have been digitized from the original tidal charts. They are supplemented by hourly values from an older tide gauge record (1849–1851) that was rediscovered during a survey in 2009. Both recovered data sets have been critically edited for errors and their reliability assessed. The hourly values are thoroughly analysed for the first time after their original recording. A consistent high-frequency time series is reported, increasing notably the length of one of the few European sea level records in the Mediterranean Sea spanning more than one hundred years. Changes in sea levels are examined, and previous results revisited with the extended time series. The rate of relative sea level change for the period 1849–2012 is estimated to have been %$1.08\pm 0.04%$ mm/year at Marseille, a value that is slightly lower but in close agreement with the longest time series of Brest over the common period (%$1.26\pm 0.04%$ mm/year). The data from a permanent global positioning system station installed on the roof of the solid tide gauge building suggests a remarkable stability of the ground (%$-0.04\pm 0.25%$ mm/year) since 1998, confirming the choice made by our predecessor geodesists in the nineteenth century regarding this site selection. Tide gauge (dpeaa)DE-He213 Levelling (dpeaa)DE-He213 Sea level (dpeaa)DE-He213 History of geodesy (dpeaa)DE-He213 Marseille (dpeaa)DE-He213 Marcos, M. aut Coulomb, A. aut Martín Míguez, B. aut Bonnetain, P. aut Boucher, C. aut Gravelle, M. aut Simon, B. aut Tiphaneau, P. aut Enthalten in Journal of geodesy Berlin : Springer, 1995 88(2014), 9 vom: 08. Juni, Seite 869-885 (DE-627)271175389 (DE-600)1478938-3 1432-1394 nnns volume:88 year:2014 number:9 day:08 month:06 pages:869-885 https://dx.doi.org/10.1007/s00190-014-0728-6 kostenfrei Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 88 2014 9 08 06 869-885
allfieldsSound	10.1007/s00190-014-0728-6 doi (DE-627)SPR001590316 (SPR)s00190-014-0728-6-e DE-627 ger DE-627 rakwb eng Wöppelmann, G. verfasserin aut Rescue of the historical sea level record of Marseille (France) from 1885 to 1988 and its extension back to 1849–1851 2014 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s) 2014 Abstract This paper describes the historical sea level data that we have rescued from a tide gauge, especially devised originally for geodesy. This gauge was installed in Marseille in 1884 with the primary objective of defining the origin of the height system in France. Hourly values for 1885–1988 have been digitized from the original tidal charts. They are supplemented by hourly values from an older tide gauge record (1849–1851) that was rediscovered during a survey in 2009. Both recovered data sets have been critically edited for errors and their reliability assessed. The hourly values are thoroughly analysed for the first time after their original recording. A consistent high-frequency time series is reported, increasing notably the length of one of the few European sea level records in the Mediterranean Sea spanning more than one hundred years. Changes in sea levels are examined, and previous results revisited with the extended time series. The rate of relative sea level change for the period 1849–2012 is estimated to have been %$1.08\pm 0.04%$ mm/year at Marseille, a value that is slightly lower but in close agreement with the longest time series of Brest over the common period (%$1.26\pm 0.04%$ mm/year). The data from a permanent global positioning system station installed on the roof of the solid tide gauge building suggests a remarkable stability of the ground (%$-0.04\pm 0.25%$ mm/year) since 1998, confirming the choice made by our predecessor geodesists in the nineteenth century regarding this site selection. Tide gauge (dpeaa)DE-He213 Levelling (dpeaa)DE-He213 Sea level (dpeaa)DE-He213 History of geodesy (dpeaa)DE-He213 Marseille (dpeaa)DE-He213 Marcos, M. aut Coulomb, A. aut Martín Míguez, B. aut Bonnetain, P. aut Boucher, C. aut Gravelle, M. aut Simon, B. aut Tiphaneau, P. aut Enthalten in Journal of geodesy Berlin : Springer, 1995 88(2014), 9 vom: 08. Juni, Seite 869-885 (DE-627)271175389 (DE-600)1478938-3 1432-1394 nnns volume:88 year:2014 number:9 day:08 month:06 pages:869-885 https://dx.doi.org/10.1007/s00190-014-0728-6 kostenfrei Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 88 2014 9 08 06 869-885
language	English
source	Enthalten in Journal of geodesy 88(2014), 9 vom: 08. Juni, Seite 869-885 volume:88 year:2014 number:9 day:08 month:06 pages:869-885
sourceStr	Enthalten in Journal of geodesy 88(2014), 9 vom: 08. Juni, Seite 869-885 volume:88 year:2014 number:9 day:08 month:06 pages:869-885
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	Tide gauge Levelling Sea level History of geodesy Marseille
isfreeaccess_bool	true
container_title	Journal of geodesy
authorswithroles_txt_mv	Wöppelmann, G. @@aut@@ Marcos, M. @@aut@@ Coulomb, A. @@aut@@ Martín Míguez, B. @@aut@@ Bonnetain, P. @@aut@@ Boucher, C. @@aut@@ Gravelle, M. @@aut@@ Simon, B. @@aut@@ Tiphaneau, P. @@aut@@
publishDateDaySort_date	2014-06-08T00:00:00Z
hierarchy_top_id	271175389
id	SPR001590316
language_de	englisch
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author	Wöppelmann, G.
