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| HISTORICAL TIDE
GAUGE MEASUREMENTS
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Traditionally, global sea level change has
been estimated from tide gauge measurements collected over the last
century. Tide gauges, usually placed on piers, measure the sea level
relative to a nearby geodetic benchmark. Shown in Figure 1 is the most
commonly used tide gauge measurement system, a float operating in a
stilling well. Surveys of the tide gauge site are performed regularly
to account for any settling of the site. Tide gauges may also move
vertically with the region as a result of post-glacial rebound,
tectonic
uplift or crustal subsidence. This greatly complicates the problem of
determining global sea level change from tide gauge data. Differences
in global sea level estimates from tide gauge data usually reflect the
investigator's approach in considering these vertical crustal
movements. Tide gauges also monitor meteorological factors that affect
sea levels, such as barometric pressure and windspeed, so
that these variable factors can be eliminated from long-term
assessments of sea level change. Although the global network of tide
gauges comprises of a poorly distributed sea level measurement system,
it offers the only source of historical, precise, long-term sea level
data. Major conclusions from tide gauge data have been that global sea
level has risen approximately 10-25 cm during the past century.
TIDE GAUGE ESTIMATES OF
GLOBAL SEA LEVEL RISE
Estimates of global sea level rise which were
derived from tide gauge records are found in Table 1. Most of the
investigators reported that the estimated values were sensitive to the
choice of record length and the tide gauges selected. This sensitivity
coupled with different computationa techniques and modeling would
certainly explain some of the differences shown below.
Table 1: Estimates of
Global Sea Level Rise from Tide Gauge Records
Sea Level
Rise (mm/yr) |
Error
(mm/yr) |
Data Used
(years) |
# of Tide Gauge Stations |
References |
| 1.43 |
±0.14 |
1881-1980 |
152 |
Barnett, 1984 |
| 2.27 |
±0.23 |
1930-1980 |
152 |
Barnett, 1984 |
| 1.2 |
±0.3 |
1880-1982 |
130 |
Gornitz & Lebedeff, 1987 |
| 2.4 |
±0.9 |
1920-1970 |
40 |
Peltier & Tushingham, 1989 |
| 1.75 |
±0.13 |
1900-1979 |
84 |
Trupin & Wahr, 1990 |
| 1.7 |
±0.5 |
N/A |
N/A |
Nakiboglu & Lambeck, 1991 |
| 1.8 |
±0.1 |
1880-1980 |
21 |
Douglas, 1991 |
| 1.62 |
±0.38 |
1807-1988 |
213 |
Unal & Ghil, 1995 |
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