The pattern of sea-level rise across the North Atlantic from long-term-trend tide gauges

The long-term-trend tide gauges have monthly average mean sea levels oscillating about the same perfectly linear trend before and after 1990, across the North Atlantic, same of every other water basin. This stable pattern is clear over the full length of the records starting in the late 1800s/early...
Ausführliche Beschreibung

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Autor*in:	Boretti, Alberto [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2020

Schlagwörter:	GPS data Extreme sea levels AMOC Relative sea-level change Relative sea-level rise

Übergeordnetes Werk:	Enthalten in: Ocean & coastal management - Amsterdam [u.a.] : Elsevier Science, 1992, 196
Übergeordnetes Werk:	volume:196

DOI / URN:	10.1016/j.ocecoaman.2020.105309

Katalog-ID:	ELV004662164

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520			\|a The long-term-trend tide gauges have monthly average mean sea levels oscillating about the same perfectly linear trend before and after 1990, across the North Atlantic, same of every other water basin. This stable pattern is clear over the full length of the records starting in the late 1800s/early 1900s having negligible acceleration. Across the North Atlantic, the absolute rate of rise of the sea levels, computed by coupling the monthly average mean sea levels signal with the position signal from Global Positioning System, is also about the same. The absolute sea levels of New York, U.S. and Brest, France, have a similar pattern since 1854. Measurements of the 41 °N Atlantic Meridional Overturning Circulation based on the Array for Real-time Geostrophic Oceanography and satellite altimetry, also show stable strength, since 1990. A proxy of this Overturning Circulation linked to the absolute mean sea levels of New York and Brest also show stability since 1854. Coastal management should acknowledge this fact.
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allfields	10.1016/j.ocecoaman.2020.105309 doi (DE-627)ELV004662164 (ELSEVIER)S0964-5691(20)30219-2 DE-627 ger DE-627 rda eng 330 550 380 DE-600 38.90 bkl 38.00 bkl 74.15 bkl Boretti, Alberto verfasserin aut The pattern of sea-level rise across the North Atlantic from long-term-trend tide gauges 2020 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The long-term-trend tide gauges have monthly average mean sea levels oscillating about the same perfectly linear trend before and after 1990, across the North Atlantic, same of every other water basin. This stable pattern is clear over the full length of the records starting in the late 1800s/early 1900s having negligible acceleration. Across the North Atlantic, the absolute rate of rise of the sea levels, computed by coupling the monthly average mean sea levels signal with the position signal from Global Positioning System, is also about the same. The absolute sea levels of New York, U.S. and Brest, France, have a similar pattern since 1854. Measurements of the 41 °N Atlantic Meridional Overturning Circulation based on the Array for Real-time Geostrophic Oceanography and satellite altimetry, also show stable strength, since 1990. A proxy of this Overturning Circulation linked to the absolute mean sea levels of New York and Brest also show stability since 1854. Coastal management should acknowledge this fact. GPS data Extreme sea levels AMOC Relative sea-level change Relative sea-level rise Enthalten in Ocean & coastal management Amsterdam [u.a.] : Elsevier Science, 1992 196 Online-Ressource (DE-627)306363763 (DE-600)1497382-0 (DE-576)259484091 0964-5691 nnns volume:196 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 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_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.90 Ozeanologie Ozeanographie 38.00 Geowissenschaften: Allgemeines 74.15 Großgebiete Geographie AR 196
spelling	10.1016/j.ocecoaman.2020.105309 doi (DE-627)ELV004662164 (ELSEVIER)S0964-5691(20)30219-2 DE-627 ger DE-627 rda eng 330 550 380 DE-600 38.90 bkl 38.00 bkl 74.15 bkl Boretti, Alberto verfasserin aut The pattern of sea-level rise across the North Atlantic from long-term-trend tide gauges 2020 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The long-term-trend tide gauges have monthly average mean sea levels oscillating about the same perfectly linear trend before and after 1990, across the North Atlantic, same of every other water basin. This stable pattern is clear over the full length of the records starting in the late 1800s/early 1900s having negligible acceleration. Across the North Atlantic, the absolute rate of rise of the sea levels, computed by coupling the monthly average mean sea levels signal with the position signal from Global Positioning System, is also about the same. The absolute sea levels of New York, U.S. and Brest, France, have a similar pattern since 1854. Measurements of the 41 °N Atlantic Meridional Overturning Circulation based on the Array for Real-time Geostrophic Oceanography and satellite altimetry, also show stable strength, since 1990. A proxy of this Overturning Circulation linked to the absolute mean sea levels of New York and Brest also show stability since 1854. Coastal management should acknowledge this fact. GPS data Extreme sea levels AMOC Relative sea-level change Relative sea-level rise Enthalten in Ocean & coastal management Amsterdam [u.a.] : Elsevier Science, 1992 196 Online-Ressource (DE-627)306363763 (DE-600)1497382-0 (DE-576)259484091 0964-5691 nnns volume:196 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 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_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.90 Ozeanologie Ozeanographie 38.00 Geowissenschaften: Allgemeines 74.15 Großgebiete Geographie AR 196
