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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50<br />
<strong>Seychelles</strong> <strong>Damage</strong>, <strong>Loss</strong> <strong>and</strong> <strong>Needs</strong> <strong>Assessment</strong> (<strong>DaLA</strong>) 2013 Floods<br />
Figure A3.3 Time Series of Mahé Isl<strong>and</strong> Monthly Sea-Level Anomaly<br />
SLA = + 0.1426x – 284.91<br />
1992 1993 1994 1995 1996 1997 1998 1999 2000 2001 2002 2003 2004<br />
Projection<br />
The <strong>Seychelles</strong> is highly vulnerable to climate change.<br />
It is concluded that it is likely (50–80%) that rainfall for<br />
the December–February season <strong>and</strong> the annual rainfall<br />
will increase, <strong>and</strong> it is unlikely to increase in the June–<br />
August season (20–40%).<br />
In addition, as indicated by the recent event in late<br />
January, trends over the past years indicate that the<br />
<strong>Seychelles</strong> is becoming subject to more erratic rainfall<br />
patterns with short bursts of intense rain in hourly periods<br />
rather than more extended periods of steady rainfall<br />
over 2–3 days. This pattern may have contributed<br />
to the recent flooding of January 27–28, 2013, which<br />
included flooding in low-lying areas, l<strong>and</strong>slides, <strong>and</strong><br />
contaminated runoff breaking through natural barriers<br />
along the coast to the beaches <strong>and</strong> the coastal zone.<br />
Coastal Inundation <strong>and</strong> Erosion<br />
<strong>Seychelles</strong>’ coastal zones are under almost constant<br />
pressure from both natural <strong>and</strong> man-made causes.<br />
Anse Kerlan on Praslin is a case in which human interference<br />
has completely destabilized the coastline.<br />
Erosion-sensitive sites on Mahé <strong>and</strong> Praslin are being<br />
lost at an average of between 1 <strong>and</strong> 3 meters per year<br />
(Tsunami Disaster Task Force 2005 <strong>and</strong> the <strong>Seychelles</strong>’<br />
Nation 1998). Noticeable changes in the wave energy<br />
reaching the shores have occurred during the past decade.<br />
Greater wave energy results in greater erosion<br />
of the beaches. Climate change will exacerbate these<br />
problems <strong>and</strong> lead to further destabilization of the<br />
coastline.<br />
Flooding in the low-lying areas is already becoming<br />
more pronounced, especially with the occurrence of<br />
storms that coincide with the spring tides. The recent<br />
floods fit within this pattern <strong>and</strong> were further compounded<br />
by the lack of appropriate drainage <strong>and</strong> highdensity<br />
developments (as discussed in the section on<br />
damage <strong>and</strong> losses in the environment sector).<br />
Trends<br />
Erosion along some of the coastlines has caused the<br />
roots of existing coastal vegetation to be denuded, as<br />
is the case at Anse Sevère on La Digue, <strong>and</strong> as a result,<br />
breaks at certain spots <strong>and</strong> beach cliffs are formed.<br />
Similar effects have been seen on Mahé at Anse aux<br />
Pins beach as a result of the recent disaster.