Knowledge (XXG)

Tide gauge

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In recent years new technologies have developed allowing for real-time, remote tide information to be published online via a solar powered wireless connection to a tide sensor. Acoustic/ultrasonic sensors have already been deployed to great effect and the data is regularly broadcast via
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Tidal poles and float gauges were the primary means of sea-level measurement for over 150 years and continue to operate at some locations today. While still part of modern-day tide gauge instrumentation, these technologies have since been superseded by pressure gauges (similar to
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Historical data are available for about 1,450 stations worldwide, of which about 950 have provided updates to the global data center since January 2010. At some places records cover centuries, for example in
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Tide gauges have a practical application in the shipping and fishing industries where low or high tide levels can hinder or prohibit access to shallow bays or locations with bridges. An example is the
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Data collected from tide gauges is also of interest to scientists measuring global weather patterns, the mean sea water level, and trends - notably those potentially associated with global warming.
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port. Because of similar problems many industries have installed private tide gauges in ports around the world, and also rely on government agencies (such as
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Sea-level measurements were made using simple measuring poles or "tide staffs" until around 1830, when self-recording gauges with mechanical
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When it comes to estimating the greater ocean picture, new modern tide gauges can often be improved upon by using satellite data.
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A tsunami can be detected when the sea level begins to rise, although warnings from
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in Portugal, which was originally installed because of the sand bar in the River
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Hydrometrie: Theorie und Praxis der Durchflussmessung in offenen Gerinnen
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With explanatory diagram showing Lea-type float gauge and stilling-well.
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Interior view of Cascais Tide Gauge showing data recording equipment
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The following types of tide gauges have been used historically:
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Device for measuring the change in sea level relative to a datum
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Ian Shennan; Antony J. Long; Benjamin P. Horton, eds. (2015).
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with respect to a height reference surface close to the
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Iliffe, J. C.; Ziebart, M. K.; Turner, J. F. (2007).
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Tide gauge history UK National Oceanographic Centre
