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Revitalization of Rivers in India Draft Policy - Isha Guru Jaggi Vasudev

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<strong>Revitalization</strong> <strong>of</strong> <strong>Rivers</strong> In <strong>India</strong><br />

<strong>Draft</strong> <strong>Policy</strong> Recommendation<br />

We still carry this legacy <strong>of</strong> a narrow understand<strong>in</strong>g <strong>of</strong> rivers as an<br />

exploitable resource. This idea is <strong>in</strong>stilled <strong>in</strong> eng<strong>in</strong>eers <strong>in</strong> this country.<br />

Even now rivers are considered to be a subject meant only for eng<strong>in</strong>eers.<br />

The roles <strong>of</strong> other pr<strong>of</strong>essionals like ecologists, hydrogeologists and<br />

others are deemed irrelevant. In the Western countries, though, the<br />

paradigm <strong>of</strong> river management and utilization has shifted to Integrated<br />

Water Resource Management (IWRM). The new IWRM paradigm takes <strong>in</strong>to<br />

consideration demand management and provides for ecological needs<br />

<strong>of</strong> water too. The ancient <strong>India</strong>n ethos to revere our rivers and worship<br />

them as goddesses took these two considerations <strong>in</strong>to account as well as<br />

the needs <strong>of</strong> all other liv<strong>in</strong>g be<strong>in</strong>gs dependent on the river. However, the<br />

current reductionist approach adopted towards rivers <strong>in</strong> <strong>India</strong> has given<br />

rise to an unsusta<strong>in</strong>able number <strong>of</strong> dams, irrigation canals and hydropower<br />

projects.<br />

SECOND KNOT - DEFORESTATION IN RIVER CATCHMENT AREAS<br />

The shr<strong>in</strong>k<strong>in</strong>g <strong>of</strong> glaciers is largely perceived as the cause for<br />

the reduction <strong>of</strong> water <strong>in</strong> the rivers, especially the Himalayan rivers.<br />

Glaciers are important to rivers, no doubt, but the extent <strong>of</strong> glaciation<br />

that contributes to the river is only 10% on an average. To elaborate on<br />

this further, the case <strong>of</strong> Ganga is represented <strong>in</strong> Table 1, which <strong>in</strong>dicates<br />

the catchment area from glaciers <strong>in</strong> comparison to the catchment area<br />

covered by mounta<strong>in</strong>s. Similar is the case for other Himalayan rivers too.<br />

It may, therefore, be concluded that majority <strong>of</strong> water <strong>in</strong> the rivers<br />

come from the run<strong>of</strong>f from the catchment area rather than glaciers. If<br />

the contribution <strong>of</strong> run<strong>of</strong>f from catchment areas is so high <strong>in</strong> the case <strong>of</strong><br />

Himalayan rivers fed by glaciers, then, the central <strong>India</strong>n and pen<strong>in</strong>sular<br />

rivers must have an even higher dependency on this run<strong>of</strong>f. 41<br />

55

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