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Ocean power in New Zealand

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122: 509: 1831: 483: 783: 1949: 1938: 1926: 811: 797: 30: 1914: 652:. It narrows to a width of 6 kilometres (3.7 mi), and is over 50 metres (160 ft) deep in parts. On average, Kaipara tides rise and fall 2.10 metres (6.9 ft). At high tide, nearly 1000 square kilometres are flooded. Spring tidal flows reach 9 km/h (5 knots) in the entrance channel and move 1,990 million cubic metres per tidal movement or 7,960 million cubic meters daily. 561:
high tide occurs five hours before it occurs at the Tasman Sea side. On one side is high tide and on the other is low tide. The difference in sea level can drive tidal currents up to 2.5 metres per second (5 knots) across Cook Strait as well as into the Tory Channel. An unusual complication is that although there are two spring tides a month on the south side, the north side has only
765:, a Crown Research Institute, and Power Projects Limited, a privately owned Wellington-based company. The programme seeks to develop a wave energy device that generates electricity from both the kinetic and potential energy available in open ocean waves. In 2010 WET-NZ received resource consent for half-scale prototype testing at two test sites. The device is now called 742: 633: 621: 542: 526: 405: 492:
Since the construction of the Manapouri power station, there has been about five MW of tide-determined generation. The tailrace tunnel exit by Dusky Sound debouches at sea level, and thus the effective head of the power station is affected by the level of the tide there. If the turbines are operated
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rather than circular. The effect of this is that the time between high tides changes a little from day to day. The Moon takes about 24.8 hours to orbit around the Earth, so it takes half this time, 12.4 hours, for the M2 tides to occur. The tides can be predicted far in advance, because the Moon and
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that also travels around the Earth. There are actually two high tides, because the Earth and Moon, as a system, both rotate about a common centre of mass. This centre is two-thirds out from the centre of the Earth, not at the centre of the Earth. The effect of the Earth spinning about this centre is
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On average, ocean waves in New Zealand deliver about 25 kW to each metre of coastline. The west and south-west coasts have the country's most energetic waves. Even on windless days, swells that were generated in the Southern Ocean still arrive. Less wave energy arrives at the north-east coast,
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spring tide a month, as shown in the plot. A further consequence of these opposed tides is that there is almost zero tidal height change at the centre of the strait. Although the tidal surge should flow in one direction for six hours and then the reverse direction for six hours, a particular surge
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The actual tide pattern and timing is determined by the nature of the resonances in each ocean basin with the various frequencies of the gravitational influences, over many cycles. New Zealand's situation (like Iceland's) is a small island in a large basin, and the peaks and troughs of the M2 tides
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has tidal flows amongst the strongest in the world, even though it has a smaller tidal range than most places in New Zealand. This is because the main M2 lunar tide component which circulates anti-clockwise around New Zealand is out of phase at each end of the strait. On the Pacific Ocean side the
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Crest plans to place the turbines at least 30 metres deep along a ten kilometre stretch of the main channel. Historical charts show this stretch of the channel has changed little over 150 years. The output of the turbines will cycle twice daily with the predictable rise and fall of the tide. Each
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substation. The turbine is a pilot, and will be sited in slower tides for testing. Neptune hopes to generate power from the unit by 2010. The company has claimed there is enough tidal movement in Cook Strait to generate 12 GW of power, more than one-and-a-half times New Zealand's current
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might last eight or ten hours with the reverse surge enfeebled. In especially boisterous weather conditions the reverse surge can be negated, and the flow can remain in the same direction through three surge periods and longer. This is indicated on marine charts for the region.
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sweep continuously anticlockwise around New Zealand. When it is high tide on the west coast, it is low tide on the east coast, and vice versa: the straightforward notion of tidal bulges aligned with the Moon is insufficient. These currents are most noticeable in
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A third influence occurs because the Moon orbits at an angle to the equator. This means that if one of the bulges travelling around the Earth is above the equator, then the other bulge is below the equator. It also follows that some places will have one daily
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into electricity using devices either fixed to the shore, the seabed or floating out at sea. Wave energy varies with time, depending on when and where the winds and storms that drive the waves occur. Tidal energy is more regular and predictable.
