Seychelles Damage, Loss, and Needs Assessment (DaLA ... - GFDRR
Seychelles Damage, Loss, and Needs Assessment (DaLA ... - GFDRR
Seychelles Damage, Loss, and Needs Assessment (DaLA ... - GFDRR
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appendix 3<br />
49<br />
Figure A3.2 Time Series of Pointe Larue Monthly Observed Sea-Level Anomaly<br />
30<br />
Point La Rue 04 40S 055 32E <strong>Seychelles</strong> 1993–2006<br />
20<br />
10<br />
cm<br />
0<br />
-10<br />
-20<br />
-30<br />
1986 1988 1990 1992 1994 1996 1998 2000 2002 2004 2006<br />
Source: University of Hawaii.<br />
Note: The red curve represents smooth sea level.<br />
Sea-Level Rise<br />
Sea-level variability in the last few years has also been<br />
influenced by extreme equatorial <strong>and</strong> mid-latitude<br />
generated storm surge <strong>and</strong> swells. Sea-level monitoring<br />
in the <strong>Seychelles</strong> began in 1993 (figure A3.2).<br />
Status<br />
Recently, there has been a notable increase in the gradient<br />
of the mean sea-level slope, as highlighted by an<br />
arrow on the sea-level time series (figure A3.2). From<br />
2002 to 2006, there were five instances when sea-level<br />
anomaly exceeded +10 cm. Consequently, although<br />
not properly documented, there have been increased<br />
reports of coastal impacts.<br />
Trends<br />
Chang-Seng (2007) suggests an annual sea-level<br />
trend anomaly of +1.46 mm (± 2.11 mm) per year on<br />
Mahé Isl<strong>and</strong> (figure A3.3), which is very close to Ragoonaden’s<br />
(2006) estimate of +1.69 mm/year. Most<br />
stations in the southwest Indian Ocean are reporting<br />
a similar positive trend. The local sea-level rise is also<br />
consistent with the global average sea-level rise, with<br />
an average rate of +1.8 mm (1.3 to 2.3 mm) per year<br />
over the 1961 to 2003 period.<br />
The sea-level variability in the last few years has also<br />
been influenced by extreme equatorial <strong>and</strong> mid-latitude<br />
generated storm surges <strong>and</strong> swells, as was the<br />
case with cyclone Bondo in December 2006 <strong>and</strong> the<br />
latest high-wave event, which unfolded over May 13–<br />
20, 2007.<br />
Rainfall Trends<br />
Annual rainfall anomaly trends on Mahé for the period<br />
1972 to 2006 are upward by 13.7 mm per year,<br />
indicating a wetter climate. However, these trends may<br />
have been distorted by heavy rainfall events rather<br />
than subtle changes in rainfall. The effects of the El<br />
Niño Southern Oscillation (ENSO) are also observed, in<br />
particular in 1998, when it caused mass coral bleaching<br />
<strong>and</strong> significant damage to the <strong>Seychelles</strong>’ economy.