Chapter 3 Flashcards

1
Q

What is the Big Bang Theory?

A

A concept that the universe emerged from a single dense, hot state 14 billion years ago. The universe is currently 20 light-years across and will either continue expanding or collapse in on itself, depending on average density matter and energy within.

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2
Q

What is the evidence for the Big Bang Theory?

A
  1. distant star clusters moving away at greater speeds than closer ones
  2. amount of cosmic microwave background radiation is uniform throughout the universe, which implies it represents leftover energy from an early period of expansion
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3
Q

How many galaxies are in the universe and which are we in?

A

The universe contains 50 billion galaxies. We live in the Milky Way with 400 billion stars - it is a typical spiral galaxy consisting of a bright central region with a high density of stars & a flat circular region containing most of the other stars. Younger & brighter stars form in long spiral arms that extend out from the galactic centre, our solar system lies in one of these spiral arms.

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4
Q

How is our solar system structured?

A

8 planets orbit the sun, most of which are too far or too close to habit life. Earth is the 3rd planet and is the perfect distance of orbit for supporting life.

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5
Q

What are terrestrial planets vs jovian planets?

A

Terrestrial planets have solid surfaces and are relatively small in size & mass. Earth, Mercury, Venus and Mars.

Jovian planets are much larger and made up of gases. They tend to have rings around them and also have more moons. Jupiter, Saturn, Uranus, Neptune.

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6
Q

What is the shape of the Earth?

A

Not a perfect sphere, it bulges slightly at the equator and is flattened somewhat at the poles (an oblate spheroid). Circumference at equator=40075km vs poles=40008km.

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7
Q

What causes the Earth’s shape?

A

The bulge at the equator is caused by the centrifugal force of the Earth’s rotation and by the different densities of the Earth’s crust & gravitational field.

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8
Q

How does Earth receive solar radiation?

A

Earth has a curved surface so the intensity of the arriving sun rays varies by latitude.

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9
Q

What is the angle of incidence?

A

The angle at which the sun’s rays strike the Earth’s surface. High at low latitudes, becoming lower going toward the poles. Therefore solar energy is spread over larger surface areas at higher latitudes compared to the same amount received at a lower latitude. Incoming energy = low when angle of incidence = low (high lat.). Lower lat. = more intense solar radiation & higher angle of incidence (75-90) & solar radiation most direct.

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10
Q

How does Earth revolve around the sun?

A

Earth reloves around the sun (every 365 days) on an elliptical path and orbits counterclockwise relative to a view above the North Pole on a flat plane - the plane of the ecliptic. The sun is not located in the centre of orbit and the distance between Earth & sun varies over the course of the year.

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11
Q

What is perihelion?

A

Earth’s closet point to the sun (January) 147 mill km

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12
Q

What is aphelion?

A

Earth’s furthest point from the sun (July) 152 mill km

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13
Q

Earth’s Rotation and Axial Tilt

A

As Earth revolves around the sun it rotates counterclockwise (24h for 1 rotation) on its axis (imaginary line pole to pole). The axis of Earth is an important reference point as it is 23.5 degrees from a line perpendicular to the plane of the ecliptic (maintaining this degree all year) and is the reason for the reasons.

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14
Q

What is the circle of illumination?

A

The great circle on Earth that borders day and night and moves as the Earth rotates.

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15
Q

Time Zones

A

24 time zones
15 degrees each
Each TZ is 7.5 degrees east and west of its meridian
Prime Meridian is the Standard - UTC system calculated as # of hours ahead or behind the Prime Meridian

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16
Q

What is the international date line?

A

180 degrees latitude - the beginning and end of each calendar day

17
Q

What are Canada’s time zones?

A

East to West:

  1. Newfoundland Standard Time
  2. Atlantic Standard Time
  3. Eastern Standard Time
  4. Central Standard Time
  5. Mountain Standard Time
  6. Pacific Standard Time
  • time zones change slightly in the summer in provinces and territories that observe daylight savings time
18
Q

What would happen if Earth’s axis were not tilted?

A

Sun rays would strike most direct at the equator, making the subsolar point, and the amount of energy decreasing toward the poles. All places on Earth would receive the consistent intensity of solar radiation all year / no distinct seasons anywhere.

19
Q

What is the result of Earth’s axial tilt?

A

Earth’s axial tilt is 23.5 degrees from a line perpendicular to the plane of the ecliptic. The angle & orientation are the cause of the seasons. One hemisphere is always gradually tilting more toward the sun the other slowly tilting away.

NH: June- tilted toward Sun, December- tilted away.
SH: opposite

Tilt does not change, nor the orientation of the tilt, however, the position of the Earth relative to the sun changes as orbit progresses. Has the effect of moving each hemisphere toward or away from the sun’s rays, causing seasons bc it results in the migration of the subsolar point 23.5 degrees N or S of the equator in the year.

20
Q

What is the Equinox?

A

When the subsolar point is at the equator and all of Earth has 12 hours of daylight and 12 hours of darkness.

21
Q

What is the Solstice?

A

The angle of incidence is equal to 90 degrees at either of the tropical boundaries.

22
Q

Spring Equinox

A

March 20-21. Beginning of spring in NH, fall in SH. The subsolar point located at the equator, neither NH or SH tilted toward the sun. The circle of illumination extends through the poles, cutting parallels in 1/2. Each point on Earth has 12 hours of daylight & darkness. Equinox = equal day/night.

23
Q

Summer Solstice

A

June 20-21. Beginning of summer in NH, winter in SH. Earth continues to orbit the sun counterclockwise and as the orbit progresses the NH reaches its position of greatest tilt toward the sun. The subsolar point is at the Tropic of Cancer 23.5 degrees N. All latitudes above 66.5 degrees N receive 24 hours daylight (land of the midnight sun). All latitudes above 66.5 degrees S receive 24 hours of darkness.

24
Q

Fall Equinox

A

September 22-23. Fall in NH, spring in SH. The subsolar point is located at the equator. 12 hours of daylight and darkness. Neither hemispheres tilted toward poles.

25
Q

Winter Solstice

A

December 21-22. Winter in NH, summer in SH. NH at greatest tilt away from the sun, SH at greatest tilt toward the sun. The subsolar point at Tropic of Capricorn 23.5 degrees S. All lat. above 66.5 N receive 24-hour darkness, all lat. above 66.5 S receive 24-hour daylight.

26
Q

Precession of Earths Axis

A
  • another factor affecting seasons is the precession of the Earths axis as it spins
  • precession means as the Earth’s axis rotates, the Earth is moving around the sun
  • rotation is caused by the gravitational pull of the Sun & Moon on Earth’s equatorial bulge
27
Q

Day and Night

A
  • sun rises in the east, sets in the west
  • sun reaches its highest position at solar noon
  • when the day is beginning on one side of the circle of illumination, night has begun on the opposite side
28
Q

What is a diurnal cycle?

A

24 hour cycle, related to Earth’s rotation

29
Q

5 reasons for seasons

A
  1. revolution
    - due to axial parallelism
    - N-S hemispheres tilt toward & away from Sun
    - causing changing declination
  2. rotation of Earth’s axis
    - results in the diurnal pattern of day and night as Earth rotates through the circle of illumination
  3. tilts of Earth’s axis
    - determines intensity of seasons
  4. axial parallelism
    - causes change in orientation of N & S hemispheres relative to the Sun
  5. sphericity
    - causes variations in insolation due to angle of incidence