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Crop Insurance as a Risk Management Strategy in Bangladesh

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H<strong>as</strong>himoto et al., 1982 <strong>in</strong>troduced the above risk <strong>in</strong>dices for water resources availability<br />

study. This study adapted the methodology to apply <strong>in</strong> quantify<strong>in</strong>g risk derived from climatic<br />

changes. This part should be considered <strong>as</strong> an important value addition of the project output<br />

<strong>as</strong> because quantification of risk is a very important for a sound actuarial analysis. Especially,<br />

<strong>in</strong> the c<strong>as</strong>e of Index b<strong>as</strong>ed <strong>Crop</strong> <strong>Insurance</strong> like Weather Index <strong>Insurance</strong>, this methodology<br />

can be used effectively to quantify risk at both present and future scenarios.<br />

<strong>Risk</strong> is the term def<strong>in</strong>ed here <strong>as</strong> the probability of the system <strong>in</strong> failure state. The term<br />

Reliability, on the contrary is the ability of the system to be with<strong>in</strong> target level, i.e. it is the<br />

probability of the system be<strong>in</strong>g <strong>in</strong> a satisfactory state. The relationship between risk and<br />

reliability is thus established <strong>as</strong>:<br />

<strong>Risk</strong> = 1- Reliability<br />

i.e if Reliability, α=P{Xt ∈ S},<br />

<strong>Risk</strong> = 1- P{Xt ∈ S} = P{Xt ∈ F}<br />

Here, S and F are respectively sates of satisfactory and failure condition.<br />

Resiliency is the capability of the system to recover from a failure, i.e. return to a satisfactory<br />

state after a state of failure. It can be def<strong>in</strong>ed <strong>as</strong> the conditional probability:<br />

β = P{Xt ∈ S / Xt-1 ∈ F}<br />

Vulnerability on the other hand is def<strong>in</strong>ed <strong>as</strong> the severity of the damage that might cause<br />

while the system is <strong>in</strong> failure. It is actually related to the deficit occurs dur<strong>in</strong>g a failure <strong>as</strong>:<br />

γ = ∑sjej ; j ∈ F<br />

Where, ej is the probability of the system is <strong>in</strong> failure state,<br />

sj <strong>as</strong> the estimation of deficit.<br />

Figure 5.8 expla<strong>in</strong>s the risk <strong>in</strong>dices <strong>in</strong> a simple manner. Assume the climatic attribute <strong>as</strong><br />

Ra<strong>in</strong>fall. In that c<strong>as</strong>e, if the ra<strong>in</strong>fall is below the target level, it can be said <strong>as</strong> drought<br />

condition. Now, <strong>as</strong>sume that historically out of 100 days 30 days the precipitation w<strong>as</strong> below<br />

the target level, so the <strong>Risk</strong> of drought occurrence is 30%. In other way the Reliability of the<br />

system that there will be no drought is 70%.<br />

As it is seen from the figure 5.8, 30 days of failure occurred <strong>in</strong> 3 failure events, i.e. on an<br />

average the length of each drought period w<strong>as</strong> 10 days. Now <strong>as</strong>sume another system where<br />

for the same total days of drought condition, i.e. 30 days, there were 10 failure events, which<br />

mean on an average the length of each drought period w<strong>as</strong> 3 days. The later system can be<br />

said to be more Resilient <strong>as</strong> it can recover from a failure with<strong>in</strong> a shorter period of time. The<br />

<strong>in</strong>dex is important to quantify <strong>as</strong> because the loss amount usually multiplies quickly for<br />

prolonged climatic extreme events other than shorter ones.<br />

Other than length of failure, <strong>as</strong> shown <strong>in</strong> Figure 5.8, another <strong>in</strong>formation might be important<br />

<strong>as</strong> magnitude of failure, i.e. for a failure event, the observed value w<strong>as</strong> below the target level<br />

by what per cent or magnitude. The magnitude of failure determ<strong>in</strong>es the severity of the event,<br />

like the height of storm surge or the water level for flood<strong>in</strong>g, which actually determ<strong>in</strong>es the<br />

Vulnerability level from the dis<strong>as</strong>ter. Whether a prolonged drought or flood of moderate<br />

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