2008Geophysical Research LettersOpen access

Tide gauge datum continuity at Brest since 1711: France's longest sea‐level record

Guy Wöppelmann, Nicolas Pouvreau, Alain Coulomb, Bernard Simon, Philip Woodworth

Open full text 84 citations

Abstract

The issue of a possible tide gauge datum discontinuity at Brest, caused by the bombing of the city in August 1944, is discussed. This issue is very important, as many scientists have used this long record to derive a long‐term sea level trend estimate for use within global sea level rise studies. A detailed analysis of historical leveling information, and comparison of sea level data between adjacent stations, proved to be worthwhile, even beyond this initial scope of the study: it led to an accurate datum connection between recently rediscovered 18th century sea level data (back to 1711) and those of the present day. The study provides additional evidence that the onset of recent rapid sea level rise most likely took place in the late 19th century, in agreement with the nearby Liverpool sea‐level record and with independent results from sediment cores collected in salt marshes located in both hemispheres.

Open-access reader

About this research paper

What this paper is about

The issue of a possible tide gauge datum discontinuity at Brest, caused by the bombing of the city in August 1944, is discussed. This issue is very important, as many scientists have used this long record to derive a long‐term sea level trend estimate for use within global sea level rise studies. A detailed analysis of historical leveling information, and comparison of sea level data between adjacent stations, proved to be worthwhile, even beyond this initial scope of the study: it led to an accurate datum connection between recently rediscovered 18th century sea level data (back to 1711) and those of the present day. The study provides additional evidence that the onset of recent rapid sea level rise most likely took place in the late 19th century, in agreement with the nearby Liverpool sea‐level record and with independent results from sediment cores collected in salt marshes located in both hemispheres.

Why it matters

OpenAlex reports 84 citations for this work. Citation counts describe recorded attention and do not establish research quality.

Key contribution

A contribution statement is not available in the OpenAlex record.

Method / approach

Method details are not available in the OpenAlex metadata.

Main findings

Findings are not separately available in the OpenAlex metadata.

Limitations

Limitations are not available in the OpenAlex metadata.

Applications

Application details are not available in the OpenAlex metadata.

Available abstract

The issue of a possible tide gauge datum discontinuity at Brest, caused by the bombing of the city in August 1944, is discussed. This issue is very important, as many scientists have used this long record to derive a long‐term sea level trend estimate for use within global sea level rise studies. A detailed analysis of historical leveling information, and comparison of sea level data between adjacent stations, proved to be worthwhile, even beyond this initial scope of the study: it led to an accurate datum connection between recently rediscovered 18th century sea level data (back to 1711) and those of the present day. The study provides additional evidence that the onset of recent rapid sea level rise most likely took place in the late 19th century, in agreement with the nearby Liverpool sea‐level record and with independent results from sediment cores collected in salt marshes located in both hemispheres.

Key concepts: Tide gauge, Sea level, Geodetic datum, Sea level rise, Sea level change, Gauge (firearms), Geology, Salt marsh

Related papers

Back to paper searchBrowse research topicsOriginal source
Tide gauge datum continuity at Brest since 1711: France's longest sea‐level record — Research Paper | ScholarLens