Astronomy Tides and Latitude Quiz
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Questions and Answers

What is the approximate range of latitudes between which the sun appears to move?

  • 0°N to 23°N
  • 0°S to 23°S
  • 23°N to 46°S
  • 23°N to 23°S (correct)
  • What is the primary cause of astronomical tides?

  • The Earth's rotation
  • Gravitational force from the sun and moon alone
  • The combined and simultaneous response of inertia and the gravitational force from the sun and moon (correct)
  • Inertia alone
  • What conditions lead to a spring tide?

  • Earth, moon, and sun forming a right angle
  • Only the moon and Earth in linear alignment
  • When the sun is at its greatest distance to the Earth
  • Earth, moon, and sun in linear alignment (correct)
  • What is the effect of a neap tide?

    <p>High tides that are not very high and low tides that are not very low (B)</p> Signup and view all the answers

    Why doesn't the solar tide completely cancel the lunar tide during a neap tide?

    <p>The moon's contribution to tides is more than twice that of the sun. (D)</p> Signup and view all the answers

    What is the approximate interval between spring and neap tides?

    <p>1 week (C)</p> Signup and view all the answers

    How does the distance between the moon and Earth affect tidal force?

    <p>Tidal force is inversely proportional to the cube of the distance between the bodies. (A)</p> Signup and view all the answers

    What defines the period of the lunar hour angle?

    <p>A lunar day of 24 hr 50.47 min (D)</p> Signup and view all the answers

    What is the primary assumption of the equilibrium theory of tides regarding the ocean surface?

    <p>The ocean surface instantly adjusts to the forces acting upon it, achieving a state of balance. (C)</p> Signup and view all the answers

    According to the equilibrium theory, what two forces are balanced to maintain a stable orbit between the Earth and the Moon?

    <p>Gravitational attraction and inertia (centrifugal force). (B)</p> Signup and view all the answers

    What is the approximate location of the center of mass around which the Earth-Moon system revolves?

    <p>1,650 kilometers inside the Earth. (D)</p> Signup and view all the answers

    Why does the Moon's gravity create two tidal bulges on Earth?

    <p>The Moon's gravity attracts the ocean on the near side, while inertia creates a bulge on the opposite side. (A)</p> Signup and view all the answers

    What are tractive forces, in the context of the equilibrium theory of tides, composed of?

    <p>The sum of gravitational attractions and the force of inertia. (B)</p> Signup and view all the answers

    Which of these is NOT an assumption of the equilibrium theory of tides?

    <p>The Coriolis effect is the most significant factor in tide formation. (C)</p> Signup and view all the answers

    What would happen if the inertia (centrifugal force) between the Earth and the Moon were significantly weaker than their gravitational attraction?

    <p>The Moon would crash into the Earth. (C)</p> Signup and view all the answers

    According to the equilibrium theory of tides, which factor is considered negligible?

    <p>The influence of the seafloor on tides. (C)</p> Signup and view all the answers

    According to the equilibrium theory of tides, what is the primary mechanism driving the movement of tides?

    <p>Earth rotating beneath the tidal bulges aligned with the Moon. (C)</p> Signup and view all the answers

    In the equilibrium model, what is the approximate wavelength of the planet sized tide waves?

    <p>$20,000$ kilometers (A)</p> Signup and view all the answers

    Why is a complete tidal day 24 hours and 50 minutes long?

    <p>Because the moon moves through about $1/27$ of its orbit in a day. (A)</p> Signup and view all the answers

    What happens when the moon is at its maximum declination of $28.5$ degrees north or south of the equator?

    <p>An island north of the equator will pass through the bulge on one side of Earth but miss the bulge on the other side. (D)</p> Signup and view all the answers

    What percentage of the Moon's influence on tides does the Sun have?

    <p>$46%$ (B)</p> Signup and view all the answers

    Which factor does NOT complicate the lunar tides?

    <p>The ocean's average temperature variations throughout the year. (D)</p> Signup and view all the answers

    Which of the following statements accurately describes the relationship between high tides and the bulges in the equilibrium theory?

