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...
| Main Authors: | , , , , , |
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| Format: | Text |
| Language: | English |
| Published: |
2023
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| Subjects: | |
| Online Access: | https://doi.org/10.5194/egusphere-2022-935 https://egusphere.copernicus.org/preprints/2022/egusphere-2022-935/ |
| Summary: | 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" ... |
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