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However, while the Department of Conservation has approved the project, and has made substantial environmental monitoring conditions part of the consent, the project also has objectors on the grounds of claimed influences on the local
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By world standards, New Zealand's tides are, for the most part, moderate. The tide usually ranges between one and two metres. Tidal currents are usually around two kilometres per hour (one knot). Some exception are in and around
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On the other side of the strait, Energy Pacifica has talked for some time about applying for resource consent to install up to ten marine turbines, each able to produce up to 1.2 MW, near the Cook Strait entrance to
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A second influence on the tides occurs because of gravitation from the Sun. Gravitation from the Sun has less influence than the Moon, because it is so much further from Earth. However, the Sun influences the
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near Antarctica every 24.84 hours. The height of this tide dwindles to almost zero in a cycle which takes 13.66 days. New Zealand's tides are semi-diurnal. The primary cause, the lunar tide, is labelled the
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was established in 2006 to "promote the uptake of marine energy in New Zealand". According to their 10 February 2008 newsletter, they have 59 members. However, the association doesn't list its members.
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The power generated by tidal marine turbines varies as the cube of the tidal speed. Because the tidal speed doubles, eight times more tidal power can be produced at spring tides than at neap tides.
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at a fixed flow aperture, the power produced is not constant but follows the tide, an effect that can be seen in the following graph. Note that the timing follows the tides around the clock,
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There are numerous computer model representations of the tidal flow through Cook Strait. While the tidal components are readily realizable, the residual flow is more difficult to model.
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Bowman, M.J., A.C. Kibblewhite, R. Murtagh, S.M. Chiswell and B.G. Sanderson (1983) Circulation and mixing in greater Cook Strait, New Zealand. Oceanologica Acta 6(4): 383-391
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New Zealand has a relatively small tidal range, usually less than two metres. However, some of the larger harbours on the west coast of the North Island, in particular the
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The Opunake power station has its tailrace exiting to the beach but its operation is intermittent so if there is any tidal effect on generation there, it is unclear.
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seem to offer the most promising sites for using underwater turbines. Two resource consents have been granted for pilot projects in Cook Strait itself and in the
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in the strait. The turbine has been designed in Britain and will be built in New Zealand at a cost $ 10 million. Fourteen metres in diameter and constructed of
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2008: Energy Pacifica applies for resource consent to install up to 10 marine turbines, each able to produce up to 1.2 MW, near the Cook Strait entrance to
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This computer animation shows the peaks and troughs of the M2 tides sweeping anticlockwise around New Zealand. When it is high tide on one side of
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Tidal patterns in Cook Strait. The south part (Nelson) has two spring tides per month, versus only one on the north side (Wellington and Napier).
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with tidal flows up to 100,000 cubic metres a second. These tidal volumes are 12 times greater than the flows in the largest New Zealand rivers.
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Tidal power is generated by capturing some of the energy in the tides as they cycle forth and back, twice each day. Tidal devices can be
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on the tides, though only some will be significant at a given location. The gravitation of the Moon and Sun are the most important.
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is allocating $ 2 million each year from a Marine Energy Deployment Fund, set up to encourage the utilisation of this resource.
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Wave Energy Technology - New Zealand (WET-NZ) is a Government-funded research and development collaboration programme between
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The peak level of generation for the combined turbines is about 200 MW. This exceeds the projected peak electricity needs of
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projects are currently under development. However, not a lot of public information is available about these projects. The
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dominate in the north, enlivened by an occasional cyclone from the tropics. The rest of the country is dominated by the
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of the Moon. About once a day the Moon rotates around the Earth, attracting as it travels the bulge of water called the
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A fourth influence occurs because the orbit of the Moon around the Earth and the orbit of the Earth around the Sun are
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is proportional to the square of its height, so a two-metre wave contains four times the energy of a one-metre wave.
