Why tidal resource is concentrated
Tidal energy ultimately comes from the rotational coupling between Earth, Moon and Sun — the same astronomical forcing that produces ocean tides. Predictable is the buy-word: a half-century of tide-gauge data tells you a site’s tidal range to within centimetres. The catch is that the resource is concentrated into a small number of bay-and-channel geometries that amplify the astronomical tide.
Three Indian sites are repeatedly identified by INCOIS and feasibility studies because they share this geometry:
- Gulf of Khambhat, Gujarat — a funnel-shaped bay with spring tidal ranges commonly cited at 8–11 m and high tidal-stream velocities in the narrower reach. The most-studied Indian site.
- Gulf of Kutch, Gujarat — a smaller but tidally-significant basin north of the Kathiawar peninsula.
- Sundarbans channels, West Bengal — a network of tidal channels through mangrove islands, with strong tidal-stream flow in channels despite a more modest bay-as-amplifier geometry.
Other Indian sites show interesting signatures — Chilika lagoon, Odisha, parts of the Andaman & Nicobar channel network, parts of the Palk Bay — but at present have only preliminary resource studies.