1992:North West Shelf Operational Oceanographic System 155:), acoustic/ultrasonic gauges, and radar gauges. 1982:Deep-ocean Assessment and Reporting of Tsunamis 407:. De Gruyter Textbook. De Gruyter. p. 80. 199:that causes difficulties for shipping entering 566:"Other Long Records not in the PSMSL Data Set" 94:Sensors continuously record the height of the 1034: 760: 110:where data dating back to 1700 is available. 8: 777:meteorological equipment and instrumentation 1041: 1027: 1019: 767: 753: 745: 434:International Tsunami Information Center. 613:Geospatial Information Authority of Japan 663:"ioBridge Apps - Ockway Bay Tide Levels" 182: 54:is a device for measuring the change in 275: 1313:one-dimensional Saint-Venant equations 82:, the instrument may also be called a 7: 2260: 545:Permanent Service for Mean Sea Level 174:High resolution automatic tide gauge 147:and stilling wells were introduced. 2140:National Oceanographic Data Center 1567:World Ocean Circulation Experiment 1455:Global Ocean Data Analysis Project 171:High accuracy automatic tide gauge 25: 1987:Global Sea Level Observing System 2270: 2259: 2250: 2249: 1445:Geochemical Ocean Sections Study 1361: 1350: 436:"4. Tide, Mareograph, Sea Level" 233: 116:Tide gauges are used to measure 2175:Ocean thermal energy conversion 1898:Vine–Matthews–Morley hypothesis 638:"Remote Monitoring a MaxSonar®" 467:Handbook of Sea-Level Research 401:Torge, W.; MĂĽller, J. (2012). 1: 1435:El Niño–Southern Oscillation 1405:Craik–Leibovich vortex force 1161:Luke's variational principle 691:Gerd Morgenschweis (2010). 541:"Obtaining Tide Gauge Data" 288:Your Guide in St Petersburg 223:and also displayed online. 2314: 1500:Ocean dynamical thermostat 1348: 735:Mean Sea Level Explanation 517:"Definition of LIMNIMETER" 492:"Definition of LIMNIMETER" 2245: 2035:Ocean acoustic tomography 1848:MohoroviÄŤić discontinuity 1440:General circulation model 1076:Benjamin–Feir instability 783: 373:10.1080/01490410050128591 355:Mitchum, Gary T. (2000). 327:10.1080/01490410701568384 284:"The Kronstadt sea-gauge" 120:and quantify the size of 2165:Ocean surface topography 1540:Thermohaline circulation 1530:Subsurface ocean current 1470:Hydrothermal circulation 1303:Wave–current interaction 1081:Boussinesq approximation 605:"History of tide gauges" 62:. It is also known as a 2202:Sea surface temperature 2185:Outline of oceanography 1380:Atmospheric circulation 1318:shallow water equations 1308:Waves and shallow water 1201:Significant wave height 858:Ice accretion indicator 521:www.merriam-webster.com 264:Fort Denison#Tide gauge 2197:Sea surface microlayer 1562:Wind generated current 898:Present weather sensor 470:. Wiley. p. 557. 188: 162:Kelvin type tide gauge 47: 35: 2030:Deep scattering layer 2012:World Geodetic System 1520:Princeton Ocean Model 1400:Coriolis–Stokes force 1050:Physical oceanography 186: 165:Fuess type tide gauge 41: 33: 2050:Underwater acoustics 1610:Perigean spring tide 1475:Langmuir circulation 1186:Rossby-gravity waves 823:Dark adaptor goggles 135:can be more useful. 2212:Science On a Sphere 1818:Convergent boundary 1490:Modular Ocean Model 1450:Geostrophic current 1166:Mild-slope equation 722:Historical Examples 697:. Springer-Verlag. 