Tide (English Wikipedia)

Analysis of information sources in references of the Wikipedia article "Tide" in English language version.

Last modified:

Ref.Un. Ref.Website
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adsabs.harvard.edu (Global: 14th place; English: 9th place)

ui.adsabs.harvard.edu

ametsoc.org (Global: 4,084th place; English: 3,491st place)

glossary.ametsoc.org

arachnoid.com (Global: low place; English: low place)

  • To demonstrate this Tides Home Page offers a tidal height pattern converted into an .mp3 sound file, and the rich sound is quite different from a pure tone.

archive.org (Global: 6th place; English: 6th place)

bbc.com (Global: 26th place; English: 23rd place)

biodiversitylibrary.org (Global: 168th place; English: 136th place)

bofep.org (Global: low place; English: low place)

  • O'reilly, Charles T.; Solvason, Ron; Solomon, Christian (2005). "Resolving the World's largest tides" (PDF). In Percy, J.A; Evans, A.J.; Wells, P.G.; Rolston, S.J. (eds.). The Changing Bay of Fundy-Beyond 400 years, Proceedings of the 6th Bay of Fundy Workshop, Cornwallis, Nova Scotia, Sept. 29, 2004 to October 2, 2004. Environment Canada-Atlantic Region, Occasional Report no. 23. Dartmouth, N.S. and Sackville, N.B. Archived (PDF) from the original on August 27, 2016. Retrieved April 1, 2013.

books.google.com (Global: 3rd place; English: 3rd place)

copernicus.org (Global: 5,068th place; English: 3,578th place)

os.copernicus.org

hess.copernicus.org

darwin-online.org.uk (Global: 3,419th place; English: 2,737th place)

doi.org (Global: 2nd place; English: 2nd place)

fig.net (Global: low place; English: low place)

great-lakes.net (Global: low place; English: low place)

gutenberg.org (Global: 629th place; English: 427th place)

hdl.handle.net (Global: 66th place; English: 34th place)

jstor.org (Global: 23rd place; English: 15th place)

lewiscollard.com (Global: low place; English: low place)

wat.lewiscollard.com

linz.govt.nz (Global: 5,992nd place; English: 3,948th place)

mundogeo.com (Global: low place; English: low place)

nasa.gov (Global: 12th place; English: 73rd place)

svs.gsfc.nasa.gov

descanso.jpl.nasa.gov

science.nasa.gov

ntrs.nasa.gov

nih.gov (Global: 5th place; English: 5th place)

ncbi.nlm.nih.gov

pubmed.ncbi.nlm.nih.gov

niwa.cri.nz (Global: low place; English: low place)

  • "Tide forecasts". New Zealand: National Institute of Water & Atmospheric Research. Archived from the original on 2008-10-14. Retrieved 2008-11-07. Including animations of the M2, S2 and K1 tides for New Zealand.

noaa.gov (Global: 111th place; English: 78th place)

oceanservice.noaa.gov

tidesandcurrents.noaa.gov

nauticalcharts.noaa.gov

pol.ac.uk (Global: low place; English: low place)

sciencedirect.com (Global: 137th place; English: 146th place)

semanticscholar.org (Global: 15th place; English: 8th place)

api.semanticscholar.org

springer.com (Global: 182nd place; English: 172nd place)

link.springer.com

thespaceguy.com (Global: low place; English: low place)

unb.ca (Global: 6,706th place; English: 3,983rd place)

journals.lib.unb.ca

vliz.be (Global: low place; English: 9,356th place)

  • "Simon Stevin" (PDF) (pdf) (in Dutch). Flanders Marine Institute. Archived (PDF) from the original on 2014-08-05. Retrieved 2014-06-01.

wa.gov (Global: 1,564th place; English: 741st place)

ecy.wa.gov

washington.edu (Global: 1,171st place; English: 736th place)

faculty.washington.edu

  • Thompson, LuAnne (2006). "Physical Processes in the Ocean" (PDF). Archived (PDF) from the original on 2020-09-28. Retrieved 2020-06-27. The ocean does not produce tides as a direct response to the vertical forces at the bulges. The tidal force is only about 1 ten millionth the size of the gravitational force owing to the Earth's gravity. It is the horizontal component of the tidal force that produces the tidal bulge, causing fluid to converge at the sublunar and antipodal points and move away from the poles, causing a contraction there." (...) "The projection of the tidal force onto the horizontal direction is called the tractive force (see Knauss, Fig. 10.11). This force causes an acceleration of water towards the sublunar and antipodal points, building up water until the pressure gradient force from the bulging sea surface exactly balances the tractive force field.

waterlevels.gc.ca (Global: low place; English: low place)

web.archive.org (Global: 1st place; English: 1st place)

wiley.com (Global: 150th place; English: 174th place)

agupubs.onlinelibrary.wiley.com

onlinelibrary.wiley.com

worldcat.org (Global: 4th place; English: 4th place)

search.worldcat.org