allfields_unstemmed	10.1016/j.ocecoaman.2020.105309 doi (DE-627)ELV004662164 (ELSEVIER)S0964-5691(20)30219-2 DE-627 ger DE-627 rda eng 330 550 380 DE-600 38.90 bkl 38.00 bkl 74.15 bkl Boretti, Alberto verfasserin aut The pattern of sea-level rise across the North Atlantic from long-term-trend tide gauges 2020 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The long-term-trend tide gauges have monthly average mean sea levels oscillating about the same perfectly linear trend before and after 1990, across the North Atlantic, same of every other water basin. This stable pattern is clear over the full length of the records starting in the late 1800s/early 1900s having negligible acceleration. Across the North Atlantic, the absolute rate of rise of the sea levels, computed by coupling the monthly average mean sea levels signal with the position signal from Global Positioning System, is also about the same. The absolute sea levels of New York, U.S. and Brest, France, have a similar pattern since 1854. Measurements of the 41 °N Atlantic Meridional Overturning Circulation based on the Array for Real-time Geostrophic Oceanography and satellite altimetry, also show stable strength, since 1990. A proxy of this Overturning Circulation linked to the absolute mean sea levels of New York and Brest also show stability since 1854. Coastal management should acknowledge this fact. GPS data Extreme sea levels AMOC Relative sea-level change Relative sea-level rise Enthalten in Ocean & coastal management Amsterdam [u.a.] : Elsevier Science, 1992 196 Online-Ressource (DE-627)306363763 (DE-600)1497382-0 (DE-576)259484091 0964-5691 nnns volume:196 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 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_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.90 Ozeanologie Ozeanographie 38.00 Geowissenschaften: Allgemeines 74.15 Großgebiete Geographie AR 196
allfieldsGer	10.1016/j.ocecoaman.2020.105309 doi (DE-627)ELV004662164 (ELSEVIER)S0964-5691(20)30219-2 DE-627 ger DE-627 rda eng 330 550 380 DE-600 38.90 bkl 38.00 bkl 74.15 bkl Boretti, Alberto verfasserin aut The pattern of sea-level rise across the North Atlantic from long-term-trend tide gauges 2020 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The long-term-trend tide gauges have monthly average mean sea levels oscillating about the same perfectly linear trend before and after 1990, across the North Atlantic, same of every other water basin. This stable pattern is clear over the full length of the records starting in the late 1800s/early 1900s having negligible acceleration. Across the North Atlantic, the absolute rate of rise of the sea levels, computed by coupling the monthly average mean sea levels signal with the position signal from Global Positioning System, is also about the same. The absolute sea levels of New York, U.S. and Brest, France, have a similar pattern since 1854. Measurements of the 41 °N Atlantic Meridional Overturning Circulation based on the Array for Real-time Geostrophic Oceanography and satellite altimetry, also show stable strength, since 1990. A proxy of this Overturning Circulation linked to the absolute mean sea levels of New York and Brest also show stability since 1854. Coastal management should acknowledge this fact. GPS data Extreme sea levels AMOC Relative sea-level change Relative sea-level rise Enthalten in Ocean & coastal management Amsterdam [u.a.] : Elsevier Science, 1992 196 Online-Ressource (DE-627)306363763 (DE-600)1497382-0 (DE-576)259484091 0964-5691 nnns volume:196 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 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_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.90 Ozeanologie Ozeanographie 38.00 Geowissenschaften: Allgemeines 74.15 Großgebiete Geographie AR 196
allfieldsSound	10.1016/j.ocecoaman.2020.105309 doi (DE-627)ELV004662164 (ELSEVIER)S0964-5691(20)30219-2 DE-627 ger DE-627 rda eng 330 550 380 DE-600 38.90 bkl 38.00 bkl 74.15 bkl Boretti, Alberto verfasserin aut The pattern of sea-level rise across the North Atlantic from long-term-trend tide gauges 2020 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The long-term-trend tide gauges have monthly average mean sea levels oscillating about the same perfectly linear trend before and after 1990, across the North Atlantic, same of every other water basin. This stable pattern is clear over the full length of the records starting in the late 1800s/early 1900s having negligible acceleration. Across the North Atlantic, the absolute rate of rise of the sea levels, computed by coupling the monthly average mean sea levels signal with the position signal from Global Positioning System, is also about the same. The absolute sea levels of New York, U.S. and Brest, France, have a similar pattern since 1854. Measurements of the 41 °N Atlantic Meridional Overturning Circulation based on the Array for Real-time Geostrophic Oceanography and satellite altimetry, also show stable strength, since 1990. A proxy of this Overturning Circulation linked to the absolute mean sea levels of New York and Brest also show stability since 1854. Coastal management should acknowledge this fact. GPS data Extreme sea levels AMOC Relative sea-level change Relative sea-level rise Enthalten in Ocean & coastal management Amsterdam [u.a.] : Elsevier Science, 1992 196 Online-Ressource (DE-627)306363763 (DE-600)1497382-0 (DE-576)259484091 0964-5691 nnns volume:196 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 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_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.90 Ozeanologie Ozeanographie 38.00 Geowissenschaften: Allgemeines 74.15 Großgebiete Geographie AR 196