    <p>High tides correspond to the crests of the planet-sized waves that form the bulges. (C)</p> Signup and view all the answers

    How do solar tides compare to lunar tides in terms of their effect on Earth's oceans?

    <p>Solar tides are weaker than lunar tides but still contribute significantly to tidal variations. (B)</p> Signup and view all the answers

    What is the approximate mean angle of the moon's orbit relative to the plane of the ecliptic?

    <p>5.15 degrees (D)</p> Signup and view all the answers

    What is the period of the lunar declination variation?

    <p>One tropical month of 27.32 solar days (A)</p> Signup and view all the answers

    According to Newton's incomplete explanation, what is the theoretical maximum range of a solar tide?

    <p>24 cm (D)</p> Signup and view all the answers

    Why did Newton consider his explanation of tidal ranges incomplete?

    <p>His calculations predicted tidal ranges much smaller than observed. (A)</p> Signup and view all the answers

    What ocean depth would be required for a tidal crest to move at 1,600 km/h, based on the equilibrium model?

    <p>22 km (C)</p> Signup and view all the answers

    What is the primary cause of different tidal patterns observed at various coastlines?

    <p>Obstruction of tidal crests by landmasses. (B)</p> Signup and view all the answers

    Which of the following is a characteristic of mixed tides?

    <p>Successive high tides or low tides of significantly different heights. (B)</p> Signup and view all the answers

    What happens to water moving north in a Northern Hemisphere ocean due to the influence of amphidromic points?

    <p>It moves toward the eastern boundary of the basin. (A)</p> Signup and view all the answers

    How does a narrow and restricted basin affect the tide wave crest?

    <p>It prevents the tide wave crest from rotating around an amphidromic point, causing it to move in and out of the bay. (A)</p> Signup and view all the answers

    What defines a tidal bore?

    <p>A steep wave moving upstream, generated by the tide crest in a confined river mouth. (D)</p> Signup and view all the answers

    What happens when a river mouth confines a tide wave?

    <p>The tide wave speed exceeds the theoretical shallow-water wave speed. (C)</p> Signup and view all the answers

    What is a flood current?

    <p>Water rushing into an enclosed area because of the rise in sea level. (B)</p> Signup and view all the answers

    What characterizes an Ebb Current?

    <p>Water rushing out because of the fall in sea level as the tide trough approaches. (B)</p> Signup and view all the answers

    When do tidal currents reach their maximum velocity?

    <p>Midway between high tide and low tide. (D)</p> Signup and view all the answers

    What are the periods of the main lunar and solar tides?

    <p>12.42 h and 12 h, respectively. (C)</p> Signup and view all the answers

    What is indicated by the index '2' in tidal constituents like M2 and S2?

    <p>Phenomena that occur twice daily. (B)</p> Signup and view all the answers

    What is the primary cause of storm surges affecting local sea levels?

    <p>Low atmospheric pressure (A)</p> Signup and view all the answers

    Approximately how much power do tides dissipate globally?

    <p>3.75 ± 0.08 TW (C)</p> Signup and view all the answers

    By approximately how much does tidal dissipation increase the length of day per century?

    <p>2.07 milliseconds (B)</p> Signup and view all the answers

    What evidence suggests that a year contained between 400 and 410 days, with each day being about 22 hours long?

    <p>Tidal friction measurements (D)</p> Signup and view all the answers

    What phenomenon has resulted from tidal forces acting between Earth and the Moon?

    <p>The Moon's synchronous tidal locking (B)</p> Signup and view all the answers

    Which statement accurately describes the distribution of marine organisms in the intertidal zone?

    <p>Organisms sort themselves into horizontal bands or subzones. (B)</p> Signup and view all the answers

    What is a potential benefit of using trapped high-tide water to generate electricity?

    <p>Providing an alternative to fossil fuels (B)</p> Signup and view all the answers

    Which of the following can significantly alter local sea level?