179:Common applications 168:GSI type tide gauge 1868:Seafloor spreading 1858:Outer trench swell 1823:Divergent boundary 1723:Continental margin 1708:Carbonate platform 1605:Lunitidal interval 868:Lightning detector 727:2013-01-05 at the 591:2015-08-24 at the 193:Cascais tide gauge 189: 74:. When applied to 72:sea-level recorder 48: 42:The tide gauge in 36: 2285: 2284: 2277:Oceans portal 2237:World Ocean Atlas 2227:Underwater glider 2170:Ocean temperature 1833:Hydrothermal vent 1798:Submarine volcano 1733:Continental shelf 1713:Coastal geography 1703:Bathymetric chart 1585:Amphidromic point 1273:Wave nonlinearity 1131:Infragravity wave 1016: 1015: 958:Thermo-hygrograph 948:Sunshine recorder 813:Ceiling projector 704:978-3-642-05390-0 477:978-1-118-45257-8 414:978-3-11-025000-8 16:(Redirected from 2305: 2275: 2274: 2263: 2262: 2253: 2252: 2192:Pelagic sediment 2130:Marine pollution 1924:Deep ocean water 1793:Submarine canyon 1728:Continental rise 1620:Rule of twelfths 1535:Sverdrup balance 1465:Humboldt Current 1390:Boundary current 1365: 1354: 1171:Radiation stress 1141:Iribarren number 1116:Equatorial waves 1071:Ballantine scale 1066:Airy wave theory 1043: 1036: 1029: 1020: 998:Whole sky camera 943:Stevenson screen 848:Heat flux sensor 769: 762: 755: 746: 731:Brown University 711: 708: 678: 677: 675: 674: 665:. Archived from 659: 653: 652: 650: 649: 640:. Archived from 634: 628: 627: 625: 624: 615:. Archived from 609:Tide Observation 601: 595: 583: 577: 576: 574: 573: 562: 556: 555: 553: 552: 537: 531: 530: 528: 527: 513: 507: 506: 504: 503: 488: 482: 481: 461: 455: 454: 452: 451: 442:. Archived from 431: 425: 424: 422: 421: 398: 392: 391: 389: 387: 352: 346: 345: 343: 341: 306: 300: 298: 296: 294: 280: 243: 238: 237: 133:seismic activity 21: 2313: 2312: 2308: 2307: 2306: 2304: 2303: 2302: 2288: 2287: 2286: 2281: 2269: 2241: 2080: 2054: 2016: 1997:Sea-level curve 1968: 1907: 1893:Transform fault 1843:Mid-ocean ridge 1809: 1802: 1768:Oceanic plateau 1674: 1660:Tidal resonance 1630:Theory of tides 1571: 1480:Longshore drift 1430:Ekman transport 1366: 1360: 1359: 1358: 1357: 1356: 1355: 1346: 1298:Wave turbulence 1231:Trochoidal wave 1156:Longshore drift 1052: 1047: 1017: 1012: 978:Weather balloon 973:Transmissometer 938:Sounding rocket 883:Pan evaporation 808:Ceiling balloon 779: 773: 729:Wayback Machine 718: 709: 705: 690: 687: 685:Further reading 682: 681: 672: 670: 661: 660: 656: 647: 645: 636: 635: 631: 622: 620: 603: 602: 598: 593:Wayback Machine 584: 580: 571: 569: 564: 563: 559: 550: 548: 539: 538: 534: 525: 523: 515: 514: 510: 501: 499: 496:Merriam-Webster 490: 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geology 1835: 1830: 1825: 1820: 1814: 1812: 1804: 1803: 1801: 1800: 1795: 1790: 1785: 1780: 1778:Passive margin 1775: 1773:Oceanic trench 1770: 1765: 1760: 1755: 1750: 1745: 1740: 1735: 1730: 1725: 1720: 1715: 1710: 1705: 1700: 1695: 1690: 1684: 1682: 1676: 1675: 1673: 1672: 1667: 1662: 1657: 1652: 1647: 1642: 1637: 1632: 1627: 1622: 1617: 1612: 1607: 1602: 1597: 1592: 1587: 1581: 1579: 1573: 1572: 1570: 1569: 1564: 1559: 1554: 1549: 1548: 1547: 1537: 1532: 1527: 1522: 1517: 1512: 1507: 1505:Ocean dynamics 1502: 1497: 1492: 1487: 1482: 1477: 1472: 1467: 1462: 1457: 1452: 1447: 1442: 1437: 1432: 1427: 1422: 1417: 1412: 1407: 1402: 1397: 1395:Coriolis force 1392: 1387: 1382: 1376: 1374: 1368: 1367: 1349: 1347: 1345: 1344: 1343: 1342: 1332: 1327: 1322: 1321: 1320: 1315: 1305: 1300: 1295: 1290: 1285: 1280: 1275: 1270: 1265: 1260: 1255: 1250: 1245: 