383:. When the Sun is at right angles to the Moon, the effects are partially cancelled, producing the small tides called 474:, just off the greater Cook Strait, where, despite the low tidal range, tidal streams can reach nearly eight knots. 1763: 1391: 1200: 348:. Headlands and constrictions like these focus the currents, giving energy levels reaching 750 W per square metre. 572:
In April 2008, a resource consent was granted to Neptune Power for the installation of an experimental underwater
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that it behaves as a centrifuge, resulting in a second high tide bulge in the ocean most distant from the Moon.
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tide, while other places will have semi-diurnal tides twice a day. For example, there is a diurnal tide in the
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because it is sheltered from the south-west waves (click the link on the right for a diagram). The amount of
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it is low tide on the other side. For this reason, Cook Strait can experience exceptionally fast tidal flows.
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moving in and out every day near the harbour mouth to produce electricity for approximately 250,000 homes.
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turbine will have a maximum output of 1.2 MW, and is expected to generate 0.75 MW averaged over time.
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2008: SeaGen, the world's first commercial scale tidal stream energy generator, goes on stream in
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2008: Neptune Power given resource consent to build a pilot turbine off Sinclair Head in
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Pathway to energy generation from marine tidal currents in New Zealand's Kaipara Harbour
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2003: Seaflow, the world's first underwater turbine prototype, goes on stream off north
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and access to the electricity network. No application had been lodged by March 2011.
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Squeezing information from an elusive ocean: surface currents from satellite imagery
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were concluded in 2010, with a favourable decision released in February 2011.
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Prepared for the Energy Efficiency and Conservation Authority, 18 May 2005
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Marine Energy: Summary of Current Developments and Outlook for New Zealand
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requirements. In practice, only some of this energy could be harnessed.
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Bowen M, Richardson K, Pinkerton M, Korpela A and Uddstrom M (2004)
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project goes online at La Rance, France, with a capacity of 240 MW.
1513:"Making waves: UK firm harnesses power of the sea ... in Portugal" 1449:"Marine Current Turbines: progress with tidal turbine development" 1426:
Te Ara: The Encyclopedia of New Zealand, updated 21 September 2007
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Te Ara: The Encyclopedia of New Zealand, updated 21 September 2007
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such as Cook Strait and in Foveaux Strait. A notable example is
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Prepared for the Energy Efficiency and Conservation Authority.
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Cook Strait currents before and after high tide at Wellington
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Global surface elevation of the M2 ocean tide (NASA) 
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Stevens, Craig; Smith, Murray and Gorman, Richard (2005)
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resources but does not yet generate any power from them.
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Electricity Generation from Tidal Power In New Zealand
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National Institute of Water and Atmospheric Research
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Energy NZ No.6, Spring 2008. Contrafed Publishing.
