has shown a positive change of 53.65%, while Tapukara station has shown a
negative change of 45.38%. The rest of the stations have shown an almost constant
trend during the 57-year study period. Remarkably, SD and CV have shown a high
interannual variability over all the stations.
Fig. 12.2 Annual variation in (a) rainfall and (b) coefficient of variation over Sahibi Basin in
Rajasthan during 1961–2017
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negative change of 45.38%. The rest of the stations have shown an almost constant
trend during the 57-year study period. Remarkably, SD and CV have shown a high
interannual variability over all the stations.
Fig. 12.2 Annual variation in (a) rainfall and (b) coefficient of variation over Sahibi Basin in
Rajasthan during 1961–2017
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M. Chahal et al.