High tide Rising tide АР Falling tide Falling tide Rising tideN Unable to continue turning to the right because of the inter- ference of the shore, the crest moves northward, following the shoreline and causing a Low High tide tide АР АР High tide Low tide high tide on the basins north- ern shore. d The wave continues its The wave trends to the right because of the Coriolis effect, causing a high tide on the basins progress around the basin in a counterclockwise direction, forming a high tide on the western shore and eastern shore. AP completing the circuit. The point Tidal crest enters basin, trends toward right side (in Northem Hemisphere) due to Coriolis effect. around which the crest moves is an amphidromic point (AP). Figure 11.14 The development of amphidromic circulation. A tide wave crest enters an ocean basin in the Northern Hemisphere. BujuJee ebe bueg

Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
Section: Chapter Questions
Problem 1LR
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Question

The island of Tahiti is very close to an amphidromic point. What does daily tidal cycle look like there?

High
tide
Rising
tide
АР
Falling
tide
Falling
tide
Rising
tideN
Unable to continue turning to
the right because of the inter-
ference of the shore, the crest
moves northward, following
the shoreline and causing a
Low
High
tide
tide
АР
АР
High
tide
Low
tide
high tide on the basins north-
ern shore.
d The wave continues its
The wave trends to the right because of the
Coriolis effect, causing a high tide on the basins
progress around the basin
in a counterclockwise
direction, forming a high tide
on the western shore and
eastern shore.
AP
completing the circuit. The point
Tidal crest enters basin,
trends toward right side
(in Northem Hemisphere)
due to Coriolis effect.
around which the crest
moves is an amphidromic
point (AP).
Figure 11.14 The development of amphidromic circulation.
A tide wave crest enters an ocean basin
in the Northern Hemisphere.
BujuJee ebe bueg
Transcribed Image Text:High tide Rising tide АР Falling tide Falling tide Rising tideN Unable to continue turning to the right because of the inter- ference of the shore, the crest moves northward, following the shoreline and causing a Low High tide tide АР АР High tide Low tide high tide on the basins north- ern shore. d The wave continues its The wave trends to the right because of the Coriolis effect, causing a high tide on the basins progress around the basin in a counterclockwise direction, forming a high tide on the western shore and eastern shore. AP completing the circuit. The point Tidal crest enters basin, trends toward right side (in Northem Hemisphere) due to Coriolis effect. around which the crest moves is an amphidromic point (AP). Figure 11.14 The development of amphidromic circulation. A tide wave crest enters an ocean basin in the Northern Hemisphere. BujuJee ebe bueg
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