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The 69:Energy Efficiency and Conservation Authority 1684:NZ: Chance to turn the tide of power supply 848:devices and has a peak capacity of 2.25 MW. 1771: 1757: 1749: 1631:Rickard, Graham and Hadfield, Mark (2004) 1322:Bellve, AR; Austin, G and Woods, B (2007) 1295:Haggit T, Mead S, and Bellingham M (2008) 1034:Aotearoa Wave and Tidal Energy Association 311: 297: 269:Nuclear power proposed as renewable energy 104: 61:Aotearoa Wave and Tidal Energy Association 36:has the fastest tidal flows in New Zealand 1144: 1142: 1140: 1138: 1136: 1088:Ocean bounty: energy from waves and tides 1081: 1079: 690:and charter fishing. Appeals before the 98:. The harbours produce currents up to 6 28: 1179:Lunar tides in Cook Strait, New Zealand 967: 534:Te Ara: The Encyclopedia of New Zealand 112: 1863:Development of tidal stream generators 1739:(Wave Energy Technology - New Zealand) 1551:"DOC considering Kaipara turbine plan" 1420:Stevens, Craig and Chiswell, Stephen. 1390:Doesburg, Anthony (1 September 2008). 1067:Stevens, Craig and Chiswell, Stephen. 976:"Tidal power rides wave of popularity" 746:Average wave height around New Zealand 731: 610: 515: 1091:Water & Atmosphere, Vol.13, No.4. 7: 1672:Tidal power rides wave of popularity 1646:Water & Atmosphere, Vol.12, No.4 1372:Energy NZ, Vol 1, No 1, Winter 2007. 546:Underwater topography of Cook Strait 1249:Energy NZ, Vol 1, No 1, Winter 2007 1199:Doesburg, Anthony (15 April 2008). 844:goes on line in Portugal. It uses 840:2008: The world's first commercial 705:involves converting the energy in 667:, which would use the substantial 67:From 2008 to 2011, the government 25: 1617:Marine energy in NZ report - 2008 1308:ARC Technical Publication TP 354. 1948: 1947: 1936: 1924: 1912: 1829: 1284:Photo gallery of Kaipere Harbour 870:, with a peak capacity of 200MW. 809: 795: 781: 740: 659:to install about 200 underwater 631: 619: 540: 524: 421: 120: 1984:Renewable energy in New Zealand 1889:Ocean thermal energy conversion 1423:Ocean currents and tides: Waves 1370:Harnessing the power of the sea 1247:Harnessing the power of the sea 1101:Ocean Tides and Magnetic Fields 1070:Ocean currents and tides: Tides 956:Renewable energy in New Zealand 921:Renewable energy in New Zealand 911:Ocean thermal energy conversion 837:with a peak capacity of 300 KW. 769:and is being tested in Hawaii. 397:Altogether there are sixty-two 280:Topics by country and territory 1721:Video: Chasing currents (NIWA) 1511:Alok Jha (25 September 2008). 1226:Renewable energy development: 51:reported in 2007 that over 20 1: 1666:Tidal Power | Kaipara Harbour 1539:Tidal power in the UK: SeaGen 1116:Tide Forecaster (New Zealand) 916:Pelamis Wave Energy Converter 399:recognised natural influences 354:are controlled mainly by the 1848:List of tidal power stations 1715:A Beautiful Source of Energy 1583:"Tidal power trial approved" 1004:"AWATEA February newsletter" 625:Kaipara Harbour main channel 446:stands for the Moon and the 1931:Renewable energy portal 1879:List of offshore wind farms 1801:List of wave power projects 1796:List of wave power stations 1634:Forecasting ocean "weather" 763:Industrial Research Limited 665:Kaipara Tidal Power Station 637:Proposed cable and turbines 285:Marketing and policy trends 2000: 487:Generation and tide height 1907: 1827: 1228:Tidal Energy: Cook Strait 1104:NASA Visualization Studio 951:Wind power in New Zealand 901:Intermittent power source 739: 630: 618: 539: 523: 18:Wave power in New Zealand 1733:– J Floor Anthoni, 2000. 