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author	Boretti, Alberto
spellingShingle	Boretti, Alberto ddc 330 bkl 38.90 bkl 38.00 bkl 74.15 misc GPS data misc Extreme sea levels misc AMOC misc Relative sea-level change misc Relative sea-level rise The pattern of sea-level rise across the North Atlantic from long-term-trend tide gauges
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title	The pattern of sea-level rise across the North Atlantic from long-term-trend tide gauges
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title_full	The pattern of sea-level rise across the North Atlantic from long-term-trend tide gauges
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title_sort	the pattern of sea-level rise across the north atlantic from long-term-trend tide gauges
title_auth	The pattern of sea-level rise across the North Atlantic from long-term-trend tide gauges
abstract	The long-term-trend tide gauges have monthly average mean sea levels oscillating about the same perfectly linear trend before and after 1990, across the North Atlantic, same of every other water basin. This stable pattern is clear over the full length of the records starting in the late 1800s/early 1900s having negligible acceleration. Across the North Atlantic, the absolute rate of rise of the sea levels, computed by coupling the monthly average mean sea levels signal with the position signal from Global Positioning System, is also about the same. The absolute sea levels of New York, U.S. and Brest, France, have a similar pattern since 1854. Measurements of the 41 °N Atlantic Meridional Overturning Circulation based on the Array for Real-time Geostrophic Oceanography and satellite altimetry, also show stable strength, since 1990. A proxy of this Overturning Circulation linked to the absolute mean sea levels of New York and Brest also show stability since 1854. Coastal management should acknowledge this fact.
abstractGer	The long-term-trend tide gauges have monthly average mean sea levels oscillating about the same perfectly linear trend before and after 1990, across the North Atlantic, same of every other water basin. This stable pattern is clear over the full length of the records starting in the late 1800s/early 1900s having negligible acceleration. Across the North Atlantic, the absolute rate of rise of the sea levels, computed by coupling the monthly average mean sea levels signal with the position signal from Global Positioning System, is also about the same. The absolute sea levels of New York, U.S. and Brest, France, have a similar pattern since 1854. Measurements of the 41 °N Atlantic Meridional Overturning Circulation based on the Array for Real-time Geostrophic Oceanography and satellite altimetry, also show stable strength, since 1990. A proxy of this Overturning Circulation linked to the absolute mean sea levels of New York and Brest also show stability since 1854. Coastal management should acknowledge this fact.
abstract_unstemmed	The long-term-trend tide gauges have monthly average mean sea levels oscillating about the same perfectly linear trend before and after 1990, across the North Atlantic, same of every other water basin. This stable pattern is clear over the full length of the records starting in the late 1800s/early 1900s having negligible acceleration. Across the North Atlantic, the absolute rate of rise of the sea levels, computed by coupling the monthly average mean sea levels signal with the position signal from Global Positioning System, is also about the same. The absolute sea levels of New York, U.S. and Brest, France, have a similar pattern since 1854. Measurements of the 41 °N Atlantic Meridional Overturning Circulation based on the Array for Real-time Geostrophic Oceanography and satellite altimetry, also show stable strength, since 1990. A proxy of this Overturning Circulation linked to the absolute mean sea levels of New York and Brest also show stability since 1854. Coastal management should acknowledge this fact.
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title_short	The pattern of sea-level rise across the North Atlantic from long-term-trend tide gauges
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up_date	2024-07-06T23:44:33.649Z
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This stable pattern is clear over the full length of the records starting in the late 1800s/early 1900s having negligible acceleration. Across the North Atlantic, the absolute rate of rise of the sea levels, computed by coupling the monthly average mean sea levels signal with the position signal from Global Positioning System, is also about the same. The absolute sea levels of New York, U.S. and Brest, France, have a similar pattern since 1854. Measurements of the 41 °N Atlantic Meridional Overturning Circulation based on the Array for Real-time Geostrophic Oceanography and satellite altimetry, also show stable strength, since 1990. A proxy of this Overturning Circulation linked to the absolute mean sea levels of New York and Brest also show stability since 1854. 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The pattern of sea-level rise across the North Atlantic from long-term-trend tide gauges

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