    <p>Atmospheric forcing (A)</p> Signup and view all the answers

    Flashcards

    Equilibrium Theory

    Explains ocean tides by balancing forces like gravity and inertia.

    Forces Affecting Tides

    Includes gravitational force from the moon and centrifugal force from Earth’s rotation.

    Stable Orbit

    Condition where two bodies maintain their position due to balanced forces.

    Gravitational Effect

    The moon's gravity pulls the ocean, creating tides towards it.

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    Inertia

    The resistance of any physical object to any change in its velocity.

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    Center of Mass

    The point where two celestial bodies balance each other's gravitational pull.

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    Tide Bulges

    Two raised areas of ocean water caused by the moon's gravity and Earth's tendency to whirl.

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    Tractive Forces

    The combination of gravitational pull and centrifugal force acting on the oceans.

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    Equilibrium Theory of Tides

    A model explaining tidal movements based on Earth's rotation and moon's position.

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    Tidal Day Duration

    A complete tidal day lasts 24 hours and 50 minutes due to the moon's movement.

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    Equator Offset

    The moon's position varies, causing bulges to shift relative to the equator.

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    Lunar Tides

    Tides influenced primarily by the moon's gravitational pull.

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    Solar Tides

    Tides caused by the sun's gravitational pull, weaker than lunar tides.

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    High Tides and Low Tides

    High tides occur at bulges; low tides at troughs between them.

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    Wavelength of Tidal Waves

    Theoretical wavelength of tide waves can reach 20,000 km.

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    Astronomical Tides

    Tides caused by the gravitational force from the sun and moon together.

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    Spring Tide

    Occurs when the Earth, moon, and sun align, resulting in higher high tides and lower low tides.

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    Neap Tide

    Occurs when the moon, Earth, and sun form a right angle, resulting in less extreme tides.

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    Tidal Force

    The gravitational influence causing tides, inversely proportional to the cube of the distance between two bodies.

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    Perigee

    The position where the moon is closest to Earth in its orbit.

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    Apogee

    The position where the moon is farthest from Earth in its orbit.

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    Lunar Day

    The period it takes for the moon to complete one rotation relative to the Earth, which is about 24 hours and 50.47 minutes.

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    Solar Day

    The period of one complete rotation of Earth on its axis, approximately 24 hours.

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    Earth's axial tilt

    The angle of Earth's axis relative to its orbit, approximately 23.45°.

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    Ecliptic

    The plane of Earth's orbit around the Sun.

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    Lunar declination

    The angle of the Moon's orbit relative to the ecliptic, varying between ±5.15°.

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    Tidal bulge

    The rise in water level due to gravitational pull from the Moon and Sun.

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    Equilibrium model of tides

    A basic model predicting tidal behavior assuming a calm ocean without landmass interference.

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    Semidiurnal tides

    Tidal pattern with two high and two low tides each lunar day.

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    Amphidromic points

    The points in ocean basins where tidal crests do not rotate, affecting local tide height.

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    Mixed tides

    Tide pattern featuring variations in height between successive high or low tides.

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    Tidal Current

    The flow of water caused by the rise and fall of tide crests in bays and harbors.

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    Flood Current

    Water that rushes into an area as tide crests rise.

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    Ebb Current

    Water that flows out as tide troughs approach, causing a drop in sea level.

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    Slack Water

    A period with no tidal current, occurring at high and low tides.

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    Tidal Constituents

    Components that make up total tides, characterized by amplitude, phase, and period.

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    Moon and Sun's Effects

    Lunar and solar tides characterized by periods of 12.42 h and 12 h, respectively.

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    Atmospheric Forcing

    Influence of atmospheric conditions on sea levels, especially near shore.

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    Storm Surge

    Rise in sea level due to low atmospheric pressure and strong winds.

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    Tidal Power Dissipation

    Tides dissipate ~3.75 TW of power, affecting Earth's rotation.

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    Slowing Earth's Rotation

    Tidal friction gradually decreases Earth's rotation speed.

