6.1

earth, the moon, and the solar system

6.1.1 earth, moon, and planetary motion

axis and rotation

the axis is an imaginary line around which the earth rotates.

  • runs from antarctica to the arctic ocean
  • earth completes one rotation in approximately 24 hours
  • day and night are caused by rotation about the axis

equator and hemispheres

the equator is an imaginary line that divides the earth into two halves.

  • above the equator is the northern hemisphere
  • below the equator is the southern hemisphere
earth equator and hemispheres

seasons

  • the earth is tilted at an angle of 23.5°
  • sunlight does not strike both hemispheres at the same angle
  • the hemisphere tilted towards the sun experiences summer
  • summer has longer days and more direct sunlight

orbit of the moon

  • the moon orbits the earth approximately once every month
  • only the sunlit side of the moon reflects light
  • different amounts of the lit side are visible from earth
  • this causes the phases of the moon
phases of the moon

orbital speed of planets

orbital speed is calculated using distance travelled divided by time.

speed = distance / time

for a circular orbit:

distance = 2πr

speed = 2πr / orbital period

6.1.2 the solar system

components of the solar system

  • the sun is a star
  • there are eight planets: mercury, venus, earth, mars, jupiter, saturn, uranus, neptune
  • moons orbit planets
  • minor planets include pluto and similar bodies
  • asteroids are mainly found between mars and jupiter
  • comets are made of dust and gas

planetary orbits

  • planets have elliptical orbits
  • the sun is not at the centre of the orbit
  • planets orbit a point between themselves and the sun
elliptical orbit of a planet

formation of planets

  • the first four planets are small and rocky
  • the outer four planets are large and gaseous

formation process:

  • hydrogen and other elements were spread throughout space
  • gravity pulled particles together to form the sun
  • remaining gas and dust formed a rotating accretion disc
  • gravity pulled dust together to form rocks and planets
  • heat from the sun pushed lighter gases outward
  • this formed the gaseous outer planets

gravitational field strength

  • gravitational field strength depends on mass
  • it decreases with increasing distance from the object
  • the sun has the strongest gravitational field in the solar system
  • orbital speeds of planets decrease with distance from the sun

changing speed of a comet

  • comets have highly elliptical orbits
  • comets move faster when closer to the sun
  • gravitational potential energy decreases as distance decreases
  • kinetic energy increases as speed increases
  • total energy remains constant

total energy = gravitational potential energy + kinetic energy