geog 3a ~ final review chapter 10 ~ ocean waves chapter 11 ~ tides

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Geog 3A ~ Final Review Chapter 10 ~ Ocean Waves Chapter 11 ~ Tides

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Page 1: Geog 3A ~ Final Review Chapter 10 ~ Ocean Waves Chapter 11 ~ Tides

Geog 3A ~ Final Review

Chapter 10 ~ Ocean Waves

Chapter 11 ~ Tides

Page 2: Geog 3A ~ Final Review Chapter 10 ~ Ocean Waves Chapter 11 ~ Tides

The Plan

Collective Practice Exam

(Ask questions at any time)

TA Evaluations

Return Graded Assignments (after class)

Page 3: Geog 3A ~ Final Review Chapter 10 ~ Ocean Waves Chapter 11 ~ Tides

1. Waves that occur along the interface of two water masses with different densities are 

Practice Exam-Ch 10

A. internal waves.

B. chop.

C. swell.

D. tsunami.

E. tides.

Page 4: Geog 3A ~ Final Review Chapter 10 ~ Ocean Waves Chapter 11 ~ Tides

2. The restoring force for capillary waves is

A. gravity.

B. wind.

C. hydrostatic pressure

D. surface tension.

E. None of the choices are correct.

Page 5: Geog 3A ~ Final Review Chapter 10 ~ Ocean Waves Chapter 11 ~ Tides

3. The restoring force for wind waves is

A. gravity.

B. wind.

C. hydrostatic pressure.

D. surface tension.

E. None of the choices are

correct.

Page 6: Geog 3A ~ Final Review Chapter 10 ~ Ocean Waves Chapter 11 ~ Tides

4. Waves traveling in water depths deeper than 1/2 the wavelength of the wave are called

A. shallow-water waves.

B. deep-water waves.

C. intermediate waves.

D. tsunami.

E. internal waves.

Page 7: Geog 3A ~ Final Review Chapter 10 ~ Ocean Waves Chapter 11 ~ Tides

5. Waves traveling in water depths less than 1/20th of their wavelength are called

A. shallow-water waves.

B. deep-water waves.

C. intermediate waves.

D. tsunami.

E. internal waves.

Page 8: Geog 3A ~ Final Review Chapter 10 ~ Ocean Waves Chapter 11 ~ Tides

6. Once a gravity wave forms, its _______ does not change.

A. wavelength

B. height

C. steepness

D. speed

E. period

Page 9: Geog 3A ~ Final Review Chapter 10 ~ Ocean Waves Chapter 11 ~ Tides

7. A wave with a wavelength of 50 feet is traveling in water with a depth of 2 feet. Which equation correctly expresses its speed?

A.  C = 1.56 T

B.  C = 1.56 L

C.  C = gh

D.  C = square root of gh

E.  C = h/L

Page 10: Geog 3A ~ Final Review Chapter 10 ~ Ocean Waves Chapter 11 ~ Tides

8. A wave with a wavelength of 200 feet is traveling in water with a depth of 2000 feet. Which equation correctly expresses its speed?