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    Synchronous Tidal Locking

    The moon's rotation is locked to its orbit around Earth, showing one side to us.

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    Intertidal Zone

    Area between high-tide and low-tide marks with unique organisms.

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    Tidal Subzones

    Different bands in the intertidal zone where organisms live adapted to specific conditions.

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    Power Extraction

    Generating electricity from trapped high-tide water as an alternative energy source.

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    Study Notes

    Introduction to Oceanography - Tides

    • Tides are periodic, short-term changes in ocean surface height, caused by gravity and inertia.
    • The gravitational pull of the Moon and Sun, along with Earth's motion and water inertia, create tides.
    • Tides are the longest waves, with wavelengths that can equal half of Earth's circumference.
    • The pull of gravity between two bodies is proportional to their masses but inversely proportional to the square of the distance between them.
    • The force of gravity that creates tides varies inversely with the cube of the distance from Earth's center to the tide-generating object's center.
    • The Sun exerts less influence on tides than the Moon, despite being much more massive, due to greater distance.

    Aim & Learning Outcomes

    • Understand the equilibrium theory of tides.
    • Understand the dynamic theory of tides.
    • Understand several major impacts of tides.

    Tides as Ocean Waves

    • Tides are considered a type of ocean wave.
    • Crucial characteristics of tides include their periodicity and short-term nature.

    Tides Theory

    • Equilibrium and Dynamic are two foundational theories that explain tides.

    Equilibrium Theory

    • Primarily focuses on the positions and gravitational forces of Earth, Moon, and the Sun.
    • Disregards the effects of ocean depth and continental landmasses.
    • Assumes an idealized, uniformly water-covered Earth.

    Dynamic Theory

    • Considers the actual speed of tidal waves, the presence of landmasses, and water's circular movement.
    • Explains several key characteristics of tidal behaviours.

    Equilibrium Theory of Tides - Basic Principle

    • Tidal potential is derived from Moon and Sun's gravitational forces.
    • The equilibrium theory examines the balance of forces allowing planets to maintain stable orbits.

    Equilibrium Theory of Tides - Basic Assumptions

    • The seabed does not influence tides.
    • Ocean surfaces instantly conform to forces that affect them.
    • Ocean surfaces are always in equilibrium (balance) with the forces acting on them.

    Equilibrium Theory of Tides - Gravitational Force and Inertia

    • Earth and Moon don't collide because of a balance between their mutual gravitational attraction and their inertia (centrifugal force).
    • Earth-Moon systems revolve around a common center of mass, located within Earth.
    • The Moon's gravity pulls ocean water towards it, creating a bulge.
    • Earth's rotation creates a second bulge on the opposite side of Earth.

    Equilibrium Theory of Tides - Tractive Forces

    • Tractive forces result from the combined effects of inertia and gravitational attraction, causing tidal bulges.
    • At locations nearer the Moon, gravitational force surpasses inertia.
    • At locations farther from the Moon, inertia surpasses gravitational force.

    Equilibrium Theory of Tides - Rhythm of Tides

    • Tidal bulges remain aligned with the Moon as Earth rotates.
    • An island on the equator experiences tidal movements through a 24-hr period.
    • Tidal crests are high tides, and the troughs in between are low tides.
    • Tidal wavelength is around 20,000 km.

    Equilibrium Theory of Tides - Lunar Tides Complications

    • Moon's unique orbital specifications modify gravitational and inertial interactions with Earth.
    • Tidal days are longer than solar days (24 hours 50 minutes).
    • Moon's position relative to Earth's equator changes over time, affecting tidal bulges.

    Equilibrium Theory of Tides - Solar Tides

    • Driven by gravitational forces between Sun and Earth.
    • Sun's influence on tides (46%) is less than Moon's.
    • Solar bulges follow Sun's movement daily, having similar variations to lunar bulges concerning locations above or below equator.

