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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 />

Figure 10: Percentage of people affected<br />

due to top 5 natural disasters:<br />

1980-2009<br />

Drought 0%<br />

Figure 11: Percentage of people affected<br />

due to total natural climatic<br />

disasters: 1980-2009<br />

Drought 9%<br />

Flood 30%<br />

Flood 32%<br />

Storm 70%<br />

Storm 59%<br />

Figure 12: Percentage of damage (US$)<br />

due to total natural disasters:<br />

1980-2009<br />

Drought 9%<br />

Flood 37%<br />

Storm 54%<br />

change <strong>on</strong> coastal z<strong>on</strong>es, the scenario of sea level rise<br />

of 1m by 2100 was used. In the report, the potential<br />

evapotranspirati<strong>on</strong> was calculated using the<br />

modified Penman formulae and the models RRMOD<br />

and SSARR were used for calculating and assessing<br />

the variati<strong>on</strong> of annual run-off, low flow and flood<br />

flow according to the respective scenarios. However,<br />

this vulnerability and adaptati<strong>on</strong> assessment is<br />

largely qualitative, and hence, the results should<br />

<strong>on</strong>ly be regarded as preliminary.<br />

The Sea level rise scenarios for Viet Nam are d<strong>on</strong>e<br />

by the MoNRE under the Nati<strong>on</strong>al Target Program<br />

for climate change resp<strong>on</strong>se. The methodology used<br />

are MAGICC / SCENGE 5.3 software and statistical<br />

downscaling methods and criteria: plausibility of<br />

global climate change scenarios, level of details<br />

of climate change scenarios, inheritability, local<br />

appropriateness, completeness of scenarios and<br />

possibility for self updates. To develop the climate<br />

change scenarios, the study used three different<br />

greenhouse emissi<strong>on</strong> scenarios, low emissi<strong>on</strong><br />

scenario, intermediate emissi<strong>on</strong> scenario of the<br />

medium scenario group and intermediate emissi<strong>on</strong><br />

scenario of the high scenario group. Also, the<br />

temperature and rainfall scenarios are developed<br />

for seven different climate z<strong>on</strong>es: North West, North<br />

East, North Delta, North Central, South Central,<br />

Central Highlands and South.<br />

Some of the other studies reviewed are Trung’s study,<br />

which focuses <strong>on</strong> the strategic plan for integrated<br />

water resources management of the Vu Gia-Thu<br />

basin organizati<strong>on</strong> (Trung, unknown): the <strong>Climate</strong><br />

<strong>Change</strong> and Human Development Report in Viet<br />

Nam (Chaudry and Ruysschaert, 2007); the World<br />

Bank series for envir<strong>on</strong>mental m<strong>on</strong>itoring ‘Adapting<br />

to <strong>Climate</strong> <strong>Change</strong>’; and the ADAPTS program about<br />

adaptive water management at a local scale in Viet<br />

Nam (My et al., 2008).<br />

Impacts <strong>on</strong> the Water Sector<br />

According to the Human Development Report<br />

(Chaudry and Ruysschaert, 2007), the temperature<br />

has been increasing 0.1°C per decade since 1990,<br />

and is expected to increase from 1.4-1.5°C by 2050<br />

and 2.5-2.8°C by 2100. As to rainfall, and compared<br />

to changes recorded since 1990, it is expected to<br />

increase in the rage 2.5 - 4.8% by 2050 and 4.7 -<br />

8.8% by 2100, especially in Northern Viet Nam and<br />

less in Southern plains.<br />

The results described in the Sea Level Rise Scenarios<br />

for Viet Nam gives a predicti<strong>on</strong> for the medium<br />

emissi<strong>on</strong> scenarios similar to the data described in<br />

35

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