'Diurnal tides' diaporamas de présentation

Spring Tide

OCEAN SYSTEMS Geosciences 3220. Spring Tide. TIDES Chapter 11. Neap Tide. TIDES - Chapter 11 Look For the Following Key Ideas. Tides are caused by the gravitational attraction of the sun and the moon, by inertia, and by basin resonance.

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Bringing Astronomy Down to Earth

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Tides

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MOTION IN THE OCEAN

MOTION IN THE OCEAN. Waves and Tides. Waves. A disturbance which moves through or over the surface of a fluid Mostly caused by winds (Also earthquakes, volcanoes, grav. pull) Form of great energy. Wave Characteristics. Parts of a Wave Crest = high point Trough = low point

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Fig. 11-1a, p. 299

Fig. 11-1a, p. 299. Fig. 11-1b, p. 299. Chapter 11 Study Plan. Tides Are the Longest of All Ocean Waves Tides Are Forced Waves Formed by Gravity and Inertia The Dynamic Theory of Tides Adds Fluid Motion Dynamics to the Equilibrium Theory Most Tides Can Be Accurately Predicted

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N. Grieger a , U. Achatz a , H. Schmidt b and C. McLandress c

The linear interpretation of semi-annual oscillations of migrating and nonmigrating diurnal tides in the mesosphere and lower thermosphere, revealed from different general circulation models. N. Grieger a , U. Achatz a , H. Schmidt b and C. McLandress c

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Lesson 10: Tides Physical Oceanography

Lesson 10: Tides Physical Oceanography. Last lesson we learned about waves. How do you differentiate between a deepwater and shallow-water wave ? What is the period of a wave?. Figure 1: Tide predictions for Dauphin Island, 3/1/11. Water Level (ft). Time.

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Lesson 10: Tides Physical Oceanography

Lesson 10: Tides Physical Oceanography. Last lesson we learned about waves. How do you differentiate between a deepwater and shallow-water wave ? What is the period of a wave?. Figure 1: Tide predictions for Dauphin Island, 3/1/11. Water Level (ft). Time.

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Tides

Tides. By: Katie Cardwell May 2005. General Info. Tides are the periodic rise and fall of seawater These are caused by variations in gravitational attraction between the Earth, the moon and the sun. More Info. There are two tidal bulges and two low points each cycle

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Observations and model data

Interpretation of low latitudinal meteor radar observations at Learmonth, Rarotonga and Cachoeira as migrating and nonmigrating diurnal tides and their comparison with general circulation model results

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Observations and model data

Interpretation of low latitudinal meteor radar observations at Learmonth, Rarotonga and Cachoeira as migrating and nonmigrating diurnal tides and their comparison with general circulation model results

101 views • 1 slides