Trends in components of sea level around the English Channel
Trends in components of sea level around the English Channel
The longest available records of hourly sea level data have been analysed for six ports around
the English Channel. The quality of the data is extremely variable with the longest and most
reliable records belonging to Brest and Newlyn. A separate analysis of the components of sea
level: mean sea level, tides and meteorological residuals (surges), is used. Results show a
general increase in mean sea level throughout the period of observation. The various tidal
constituents show interesting local short-term variations in amplitude and phase but no longterm
trends. There is no evidence of an increase in weather effects on sea levels over the
period analysed. De-trended sea level and pressure values show annual sea level fall as annual
air pressures increase, as expected for the inverse barometer response. Meteorological
residuals were compared to North Atlantic Oscillation (NAO) index values. The correlations
are in general very small, especially for the annual mean NAO values. However correlations
are slightly more apparent for the annual winter mean NAO values.
9728558090
107-114
Araujo, I.
3fb34735-76aa-4b54-ad17-38faf7c79b48
Pugh, D.
ec256ec5-072b-4c4b-8ced-471c277803ff
Collins, M.
3b70278b-0004-45e0-b3c9-0debdf0a9351
2002
Araujo, I.
3fb34735-76aa-4b54-ad17-38faf7c79b48
Pugh, D.
ec256ec5-072b-4c4b-8ced-471c277803ff
Collins, M.
3b70278b-0004-45e0-b3c9-0debdf0a9351
Araujo, I., Pugh, D. and Collins, M.
(2002)
Trends in components of sea level around the English Channel.
In Littoral 2002: The Changing Coast.
EUROCOAST.
.
Record type:
Conference or Workshop Item
(Paper)
Abstract
The longest available records of hourly sea level data have been analysed for six ports around
the English Channel. The quality of the data is extremely variable with the longest and most
reliable records belonging to Brest and Newlyn. A separate analysis of the components of sea
level: mean sea level, tides and meteorological residuals (surges), is used. Results show a
general increase in mean sea level throughout the period of observation. The various tidal
constituents show interesting local short-term variations in amplitude and phase but no longterm
trends. There is no evidence of an increase in weather effects on sea levels over the
period analysed. De-trended sea level and pressure values show annual sea level fall as annual
air pressures increase, as expected for the inverse barometer response. Meteorological
residuals were compared to North Atlantic Oscillation (NAO) index values. The correlations
are in general very small, especially for the annual mean NAO values. However correlations
are slightly more apparent for the annual winter mean NAO values.
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Published date: 2002
Venue - Dates:
conference; 2002-09-22; 2002-09-26, Porto, Portugal, 2002-09-22 - 2002-09-26
Identifiers
Local EPrints ID: 44350
URI: http://eprints.soton.ac.uk/id/eprint/44350
ISBN: 9728558090
PURE UUID: 125e7404-8b55-4635-b29c-ba92143f93cd
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Date deposited: 27 Feb 2007
Last modified: 15 Mar 2024 09:03
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Contributors
Author:
I. Araujo
Author:
D. Pugh
Author:
M. Collins
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