A.  C = 1.56 T

B.  C = 1.56 L

C.  C = gh

D.  C = square root of

gh

E.  C = h/L

Page 11: Geog 3A ~ Final Review Chapter 10 ~ Ocean Waves Chapter 11 ~ Tides

9. The separation of waves according to their wave speed is called

A. diffusion.

B. dispersion.

C. separation.

D. refraction.

E. reflection.

Page 12: Geog 3A ~ Final Review Chapter 10 ~ Ocean Waves Chapter 11 ~ Tides

10. The speed of an individual wave is ______ the group speed. 

A. half

B. the same as

C. twice

D. three times

E. ten times

Page 13: Geog 3A ~ Final Review Chapter 10 ~ Ocean Waves Chapter 11 ~ Tides

11. The speed of shallow-water waves depends solely on

A. water density.

B. wave period.

C. wave height.

D. wave steepness.

E. water depth.

Page 14: Geog 3A ~ Final Review Chapter 10 ~ Ocean Waves Chapter 11 ~ Tides

12. The distance over which the wind blows is called

A. wind steepness.

B. wind fetch.

C. wind duration.

D. wind scale.

E. wind speed.

Page 15: Geog 3A ~ Final Review Chapter 10 ~ Ocean Waves Chapter 11 ~ Tides

13. Which of the following is generally not a factor in wave generation in the open ocean?

A. wind speed

B. wind fetch

C. wind duration

D. wind direction

Page 16: Geog 3A ~ Final Review Chapter 10 ~ Ocean Waves Chapter 11 ~ Tides

14. In general, the largest and most powerful waves for surfing are produced by

A. large storm systems.

B. tsunami.

C. hurricanes.

D. tornadoes.

E. tides.

Page 17: Geog 3A ~ Final Review Chapter 10 ~ Ocean Waves Chapter 11 ~ Tides

15. The steepness of a wave is defined as

A. wave height divided by wave

period.

B. wave height divided by wavelength.

C. wavelength divided by wave height.

D. wavelength divided by wave period.

E. wave height multiplied by

wavelength.

Page 18: Geog 3A ~ Final Review Chapter 10 ~ Ocean Waves Chapter 11 ~ Tides

16. You see a wave with a height of 2 meters and a wavelength of 18 meters. Based on the steepness

A. you don’t have enough information

to know if the wave will break.

B. S < 1/7 so the wave will break

C. S > 1/7 so the wave will not break.

D. S < 1/7 so the wave will not break

E. S > 1/7 so the wave will break

Page 19: Geog 3A ~ Final Review Chapter 10 ~ Ocean Waves Chapter 11 ~ Tides

17. The "tube" of spectacularly large waves results from

A. water particles in the crest moving faster than the speed of the wave.B. the base of the wave moving faster than the crest.C. the reversal of wave orbitals.D. a bump in the seafloor, like a sand bar.E. scientists are not sure why tubes form.

Page 20: Geog 3A ~ Final Review Chapter 10 ~ Ocean Waves Chapter 11 ~ Tides

18. The bending of a wave front as it approaches the shoreline is called

A. wave reflection.

B. wave focusing.

C. wave refraction.

D. wave diffraction.

E. wave interference.

Page 21: Geog 3A ~ Final Review Chapter 10 ~ Ocean Waves Chapter 11 ~ Tides

19. Wave refraction on a straight shoreline facing west will not occur if

A. the waves come from the northwest.

B. the waves come from the southwest.

C. the waves come directly from the

west.

D. none of the above

Page 22: Geog 3A ~ Final Review Chapter 10 ~ Ocean Waves Chapter 11 ~ Tides

20. Refraction of a wave in a bay

A. distributes the wave energy over a greater length of a wave front.B. creates smaller waves in the bay.C. creates larger waves in the bay.D. concentrates wave energy into a small portion of the bay.E. Both distributes the wave energy over a greater length of a wave front and creates smaller waves in the bay.

Page 23: Geog 3A ~ Final Review Chapter 10 ~ Ocean Waves Chapter 11 ~ Tides

21. The transfer of wave energy laterally along the crest of a wave is called

A. wave reflection.

B. wave refraction.

C. wave focusing.

D. wave diffraction.

E. wave displacement.

Page 24: Geog 3A ~ Final Review Chapter 10 ~ Ocean Waves Chapter 11 ~ Tides

22. The speed of a tsunami is largely controlled by

A. the vertical displacement that caused

it.

B. the density of seawater in which it

occurs.

C. the water depth.

D. the area over which it occurs.

E. All of the choices are correct.

Page 25: Geog 3A ~ Final Review Chapter 10 ~ Ocean Waves Chapter 11 ~ Tides

23. The horizontal distance from the shoreline to the landwardmost reach of a tsunami is called

A. inundation.

B. runup.

C. scattering.

D. tsunami break.

E. tsunami splash.

Page 26: Geog 3A ~ Final Review Chapter 10 ~ Ocean Waves Chapter 11 ~ Tides

24. The vertical height above sea level to which a tsunami reaches is called

A. inundation.

B. runup.

C. scattering.

D. tsunami break.

E. tsunami splash.

Page 27: Geog 3A ~ Final Review Chapter 10 ~ Ocean Waves Chapter 11 ~ Tides

25. A standing wave that may occur in a semi-enclosed basin or waterway is called

A. a splash wave.

B. storm surge.

C. a bore.

D. a seiche.

E. All of the choices are correct.

Page 28: Geog 3A ~ Final Review Chapter 10 ~ Ocean Waves Chapter 11 ~ Tides

1. Tides are caused by

a: centrifugal forceb: gravitational attraction between planetary bodiesc: the Earth’s rotationd: the Coriolis effecte: Newton’s law

