4.6 Review

Changes in mean sea level around Great Britain over the past 200 years

Journal

PROGRESS IN OCEANOGRAPHY
Volume 192, Issue -, Pages -

Publisher

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.pocean.2021.102521

Keywords

Sea level rise; Sea level acceleration; Mean sea level; Tide gauge; Data archaeology

Categories

Funding

  1. Natural Environment Research Council (NERC) EAO Doctoral Training Partnership
  2. NERC [NE/L002469/1]
  3. UKRI award [1950000]

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The study systematically assimilated historical sea level data around the coast of Great Britain and confirmed a weaker sea level rise trend in the 19th century compared to the 20th century. Adjusted data showed a weighted linear trend of 2.12 mm/year since 1900, with an acceleration of 0.012 mm/yr(2) observed from 1813 to 2018.
We systematically assimilate a wide range of historical sea level data from around the coast of Great Britain, much of it previously unpublished, into a single comprehensive framework. We show that this greatly increased dataset allows the construction of a robust and extended Mean Sea Level curve for Great Britain covering a period of more than two centuries, and confirms that the 19th century trend was much weaker than that in the 20th century and beyond. As well as attempting to maximise the amount of newly recovered sea level observations, we have also recovered the levelling metadata necessary to connect this 19th and early 20th century data with modern records. We adjust this data for known sources of variability and estimate overall uncertainties over the entire period. Data are processed in 36 regional clusters, before recombining to compute national statistics. We investigate the advantages of extending and adjusting the time series on sea level rise trends and low order variability. Confidence limits are improved by better than 60%. The weighted linear trend since 1900 for the fully adjusted data points from all clusters when averaged annually and adjusted for Glacial Isostatic Adjustment is 2.12 mm/year +/- 0.02 mm/year (1-sigma). The much lower trend estimated for the 19th Century alone is 0.24 +/- 0.12 mm/yr. There is an acceleration of 0.012 mm/yr(2) +/- 0.003 mm/yr(2) in the rate of rise over the period 1813 to 2018. These trends are quite sensitive to the GIA correction used, but their differences and accelerations are not.

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