    Equilibrium Theory of Tides - Astronomical Tides

    • Tides that result from combined gravitational forces of Moon and Sun are categorized as astronomical tides.
    • Spring tides occur when Earth, Moon, and Sun are aligned, resulting in high highs and low lows.
    • Neap tides occur when the celestial bodies form a right angle, resulting in less extreme high and low tides.
    • Orbital variations of Sun and Moon influence tidal ranges.

    Dynamic Theory of Tides - Newton Incomplete Explanation

    • Newton's explanation of tides was incomplete, as the predicted tidal range (55cm for Moon, and 24cm for Sun) was significantly smaller than observed (2m for typical tides).
    • The theoretical equilibrium position of ocean surface is not reached at any instant; hence, tides behave as waves.

    Dynamic Theory of Tides - Tidal Patterns

    • Earth's rotation, landmasses, and ocean basin shapes influence tidal patterns.
    • Semidiurnal, diurnal, and mixed tides are possible, each with distinct characteristics.

    Dynamic Theory of Tides - Amphidromic Points

    • Nodes with no apparent tides are called amphidromic points.
    • Tidal crests rotate around amphidromic points in respective hemispheres (clockwise in South, counterclockwise in North).
    • Tides are more extreme farther from the amphidromic point.

    Dynamic Theory of Tides - Tidal Datum

    • A reference plane is the tidal datum, marking the zero point on tide graphs.
    • Datum may vary from coast to coast.
    • Tidal datum is an average of mean sea level, using tidal records over several years.

    Dynamic Theory of Tides - Influence of Ocean Basin Shape

    • Tidal ranges are influenced by ocean basin shape.
    • Wide basins have mini-amphidromic points resembling open-ocean patterns.
    • Narrow basins yield tidal waves that simply move in and out of bays.

    Dynamic Theory of Tides - Tidal Bore / Tidal Wave

    • A tidal bore (wave) forms in river inlets due to substantial tidal variations.
    • Tidal wave speeds overcome theoretical shallow-water wave speeds in confined river mouths.

    Dynamic Theory of Tides / Tidal Current

    • Tide currents flow in and out of harbors and bays, following the rise and fall of tides.
    • Flood currents approach, and ebb currents leave.
    • Tidal currents reach peak velocity between highs and lows.
    • Slack water periods occur at high and low tides.

    Dynamic Theory of Tides – Tidal Constituents

    • Many subcomponents, or constituents, create the observed tides (e.g., M2 and S2 are main lunar and solar).
    • Constituents are defined by amplitude, phase, and period.

    Dynamic Theory of Tides – Tidal Prediction – Shallow Water

    • Tide gauges are used to measure shallow-water tides.
    • Harmonic method models tides based on >19 years of data of coastal tide gauges.
    • Response method determines the relationship between observed tide and tidal potential.

    Dynamic Theory of Tides - Tidal Prediction – Deep Ocean

    • Satellite altimeters are used in measuring deep-ocean tides.
    • Altimeter data is used with numerical models to trace tides across the entire ocean (deep-sea to coast).

    Dynamic Theory of Tides – Tidal Prediction – Deviation

    • Atmospheric pressure and wind directly affect local sea levels.
    • Storm surges and seiches result from atmospheric pressure impact and strong winds, respectively.

    Several Effects of Tides – Planetary Effects

    • Tides cause energy dissipation within Earth.
    • Tidal friction gradually reduces Earth's rotation speed.

    Several Effects of Tides – Marine Organisms

    • Organisms near the high and low tide marks face fluctuating conditions.
    • Organisms in intertidal zones exhibit adaptations to variable submersion and emergence.

    Several Effects of Tides – Power Extraction

    • Tide energy can be extracted, supplying an alternative to fossil fuel-based power.
    • Tidal power stations utilize the movement of water to generate electricity.

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    Description

    Test your knowledge on astronomical tides and the sun's movement across latitudes. This quiz explores the mechanisms behind spring and neap tides, the effects of the moon's gravity, and the equilibrium theory of tides. Ideal for students studying astronomy or Earth sciences.

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