The acceleration of sea-level rise along the coast of the Netherlands started in the 1960s

The global acceleration of sea-level rise (SLR) during the 20th century is now established. On the local scale, this is harder to establish as several drivers of SLR play a role, which can mask the acceleration. Here, we study the rate of SLR along the coast of the Netherlands from the average of si...

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Published in:Ocean Science
Main Authors: Keizer, Iris, Bars, Dewi, Valk, Cees, Jüling, André, Wal, Roderik, Drijfhout, Sybren
Format: Text
Language:English
Published: 2023
Subjects:
Gam
Online Access:https://doi.org/10.5194/os-19-991-2023
https://os.copernicus.org/articles/19/991/2023/
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spelling ftcopernicus:oai:publications.copernicus.org:os106516 2023-07-30T04:05:39+02:00 The acceleration of sea-level rise along the coast of the Netherlands started in the 1960s Keizer, Iris Bars, Dewi Valk, Cees Jüling, André Wal, Roderik Drijfhout, Sybren 2023-07-06 application/pdf https://doi.org/10.5194/os-19-991-2023 https://os.copernicus.org/articles/19/991/2023/ eng eng doi:10.5194/os-19-991-2023 https://os.copernicus.org/articles/19/991/2023/ eISSN: 1812-0792 Text 2023 ftcopernicus https://doi.org/10.5194/os-19-991-2023 2023-07-10T16:24:17Z The global acceleration of sea-level rise (SLR) during the 20th century is now established. On the local scale, this is harder to establish as several drivers of SLR play a role, which can mask the acceleration. Here, we study the rate of SLR along the coast of the Netherlands from the average of six tide gauge records covering the period 1890–2021. To isolate the effects of the wind field variations and the nodal tide from the local sea-level trend, we use four generalised additive models (GAMs) which include different predictive variables. From the sea-level trend estimates, we obtain the continuous evolution of the rate of SLR and its uncertainty over the observational period. The standard error in the estimation of the rate of SLR is reduced when we account for nodal-tide effects and is reduced further when we also account for the wind effects, meaning these provide better estimates of the rate of SLR. A part of the long-term SLR is due to wind forcing related to a strengthening and northward shift of the jet stream, but this SLR contribution decelerated over the observational period. Additionally, we detect wind-forced sea-level variability on multidecadal timescales with an amplitude of around 1 cm. Using a coherence analysis, we identify both the North Atlantic Oscillation and the Atlantic Multidecadal Variability as its drivers. Crucially, accounting for the nodal-tide and wind effects changes the estimated rate of SLR, unmasking an SLR acceleration that started in the 1960s. Our best-fitting GAM, which accounts for nodal and wind effects, yields a rate of SLR of about 1.7 2.2 1.3 <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="28pt" height="15pt" class="svg-formula" dspmath="mathimg" md5hash="9ff72ed2c15a494a31dfe47cfd759cf9"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="os-19-991-2023-ie00001.svg" width="28pt" height="15pt" src="os-19-991-2023-ie00001.png"/></svg:svg> mm yr −1 in 1900–1919 and 1.5 1.9 1.2 <svg:svg xmlns:svg="http://www.w3.org/2000/svg" ... Text North Atlantic North Atlantic oscillation Copernicus Publications: E-Journals Gam ENVELOPE(-57.955,-57.955,-61.923,-61.923) Ocean Science 19 4 991 1007
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description The global acceleration of sea-level rise (SLR) during the 20th century is now established. On the local scale, this is harder to establish as several drivers of SLR play a role, which can mask the acceleration. Here, we study the rate of SLR along the coast of the Netherlands from the average of six tide gauge records covering the period 1890–2021. To isolate the effects of the wind field variations and the nodal tide from the local sea-level trend, we use four generalised additive models (GAMs) which include different predictive variables. From the sea-level trend estimates, we obtain the continuous evolution of the rate of SLR and its uncertainty over the observational period. The standard error in the estimation of the rate of SLR is reduced when we account for nodal-tide effects and is reduced further when we also account for the wind effects, meaning these provide better estimates of the rate of SLR. A part of the long-term SLR is due to wind forcing related to a strengthening and northward shift of the jet stream, but this SLR contribution decelerated over the observational period. Additionally, we detect wind-forced sea-level variability on multidecadal timescales with an amplitude of around 1 cm. Using a coherence analysis, we identify both the North Atlantic Oscillation and the Atlantic Multidecadal Variability as its drivers. Crucially, accounting for the nodal-tide and wind effects changes the estimated rate of SLR, unmasking an SLR acceleration that started in the 1960s. Our best-fitting GAM, which accounts for nodal and wind effects, yields a rate of SLR of about 1.7 2.2 1.3 <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="28pt" height="15pt" class="svg-formula" dspmath="mathimg" md5hash="9ff72ed2c15a494a31dfe47cfd759cf9"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="os-19-991-2023-ie00001.svg" width="28pt" height="15pt" src="os-19-991-2023-ie00001.png"/></svg:svg> mm yr −1 in 1900–1919 and 1.5 1.9 1.2 <svg:svg xmlns:svg="http://www.w3.org/2000/svg" ...
format Text
author Keizer, Iris
Bars, Dewi
Valk, Cees
Jüling, André
Wal, Roderik
Drijfhout, Sybren
spellingShingle Keizer, Iris
Bars, Dewi
Valk, Cees
Jüling, André
Wal, Roderik
Drijfhout, Sybren
The acceleration of sea-level rise along the coast of the Netherlands started in the 1960s
author_facet Keizer, Iris
Bars, Dewi
Valk, Cees
Jüling, André
Wal, Roderik
Drijfhout, Sybren
author_sort Keizer, Iris
title The acceleration of sea-level rise along the coast of the Netherlands started in the 1960s
title_short The acceleration of sea-level rise along the coast of the Netherlands started in the 1960s
title_full The acceleration of sea-level rise along the coast of the Netherlands started in the 1960s
title_fullStr The acceleration of sea-level rise along the coast of the Netherlands started in the 1960s
title_full_unstemmed The acceleration of sea-level rise along the coast of the Netherlands started in the 1960s
title_sort acceleration of sea-level rise along the coast of the netherlands started in the 1960s
publishDate 2023
url https://doi.org/10.5194/os-19-991-2023
https://os.copernicus.org/articles/19/991/2023/
long_lat ENVELOPE(-57.955,-57.955,-61.923,-61.923)
geographic Gam
geographic_facet Gam
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_source eISSN: 1812-0792
op_relation doi:10.5194/os-19-991-2023
https://os.copernicus.org/articles/19/991/2023/
op_doi https://doi.org/10.5194/os-19-991-2023
container_title Ocean Science
container_volume 19
container_issue 4
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