spellingShingle	Wöppelmann, G. misc Tide gauge misc Levelling misc Sea level misc History of geodesy misc Marseille Rescue of the historical sea level record of Marseille (France) from 1885 to 1988 and its extension back to 1849–1851
authorStr	Wöppelmann, G.
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topic_title	Rescue of the historical sea level record of Marseille (France) from 1885 to 1988 and its extension back to 1849–1851 Tide gauge (dpeaa)DE-He213 Levelling (dpeaa)DE-He213 Sea level (dpeaa)DE-He213 History of geodesy (dpeaa)DE-He213 Marseille (dpeaa)DE-He213
topic	misc Tide gauge misc Levelling misc Sea level misc History of geodesy misc Marseille
topic_unstemmed	misc Tide gauge misc Levelling misc Sea level misc History of geodesy misc Marseille
topic_browse	misc Tide gauge misc Levelling misc Sea level misc History of geodesy misc Marseille
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title	Rescue of the historical sea level record of Marseille (France) from 1885 to 1988 and its extension back to 1849–1851
ctrlnum	(DE-627)SPR001590316 (SPR)s00190-014-0728-6-e
title_full	Rescue of the historical sea level record of Marseille (France) from 1885 to 1988 and its extension back to 1849–1851
author_sort	Wöppelmann, G.
journal	Journal of geodesy
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author_browse	Wöppelmann, G. Marcos, M. Coulomb, A. Martín Míguez, B. Bonnetain, P. Boucher, C. Gravelle, M. Simon, B. Tiphaneau, P.
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author-letter	Wöppelmann, G.
doi_str_mv	10.1007/s00190-014-0728-6
title_sort	rescue of the historical sea level record of marseille (france) from 1885 to 1988 and its extension back to 1849–1851
title_auth	Rescue of the historical sea level record of Marseille (France) from 1885 to 1988 and its extension back to 1849–1851
abstract	Abstract This paper describes the historical sea level data that we have rescued from a tide gauge, especially devised originally for geodesy. This gauge was installed in Marseille in 1884 with the primary objective of defining the origin of the height system in France. Hourly values for 1885–1988 have been digitized from the original tidal charts. They are supplemented by hourly values from an older tide gauge record (1849–1851) that was rediscovered during a survey in 2009. Both recovered data sets have been critically edited for errors and their reliability assessed. The hourly values are thoroughly analysed for the first time after their original recording. A consistent high-frequency time series is reported, increasing notably the length of one of the few European sea level records in the Mediterranean Sea spanning more than one hundred years. Changes in sea levels are examined, and previous results revisited with the extended time series. The rate of relative sea level change for the period 1849–2012 is estimated to have been %$1.08\pm 0.04%$ mm/year at Marseille, a value that is slightly lower but in close agreement with the longest time series of Brest over the common period (%$1.26\pm 0.04%$ mm/year). The data from a permanent global positioning system station installed on the roof of the solid tide gauge building suggests a remarkable stability of the ground (%$-0.04\pm 0.25%$ mm/year) since 1998, confirming the choice made by our predecessor geodesists in the nineteenth century regarding this site selection. © The Author(s) 2014
abstractGer	Abstract This paper describes the historical sea level data that we have rescued from a tide gauge, especially devised originally for geodesy. This gauge was installed in Marseille in 1884 with the primary objective of defining the origin of the height system in France. Hourly values for 1885–1988 have been digitized from the original tidal charts. They are supplemented by hourly values from an older tide gauge record (1849–1851) that was rediscovered during a survey in 2009. Both recovered data sets have been critically edited for errors and their reliability assessed. The hourly values are thoroughly analysed for the first time after their original recording. A consistent high-frequency time series is reported, increasing notably the length of one of the few European sea level records in the Mediterranean Sea spanning more than one hundred years. Changes in sea levels are examined, and previous results revisited with the extended time series. The rate of relative sea level change for the period 1849–2012 is estimated to have been %$1.08\pm 0.04%$ mm/year at Marseille, a value that is slightly lower but in close agreement with the longest time series of Brest over the common period (%$1.26\pm 0.04%$ mm/year). The data from a permanent global positioning system station installed on the roof of the solid tide gauge building suggests a remarkable stability of the ground (%$-0.04\pm 0.25%$ mm/year) since 1998, confirming the choice made by our predecessor geodesists in the nineteenth century regarding this site selection. © The Author(s) 2014