1709:Ocean Energy Review 2008 1626:Marine energy fact sheet 1489:. London. Archived from 450:stands for twice a day. 332:or dam like structures ( 1333:University of Auckland. 926:Salinity gradient power 817:Renewable energy portal 1974:Tidal power by country 1858:Tidal stream generator 1743:Power Projects Limited 1652:Harnessing the Oceans? 1649:Stevens, Craig (2007) 1588:Television New Zealand 1556:Television New Zealand 1397:The New Zealand Herald 1206:The New Zealand Herald 513: 489: 425: 246:Tidal stream generator 37: 1979:Wave power by country 1894:Offshore construction 1693:Anthony Bellve, 2005. 1438:October 2010 Bulletin 866:near the entrance of 511: 485: 416: 32: 1884:Marine current power 1168:Chart of Cook Strait 906:Marine current power 574:tidal stream turbine 206:Marine current power 152:Crosswind kite power 1731:Oceanography: waves 1106:, 30 December 2016. 828:first tidal barrage 707:ocean surface waves 236:Sustainable biofuel 147:Carbon-neutral fuel 108:Part of a series on 1689:2012-03-10 at the 1658:2008-10-18 at the 1377:2011-07-24 at the 1329:2008-10-14 at the 1304:2012-02-18 at the 1254:2011-07-24 at the 1233:2009-02-14 at the 1154:2010-08-01 at the 826:1966: The world's 789:New Zealand portal 514: 490: 426: 356:gravitational pull 162:Geothermal heating 38: 1961: 1960: 1943:Oceans portal 1919:Energy portal 1619:Prepared for the 984:. 2 December 2007 751: 750: 692:Environment Court 642: 641: 555: 554: 414: 321: 320: 157:Geothermal energy 92:Hokianga Harbours 16:(Redirected from 1991: 1951: 1950: 1941: 1940: 1929: 1928: 1917: 1916: 1833: 1773: 1766: 1759: 1750: 1605: 1604: 1602: 1600: 1579: 1573: 1572: 1570: 1568: 1547: 1541: 1536: 1530: 1529: 1527: 1526: 1508: 1502: 1501: 1499: 1498: 1476: 1470: 1469: 1467: 1466: 1460: 1454:. 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1535: 1532: 1520: 1519: 1514: 1507: 1504: 1493:on 2012-12-23 1492: 1488: 1487: 1482: 1475: 1472: 1461:on 2012-02-20 1457: 1450: 1444: 1441: 1437: 1432: 1429: 1425: 1424: 1417: 1415: 1411: 1399: 1398: 1393: 1386: 1383: 1380: 1376: 1373: 1371: 1365: 1362: 1358: 1353: 1350: 1345: 1339: 1336: 1332: 1328: 1325: 1319: 1317: 1315: 1311: 1307: 1303: 1300: 1299: 1292: 1289: 1285: 1280: 1278: 1274: 1269: 1263: 1260: 1257: 1253: 1250: 1248: 1242: 1239: 1236: 1232: 1229: 1223: 1220: 1208: 1207: 1202: 1195: 1192: 1186: 1183: 1180: 1175: 1172: 1169: 1164: 1161: 1157: 1153: 1150: 1145: 1143: 1141: 1139: 1137: 1133: 1129: 1124: 1121: 1117: 1112: 1109: 1105: 1102: 1097: 1094: 1090: 1089: 1082: 1080: 1076: 1072: 1071: 1064: 1062: 1060: 1058: 1056: 1054: 1050: 1046: 1041: 1038: 1035: 1030: 1027: 1016:on 2008-10-14 1012: 1005: 999: 996: 983: 982: 977: 971: 968: 962: 957: 954: 952: 949: 947: 944: 942: 939: 937: 934: 932: 929: 927: 924: 922: 919: 917: 914: 912: 909: 907: 904: 902: 899: 897: 894: 893: 888: 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163: 160: 158: 155: 153: 150: 148: 145: 143: 140: 138: 135: 133: 130: 129: 128: 127: 123: 119: 118: 115: 111: 107: 106: 103: 101: 97: 93: 89: 85: 81: 77: 72: 70: 65: 62: 58: 54: 50: 46: 42: 35: 31: 27: 19: 1810: 1745:Publications 1714: 1671: 1651: 1642: 1633: 1597:. Retrieved 1595:. 