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MR Microinsurance_2012_03_29.indd - International Labour ...

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<strong>Microinsurance</strong> and climate change<br />

As summarized in Table 4.1, signifi cant changes such as increases in the incidence<br />

of droughts and cyclones appear imminent, which will have a huge impact<br />

on local and regional risks. Th e high levels of scientifi c validation in the table are<br />

noteworthy. Th us, “very likely” means that the level of scientifi c certainty is over<br />

90 per cent. “Likely” means greater than 66 per cent and “More likely than not”<br />

means greater than 50 per cent.<br />

Table 4.1 Projections of extreme weather and climate events<br />

Phenomenon and direction<br />

Likelihood that trend Likelihood of a human Likelihood of future<br />

of of trend trend<br />

occurred in late 20th cen- contribution<br />

trends based on projections<br />

tury (typically post 1960)<br />

for 21st century<br />

Warmer and fewer cold days and<br />

nights over most land areas<br />

Very likely Likely Virtually certain<br />

Warmer and and more frequent hot days<br />

and nights over most land areas<br />

Very likely Likely (nights) Virtually certain<br />

Warm spells/heat waves. Frequency<br />

increases over most land land areas<br />

Likely More likely than not Very likely<br />

Heavy precipitation events.<br />

Frequency (or proportion of total<br />

rainfall from heavy falls) increases<br />

over most areas areas<br />

Likely More likely than not Very likely<br />

Area aff ected ected by by drought increases Likely in many regions<br />

since 1970s<br />

More likely than not Likely<br />

Intense tropical cyclone activity<br />

Likely in many regions More likely than not Likely<br />

increases<br />

since 1970<br />

Increased incidence of extreme high<br />

sea level (excludes tsunamis)<br />

Likely More likely than not Likely<br />

Source: Adapted from IPCC, 2007.<br />

To date, meaningful evidence for countries, regions or even cities is available<br />

only in individual cases. For example:<br />

– intensifi cation of heat waves in the United States (Peterson et al., 2008), Australia<br />

(Bureau of Meteorology Australia, 2011) and Europe (Robine et al., 2007);<br />

– increase in extreme precipitation in the United States (US Climate Program,<br />

2008) and in India (Munich Re, 2010).<br />

So far, there has been limited quantitative analysis of the world’s poorer countries<br />

because time series weather data are often not available. Descriptions of the<br />

impact on climate are impressive nonetheless. Africa, for example, is a frequent<br />

victim of drought. In Ethiopia alone, around 600 000 people died in the 1970s<br />

and 1980s, and about seven million were exposed to long periods of drought.<br />

Across the continent today, drought remains a major challenge. In 2011, Chad,<br />

Malawi, Mozambique, the Sudan and the Horn of Africa struggled with extreme<br />

drought, and UN scientists expect climate change to further exacerbate such<br />

extremes.<br />

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