10.11.2013 Views

Seychelles Damage, Loss, and Needs Assessment (DaLA ... - GFDRR

Seychelles Damage, Loss, and Needs Assessment (DaLA ... - GFDRR

Seychelles Damage, Loss, and Needs Assessment (DaLA ... - GFDRR

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

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.

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!