2 May 2008 1586: 1577: 1565:. Retrieved 1554: 1545: 1534: 1523:. Retrieved 1518:The Guardian 1516: 1506: 1495:. Retrieved 1491:the original 1484: 1479:Emily Ford. 1474: 1463:. Retrieved 1456:the original 1443: 1431: 1422: 1401:. Retrieved 1395: 1385: 1369: 1364: 1359:Crest Energy 1352: 1338: 1297: 1291: 1262: 1246: 1241: 1222: 1210:. Retrieved 1204: 1194: 1185: 1174: 1163: 1149:Benign tides 1123: 1111: 1103: 1096: 1086: 1069: 1040: 1029: 1018:. Retrieved 1011:the original 998: 986:. Retrieved 979: 970: 882:Tory Channel 862:to sink 200 760: 752: 712: 701: 684: 677: 673: 654: 643: 602: 594:Tory Channel 590: 578:carbon fibre 571: 568: 562: 556: 499: 494: 491: 464: 452: 447: 443: 439: 427: 396: 389: 381:spring tides 365: 350: 338: 327: 226:Solar energy 84:Tory Channel 74:The greater 73: 66: 45:ocean energy 39: 26: 1840:Tidal power 1811:New Zealand 1593:Newstalk ZB 1561:Newstalk ZB 931:Tidal power 875:Cook Strait 715:trade winds 669:tidal flows 558:Cook Strait 504:Cook Strait 472:French Pass 422:Cook Strait 369:tidal range 342:Cook Strait 324:Tidal power 241:Tidal power 231:Solar power 199:Small hydro 189:Micro hydro 96:French Pass 76:Cook Strait 57:tidal power 41:New Zealand 34:French Pass 1968:Categories 1788:Wave power 1599:1 November 1567:1 November 1525:2008-10-09 1497:2008-10-15 1465:2009-03-06 1403:1 November 1212:1 November 1020:2009-03-02 988:1 November 963:References 941:Wave power 723:Tasman Sea 703:Wave power 698:Wave power 688:ecosystems 650:Tasman Sea 598:bathymetry 585:Island Bay 455:elliptical 385:neap tides 258:Wind power 253:Wave power 194:Pico hydro 184:Hydropower 43:has large 1806:Australia 1486:The Times 946:Wind wave 936:Wave farm 842:wave farm 680:Northland 478:Manapouri 377:full moon 360:high tide 1953:Category 1821:Scotland 1687:Archived 1656:Archived 1521:. London 1375:Archived 1327:Archived 1302:Archived 1252:Archived 1231:Archived 1152:Archived 981:One News 889:See also 773:Timeline 725:and the 663:for the 582:Vector's 435:Ross Sea 334:barrages 846:Pelamis 468:straits 431:diurnal 392:Kaipara 142:Biomass 132:Biofuel 94:, and 88:Manukau 1737:WET-NZ 1680:– BWEA 1118:– NIWA 442:. The 137:Biogas 1872:Other 1459:(PDF) 1452:(PDF) 1268:"RNZ" 1014:(PDF) 1007:(PDF) 835:Devon 767:Azura 352:Tides 100:knots 1601:2011 1569:2011 1405:2011 1214:2011 990:2011 550:NIWA 375:and 330:weir 90:and 78:and 55:and 53:wave 49:TVNZ 1357:FAQ 563:one 495:not 373:new 1970:: 1591:. 1585:. 1559:. 1553:. 1515:. 1483:. 1413:^ 1394:. 1313:^ 1276:^ 1203:. 1135:^ 1078:^ 1052:^ 978:. 548:– 532:– 440:M2 387:. 1772:e 1765:t 1758:v 1603:. 1571:. 1528:. 1500:. 1468:. 1407:. 1346:. 1270:. 1216:. 1023:. 992:. 884:. 877:. 448:2 444:M 312:e 305:t 298:v 20:)

Index

Wave power in New Zealand

French Pass
New Zealand
ocean energy
TVNZ
wave
tidal power
Aotearoa Wave and Tidal Energy Association
Energy Efficiency and Conservation Authority
Cook Strait
Kaipara Harbour
Tory Channel
Manukau
Hokianga Harbours
French Pass
knots
Renewable energy

Biofuel
Biogas
Biomass
Carbon-neutral fuel
Crosswind kite power
Geothermal energy
Geothermal heating
Geothermal power
Hydroelectricity
Run-of-the-river
Hydropower

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