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<str<strong>on</strong>g>Desktop</str<strong>on</strong>g> <str<strong>on</strong>g>Study</str<strong>on</strong>g><br />

adaptati<strong>on</strong> (2010). The adaptati<strong>on</strong> strategies<br />

suggested for government units focuses <strong>on</strong> water<br />

related practices, whereas the <strong>on</strong>es addressed for the<br />

community and household levels seem to emphasise<br />

<strong>on</strong> capacity building in l<strong>on</strong>g term disaster resp<strong>on</strong>se<br />

and in short term coping practices, respectively.<br />

Shown in Table 9 are some examples of the strategies<br />

at all levels.<br />

SUMMARY OF IDENTIFIED<br />

KEY GAPS, CONSTRAINTS<br />

AND CHALLENGES<br />

Water Sector<br />

Regardless of climate change effects, many<br />

parts of Ind<strong>on</strong>esia experience the reducti<strong>on</strong><br />

of the quantity and quality of water resources<br />

due to growing populati<strong>on</strong>, ec<strong>on</strong>omic activities,<br />

forest clearing, land use practices and improper<br />

disposal of waste. For example, reservoirs and<br />

p<strong>on</strong>ds provide water to <strong>on</strong>ly about 10% of the<br />

total existing irrigated area, and supply clean<br />

water to 37% of the urban populati<strong>on</strong> but<br />

<strong>on</strong>ly to 8% of the rural populati<strong>on</strong> (Republic<br />

of Ind<strong>on</strong>esia, 2007). This water shortage is<br />

expected to increase due to climate change,<br />

especially the decrease in rainfall. There<br />

are several adaptati<strong>on</strong> opti<strong>on</strong>s that have<br />

been suggested to fulfil the water demand<br />

increased from these human- and climateinduced<br />

water shortage, but these opti<strong>on</strong>s<br />

are of high c<strong>on</strong>cern since they may cause the<br />

sec<strong>on</strong>d and third c<strong>on</strong>sequences. For example,<br />

the use of groundwater is suggested as <strong>on</strong>e<br />

adaptati<strong>on</strong> opti<strong>on</strong> (Republic of Ind<strong>on</strong>esia,<br />

2007). Groundwater resources, however, are<br />

particularly shallow and are vulnerable in<br />

terms of quantity and quality, especially in<br />

the dry seas<strong>on</strong>, and the excessive extracti<strong>on</strong> of<br />

groundwater, mainly because of the industrial<br />

use, may lead to land subsidence that would<br />

result in increasing the risk for flood and the<br />

intrusi<strong>on</strong> of salt water (Republic of Ind<strong>on</strong>esia,<br />

2007).<br />

In additi<strong>on</strong>, despite the existing studies that<br />

dem<strong>on</strong>strates both human- and climate-related<br />

causes of water shortage and sea level rise, the<br />

suggested adaptati<strong>on</strong> strategies revolve around<br />

the opti<strong>on</strong>s that addresses scientific knowledge<br />

<strong>on</strong> the expected impacts of climate change, but<br />

not to emphasise <strong>on</strong> changing socio-ec<strong>on</strong>omic<br />

as well as ecological envir<strong>on</strong>ments. The<br />

Ministry of Envir<strong>on</strong>ment (2007) recommends<br />

reducing scientific uncertainties surrounding<br />

the climate change effects through the collecti<strong>on</strong><br />

of l<strong>on</strong>g-term historical data <strong>on</strong> hydrological and<br />

meteorological phenomena and validating all<br />

climatic models and techniques. Meanwhile,<br />

the sea level rise in Ind<strong>on</strong>esia is expected to be<br />

greater with c<strong>on</strong>tinuous coastal erosi<strong>on</strong>, which<br />

is actually associated with socio-ec<strong>on</strong>omic<br />

development such as the interrupti<strong>on</strong> of the<br />

al<strong>on</strong>g-shore sand transport through physical<br />

structures, circulating currents generated by<br />

seawalls, the decrease of sediment from rivers<br />

caused by c<strong>on</strong>structi<strong>on</strong> of many dams in the<br />

upstream regi<strong>on</strong>s, coral or sand mining and<br />

deforestati<strong>on</strong> of mangrove forests (Ministry of<br />

Envir<strong>on</strong>ment, 2007). However, these human<br />

activities that have partially affected the sea<br />

level rise are not embodied in the governmental<br />

policies yet.<br />

Agriculture and Food Security Sector<br />

Although informati<strong>on</strong> <strong>on</strong> ENSO forecasts is<br />

generally available in Ind<strong>on</strong>esia, the access to<br />

informati<strong>on</strong> is not well established yet so that<br />

farmers cannot take precauti<strong>on</strong>s measures<br />

before the draught events (Keil et al., 2008).<br />

Also, climate models that are accurate for<br />

mountainous regi<strong>on</strong>s such as Central Sulawesi<br />

need to be developed, addressing the local<br />

c<strong>on</strong>text.<br />

Moreover, most of the farmers from this regi<strong>on</strong><br />

rely <strong>on</strong> n<strong>on</strong>-technical irrigati<strong>on</strong> systems with an<br />

irregular supply of water and the cropping and<br />

irrigati<strong>on</strong> schedule at the village level is not well<br />

coordinated (ibid). The land with n<strong>on</strong>-technical<br />

irrigati<strong>on</strong> facilities often faces the droughtinduced<br />

reducti<strong>on</strong> of rice yield. Given that the<br />

access to credit or a high level of technical<br />

efficiency in their agricultural producti<strong>on</strong><br />

results in a higher level of drought resilience,<br />

the technical and financial assistances for the<br />

farmers should be taken into c<strong>on</strong>siderati<strong>on</strong>.<br />

In additi<strong>on</strong>, there are limited adaptive capacity<br />

of the farmers in certain upland regi<strong>on</strong>s whose<br />

soil cover is eroded due to erratic rainfall or<br />

drought, as well as lack of well-coordinated<br />

system of water distributi<strong>on</strong> from upstream to<br />

downstream areas, for which renders farmers<br />

in downstream more exposed to climate change<br />

effects especially during a l<strong>on</strong>g dry seas<strong>on</strong><br />

(UNDP Ind<strong>on</strong>esia, 2007).<br />

84

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