<P> The graph of Cook Strait's tides shows separately the high water and low water height and time, through November 2007; these are not measured values but instead are calculated from tidal parameters derived from years - old measurements . Cook Strait's nautical chart offers tidal current information . For instance the January 1979 edition for 41 ° 13 9'S 174 ° 29 6'E (north west of Cape Terawhiti) refers timings to Westport while the January 2004 issue refers to Wellington . Near Cape Terawhiti in the middle of Cook Strait the tidal height variation is almost nil while the tidal current reaches its maximum, especially near the notorious Karori Rip . Aside from weather effects, the actual currents through Cook Strait are influenced by the tidal height differences between the two ends of the strait and as can be seen, only one of the two spring tides at the north end (Nelson) has a counterpart spring tide at the south end (Wellington), so the resulting behaviour follows neither reference harbour . </P> <P> Tidal energy can be extracted by two means: inserting a water turbine into a tidal current, or building ponds that release / admit water through a turbine . In the first case, the energy amount is entirely determined by the timing and tidal current magnitude . However, the best currents may be unavailable because the turbines would obstruct ships . In the second, the impoundment dams are expensive to construct, natural water cycles are completely disrupted, ship navigation is disrupted . However, with multiple ponds, power can be generated at chosen times . So far, there are few installed systems for tidal power generation (most famously, La Rance at Saint Malo, France) which face many difficulties . Aside from environmental issues, simply withstanding corrosion and biological fouling pose engineering challenges . </P> <P> Tidal power proponents point out that, unlike wind power systems, generation levels can be reliably predicted, save for weather effects . While some generation is possible for most of the tidal cycle, in practice turbines lose efficiency at lower operating rates . Since the power available from a flow is proportional to the cube of the flow speed, the times during which high power generation is possible are brief . </P> <P> Tidal flows are important for navigation, and significant errors in position occur if they are not accommodated . Tidal heights are also important; for example many rivers and harbours have a shallow "bar" at the entrance which prevents boats with significant draft from entering at low tide . </P>

The zero point on a tide graph is called the