Practice Exam-Ch 11

Page 29: Geog 3A ~ Final Review Chapter 10 ~ Ocean Waves Chapter 11 ~ Tides

2: Which of the following is not a characteristic of the tide-producing forces?

a: tidal forces result from differences in gravitational attraction at different points on Earth’s surfaceb: the horizontal tidal forces cause movements of waterc: the Moon’s gravity pulls water upwards towards it as a vertical forced: points directly beneath and opposite the Earth-moon axis have zero tidal forcese: tidal forces are very weak over short distances

Page 30: Geog 3A ~ Final Review Chapter 10 ~ Ocean Waves Chapter 11 ~ Tides

3: The monthly tidal pattern where the tidal range is minimal is known as

a: neap tidesb: full tidesc: spring tidesd: low tidese: high tides

Page 31: Geog 3A ~ Final Review Chapter 10 ~ Ocean Waves Chapter 11 ~ Tides

4: The monthly tidal pattern where the tidal range is maximal is known as

a: neap tidesb: full tidesc: spring tidesd: low tidese: high tides

Page 32: Geog 3A ~ Final Review Chapter 10 ~ Ocean Waves Chapter 11 ~ Tides

5: A daily tidal pattern with one high tide and one low tide is called

a: diurnalb: semidiurnalc: mixed semidiurnald: rotatinge: spring

Page 33: Geog 3A ~ Final Review Chapter 10 ~ Ocean Waves Chapter 11 ~ Tides

6: A daily tidal pattern with two high tides and two low tides of equal height is called

a: diurnalb: semidiurnalc: mixed semidiurnald: rotatinge: spring

Page 34: Geog 3A ~ Final Review Chapter 10 ~ Ocean Waves Chapter 11 ~ Tides

7: A daily tidal pattern with two high tides and two low tides of unequal height is called

a: diurnalb: semidiurnalc: mixed semidiurnald: rotatinge: spring

Page 35: Geog 3A ~ Final Review Chapter 10 ~ Ocean Waves Chapter 11 ~ Tides

8: What type of daily tidal pattern occurs in the Gulf of Mexico?

a: diurnalb: semidiurnalc: mixed semidiurnald: rotatinge: spring

Page 36: Geog 3A ~ Final Review Chapter 10 ~ Ocean Waves Chapter 11 ~ Tides

9: What type of daily tidal pattern occurs along the Northeast US coast?

a: diurnalb: semidiurnalc: mixed semidiurnald: rotatinge: spring

Page 37: Geog 3A ~ Final Review Chapter 10 ~ Ocean Waves Chapter 11 ~ Tides

10: In terms of celestial influences on ocean tides, which is more important?

a: distance from Earthb: mass of celestial bodyc: rotational speedd: angle of tilt with respect to its plane of orbit around the Earthe: hard to tell

Page 38: Geog 3A ~ Final Review Chapter 10 ~ Ocean Waves Chapter 11 ~ Tides

11: A daily tidal pattern of two equal high and low tides is known as a ________ tide and occurs in places like _________________.

a: mixed...southern Californiab: diurnal...Galveston, Texasc: semidiurnal...southern Californiad: semidiurnal...Boston, Massachusettse: mixed...Bangor, Maine

Page 39: Geog 3A ~ Final Review Chapter 10 ~ Ocean Waves Chapter 11 ~ Tides

12: In reality, tides propagate dynamically around ocean basins as a

a: tidal waveb: standing wavec: Kelvin waved: all of the abovee: none of the above

Page 40: Geog 3A ~ Final Review Chapter 10 ~ Ocean Waves Chapter 11 ~ Tides

13: A wall of water that rushes into a bay or river as the leading edge of a rising tide is called a

a: tidal waveb: tidal currentc: tidal bored: tidal walle: perigean spring tide

Page 41: Geog 3A ~ Final Review Chapter 10 ~ Ocean Waves Chapter 11 ~ Tides

Geog. Dept. TA Evaluations

Volunteer to take them to Kathy in the Geography Main Office?

Page 42: Geog 3A ~ Final Review Chapter 10 ~ Ocean Waves Chapter 11 ~ Tides

Good luck!Thanks for a great quarter.