1244: 1243: 1233: 1228: 1223: 1218: 1216:Stokes problem 1213: 1208: 1203: 1198: 1193: 1188: 1183: 1178: 1173: 1168: 1163: 1158: 1153: 1151:Kinematic wave 1148: 1143: 1138: 1133: 1128: 1123: 1118: 1113: 1108: 1103: 1098: 1093: 1088: 1083: 1078: 1073: 1068: 1062: 1060: 1054: 1053: 1048: 1046: 1045: 1038: 1031: 1023: 1014: 1013: 1011: 1010: 1005: 1000: 995: 990: 985: 980: 975: 970: 965: 960: 955: 950: 945: 940: 935: 930: 925: 920: 915: 910: 905: 900: 895: 890: 885: 880: 875: 870: 865: 860: 855: 850: 845: 840: 835: 830: 825: 820: 815: 810: 805: 800: 795: 790: 784: 781: 780: 774: 772: 771: 764: 757: 749: 743: 742: 740:NOAA Tide Data 737: 732: 717: 716:External links 714: 713: 712: 703: 686: 683: 680: 679: 654: 629: 596: 578: 557: 532: 508: 483: 476: 456: 426: 413: 393: 367:(3): 145–166. 361:Marine Geodesy 347: 321:(4): 271–296. 315:Marine Geodesy 301: 274: 273: 271: 268: 267: 266: 261: 256: 254:Sea level rise 251: 245: 244: 228: 225: 215: 212: 180: 177: 176: 175: 172: 169: 166: 163: 140: 137: 91: 88: 60:vertical datum 58:relative to a 26: 24: 14: 13: 10: 9: 6: 4: 3: 2: 2310: 2299: 2296: 2295: 2293: 2278: 2273: 2268: 2266: 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1061: 1059: 1055: 1051: 1044: 1039: 1037: 1032: 1030: 1025: 1024: 1021: 1009: 1006: 1004: 1003:Wind profiler 1001: 999: 996: 994: 991: 989: 988:Weather radar 986: 984: 981: 979: 976: 974: 971: 969: 966: 964: 961: 959: 956: 954: 951: 949: 946: 944: 941: 939: 936: 934: 931: 929: 926: 924: 921: 919: 916: 914: 911: 909: 906: 904: 901: 899: 896: 894: 893:Pyrheliometer 891: 889: 886: 884: 881: 879: 876: 874: 871: 869: 866: 864: 861: 859: 856: 854: 851: 849: 846: 844: 841: 839: 836: 834: 831: 829: 826: 824: 821: 819: 816: 814: 811: 809: 806: 804: 801: 799: 796: 794: 791: 789: 786: 785: 782: 778: 770: 765: 763: 758: 756: 751: 750: 747: 741: 738: 736: 733: 730: 726: 723: 720: 719: 715: 706: 700: 696: 695: 689: 688: 684: 669:on 2012-01-21 668: 664: 658: 655: 644:on 2012-09-03 643: 639: 633: 630: 619:on 2013-01-05 618: 614: 610: 606: 600: 597: 594: 590: 587: 582: 579: 567: 561: 558: 546: 542: 536: 533: 522: 518: 512: 509: 497: 493: 487: 484: 479: 473: 469: 468: 460: 457: 446:on 2018-07-24 445: 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PSMSL 547:. PSMSL 404:Geodesy 386:27 July 340:27 July 221:Twitter 139:History 1954:Photic 1783:Seabed 1196:Seiche 701:  474:  440:UNESCO 411:  379:  333:  201:Lisbon 145:floats 70:, and 2145:Ocean 2114:Alvin 1964:Swash 1808:Plate 1753:Knoll 1743:Guyot 1698:Atoll 1577:Tides 1340:model 1226:Swell 1058:Waves 928:SODAR 863:Lidar 197:Tagus 118:tides 100:geoid 2112:DSV 2097:Argo 1959:Surf 1415:Eddy 699:ISBN 472:ISBN 409:ISBN 388:2024 377:ISSN 342:2024 331:ISSN 295:2019 205:NOAA 369:doi 323:doi 207:). 2294:: 611:. 607:. 543:. 519:. 494:. 438:. 375:. 365:23 363:. 359:. 329:. 319:30 317:. 313:. 286:. 86:. 66:, 50:A 1042:e 1035:t 1028:v 768:e 761:t 754:v 707:. 676:. 651:. 626:. 575:. 554:. 529:. 505:. 480:. 453:. 423:. 390:. 371:: 344:. 325:: 297:. 20:)

Index

Tide gauges


Kronstadt
sea level
vertical datum
freshwater
water bodies
water level
geoid
Amsterdam
tides
tsunamis
sea level
seismic activity
floats
depth gauges

Cascais tide gauge
Tagus
Lisbon
NOAA
Twitter
icon
Oceans portal
Level sensor
Sea level rise
Stream gauge
Fort Denison#Tide gauge
"The Kronstadt sea-gauge"

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