Title: Ch 11 Tides
1- Ch 11 Tides
- Cause
- Variations with time
- Variations with location
- Dynamic vs. equilibrium model
50 ft difference between high and low tide at the
Bay of Fundy, Canada
2- Flood tide
- Ebb tide
- Slack tide
Low tide High tide
(photos from Monroe and Wicander, 2001)
3Gravitational force
Gravity of moon on water FT G m1 m2
r3 Inertia
4Tides equilibrium theory
5Affect of moons orbit elliptic Moon above
equator
equator
Moon 28 1/2o north of equator
6(No Transcript)
7December
- Affect of elliptical orbit
- Sun
- Aphelion
- Perihelion
- Moon
- Apogee
- Perigee
8Earth and Sun in line
Earth and Sun in line
days
Earth and Sun in line
Earth and Sun in line
days
Australia and New York not shown for same time
period
9Dynamic theory of tides Semidiurnal tide Diurnal
tide Mixed tide
10Geographic distribution of three tide patterns
11Amphidromic point Link http//www.es.flinders.ed
u.au/7Emattom/IntroOc/lecture11.html
12Amphidromic points of earth Blue smallest tidal
range of crest amplitude Red highest tidal
range of crest amplitude
13Gulf of St. Lawrence
Ideal amphidromic point in wide confined basin
Actual amphidromic point at Southeastern Canada
14Low tide High tide
Bay of Fundy
Ideal tide in narrow confined basin
Actual tide in confined basin in Southeastern
Canada
15Tidal Bore in Qiantang River, China
16Intertidal zone Grunion run to spawn eggs on
Pacific Coast during spring and summer