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Assessment of Capacity Gaps and Needs of South East Asia Countries<br />

in Addressing Impacts, Vulnerability and Adaptati<strong>on</strong> to <strong>Climate</strong> Variability and <strong>Climate</strong> <strong>Change</strong><br />

2007). 30% of the cycl<strong>on</strong>es passing<br />

the Philippines are c<strong>on</strong>sidered<br />

destructive (RMSI, 2007). Table 6<br />

show the top five natural disasters<br />

– with respect to the number of<br />

people affected. Also, over all the<br />

natural hazard events c<strong>on</strong>cerning<br />

climatic disasters, i.e. storms,<br />

draughts and floods, between 1980<br />

- 2009, storms were resp<strong>on</strong>sible<br />

for 84% of all the people affected<br />

(see Figure 18) and 83% of all the<br />

ec<strong>on</strong>omic damages caused (see<br />

Figure 19) within this time period.<br />

Table_6<br />

Overview <strong>on</strong> natural disasters in the<br />

Philippines from 1980 to 2009<br />

Top 5 Natural Disasters in the Philippines, 1980-2009<br />

Type of natural<br />

disaster<br />

Date/year<br />

Storm Nov 1990 6,159,569<br />

Storm Jun 2008 4,785,460<br />

Storm Sep 2009 4,321,149<br />

Storm Oct 1998 3,902,424<br />

Storm Sep 2006 3,842,406<br />

No of people<br />

affected<br />

Fluctuati<strong>on</strong> in the seas<strong>on</strong>al rainfall<br />

distributi<strong>on</strong> is observed in the<br />

Philippines. This is <strong>on</strong>e of the<br />

distinctive effects of the El Niño<br />

Southern Oscillati<strong>on</strong> (ENSO)<br />

phenomen<strong>on</strong> that is associated<br />

with ENSO warm (cold) events.<br />

For the decades between 1950 and<br />

2005, seven El Nino and La Nina<br />

episodes have occurred exhibiting<br />

certain climatic changes. For<br />

example, the seas<strong>on</strong>al rainfall<br />

resp<strong>on</strong>se to ENSO turned sign<br />

between boreal summer (July<br />

- September) and fall (October -<br />

December) for both, El Niño and La Niña. <strong>Change</strong>s<br />

in the large-scale m<strong>on</strong>so<strong>on</strong> system occurred during<br />

the ENSO events that brought drought and flood<br />

c<strong>on</strong>diti<strong>on</strong>s (Ly<strong>on</strong> et al., 2006, cited in RMSI, 2007).<br />

Meanwhile, significant decrease in the number of<br />

Figure 19: Percentage of damage (US$)<br />

due to total natural disasters<br />

1980-2009<br />

Flood 16%<br />

Total Natural* Disasters in the Philippines for the period 1980-2009<br />

Type of<br />

natural<br />

disaster<br />

Total no of<br />

events<br />

No of<br />

people<br />

affected<br />

Damage<br />

000 US$<br />

Storm 192 90,765,856 5,045,830<br />

Drought 7 6,549,542 64,453<br />

Flood 84 10,546,024 981,557<br />

*not c<strong>on</strong>sidered are earthquake, epidemic, insect infestati<strong>on</strong>, wet or dry mass<br />

movement, volcano, and wildfire<br />

Source: EM-DAT (2009) The OFDA /CRED; Internati<strong>on</strong>al Disaster Database; www.emdat.net<br />

- Université Catholique de Louvain – Brussels, – Belgium.<br />

rain days is observed in some areas since 1961<br />

throughout Southeast Asia (Mant<strong>on</strong> et al., 2001,<br />

cited in GRID-Arendal, 2003).<br />

Sea levels have risen partly due to local subsidence<br />

particularly in the Manila area and partly due to<br />

global sea level rise (Hulme and Sheard, 1999, cited<br />

in ADB, 2009c).<br />

<strong>Climate</strong> Projecti<strong>on</strong>s<br />

<strong>Climate</strong> change is expected to exacerbate existing<br />

climatic hazards by creating more flood, drought,<br />

and storm events (val Aalst, 2006, cited in RMSI,<br />

2007).<br />

Drought 1%<br />

Storm 83%<br />

<strong>Climate</strong> change projecti<strong>on</strong> studies show that<br />

temperatures are expected to rise by 2.2 °C by<br />

the last quarter of the 21st century (World Bank,<br />

2005). In additi<strong>on</strong>, not <strong>on</strong>ly are rainfall patterns and<br />

substantial sea level rise projected, but also changes<br />

in climate variability and extreme weather events are<br />

anticipated to entail higher intensity in rainfall, hot<br />

spells and m<strong>on</strong>so<strong>on</strong> rainfall variability (Amadore,<br />

2005). Moreover, peak wind and precipitati<strong>on</strong><br />

intensity of tropical cycl<strong>on</strong>es are likely to increase in<br />

some areas of the Philippines (ibid).<br />

55

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