1932 Bulletin of the National Research Council, Issues 77-80 (theorizes about multiple nodes for each harmonic)
Animation showing amphidromic systems and nodes - page where animation is from
Uni of Alaska
At and near the system's central point the tidal range is nil
The tidal range is zero at the amphidromic point and increases with distance from this point,
Principles of Tidal Sedimentology
Image from book
Elements of Marine Ecology
Essentials of Oceanography
Virginia Institute of Marine Science
page with many sources many no longer working
from an online Oceanography quiz
The center of an open-ocean tidal system is called a(n) __________.
(a) cotidal point
(b) amphidromic point
(c) ebb current
(d) tidal bore
(b) amphidromic point
The center of an open ocean tidal system is called a(n) __________.
(a) amphidromic center.
(b) cotidal center
(c) rotary center
(d) seiche
(e) tidal flux
(a) amphidromic center.
Due to the shape of the North Sea, it develops two amphidromic points.
(a) True
(b) False
(a) True
An amphidromic point is ____________.
(a) a "no tide" point in the ocean around which the tide crest rotates through one tidal cycle
(b) a place in the ocean where tides are highest
(c) a place in the ocean where tidal datum is displaced to the right (in the northern hemisphere),
or to the south (in the southern hemisphere)
(d) a "no tide" point at the coast where there is a daily high tide, but no low tide
(a) a "no tide" point in the ocean around which the tide crest rotates through one tidal cycle
New theory about currents (pdf)
(a) amphidromic center.
(b) cotidal center
(c) rotary center
(d) seiche
(e) tidal flux
(a) amphidromic center.
Due to the shape of the North Sea, it develops two amphidromic points.
(a) True
(b) False
(a) True
An amphidromic point is ____________.
(a) a "no tide" point in the ocean around which the tide crest rotates through one tidal cycle
(b) a place in the ocean where tides are highest
(c) a place in the ocean where tidal datum is displaced to the right (in the northern hemisphere),
or to the south (in the southern hemisphere)
(d) a "no tide" point at the coast where there is a daily high tide, but no low tide
(a) a "no tide" point in the ocean around which the tide crest rotates through one tidal cycle
New theory about currents (pdf)
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