abstract_unstemmed	Abstract This paper describes the historical sea level data that we have rescued from a tide gauge, especially devised originally for geodesy. This gauge was installed in Marseille in 1884 with the primary objective of defining the origin of the height system in France. Hourly values for 1885–1988 have been digitized from the original tidal charts. They are supplemented by hourly values from an older tide gauge record (1849–1851) that was rediscovered during a survey in 2009. Both recovered data sets have been critically edited for errors and their reliability assessed. The hourly values are thoroughly analysed for the first time after their original recording. A consistent high-frequency time series is reported, increasing notably the length of one of the few European sea level records in the Mediterranean Sea spanning more than one hundred years. Changes in sea levels are examined, and previous results revisited with the extended time series. The rate of relative sea level change for the period 1849–2012 is estimated to have been %$1.08\pm 0.04%$ mm/year at Marseille, a value that is slightly lower but in close agreement with the longest time series of Brest over the common period (%$1.26\pm 0.04%$ mm/year). The data from a permanent global positioning system station installed on the roof of the solid tide gauge building suggests a remarkable stability of the ground (%$-0.04\pm 0.25%$ mm/year) since 1998, confirming the choice made by our predecessor geodesists in the nineteenth century regarding this site selection. © The Author(s) 2014
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title_short	Rescue of the historical sea level record of Marseille (France) from 1885 to 1988 and its extension back to 1849–1851
url	https://dx.doi.org/10.1007/s00190-014-0728-6
remote_bool	true
author2	Marcos, M. Coulomb, A. Martín Míguez, B. Bonnetain, P. Boucher, C. Gravelle, M. Simon, B. Tiphaneau, P.
author2Str	Marcos, M. Coulomb, A. Martín Míguez, B. Bonnetain, P. Boucher, C. Gravelle, M. Simon, B. Tiphaneau, P.
ppnlink	271175389
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doi_str	10.1007/s00190-014-0728-6
up_date	2024-07-03T23:26:27.040Z
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This gauge was installed in Marseille in 1884 with the primary objective of defining the origin of the height system in France. Hourly values for 1885–1988 have been digitized from the original tidal charts. They are supplemented by hourly values from an older tide gauge record (1849–1851) that was rediscovered during a survey in 2009. Both recovered data sets have been critically edited for errors and their reliability assessed. The hourly values are thoroughly analysed for the first time after their original recording. A consistent high-frequency time series is reported, increasing notably the length of one of the few European sea level records in the Mediterranean Sea spanning more than one hundred years. Changes in sea levels are examined, and previous results revisited with the extended time series. The rate of relative sea level change for the period 1849–2012 is estimated to have been %$1.08\pm 0.04%$ mm/year at Marseille, a value that is slightly lower but in close agreement with the longest time series of Brest over the common period (%$1.26\pm 0.04%$ mm/year). The data from a permanent global positioning system station installed on the roof of the solid tide gauge building suggests a remarkable stability of the ground (%$-0.04\pm 0.25%$ mm/year) since 1998, confirming the choice made by our predecessor geodesists in the nineteenth century regarding this site selection.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Tide gauge</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Levelling</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Sea level</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">History of geodesy</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Marseille</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Marcos, M.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Coulomb, A.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Martín Míguez, B.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Bonnetain, P.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Boucher, C.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Gravelle, M.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Simon, B.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Tiphaneau, P.</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Journal of geodesy</subfield><subfield code="d">Berlin : Springer, 1995</subfield><subfield code="g">88(2014), 9 vom: 08. 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score	7.400346

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Rescue of the historical sea level record of Marseille (France) from 1885 to 1988 and its extension back to 1849–1851

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Zugang & Verfügbarkeit

Vorhandene Bände

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