AQA · A-Level · Physics

    Course version: 7408 · Version from Sept 2016

    Use of satellites in low orbits and geostationary orbits, to include plane…

    Full specification wording

    Orbits of planets and satellites (A-level only): Use of satellites in low orbits and geostationary orbits, to include plane and radius of geostationary orbit.

    Satellites stay in orbit because gravity supplies the centripetal force.

    Checked against the AQA 7408 specification (opens in a new tab) on .

    • Point 4 of 4
    • 4 key terms

    Study notes

    From the checked teaching notes for this specification point.

    The idea

    Satellites stay in orbit because gravity supplies the centripetal force. For a circular orbit, equate GMm/r² to mv²/r, giving v = √(GM/r) and T² = 4π²r³/(GM). A low orbit has a small radius, so it is fast and has a short period; these are used for Earth observation, imaging, and weather monitoring. A geostationary orbit has T = 24 hours, lies in the equatorial plane, and moves west to east so the satellite appears fixed above one point. Substituting T = 8.64 × 10⁴ s and GM = 3.99 × 10¹⁴ m³ s⁻² gives r ≈ 4.22 × 10⁷ m from Earth's centre, so the height above the surface is about 3.6 × 10⁷ m. The plane must contain the equator; any inclined orbit would drift north and south.

    What earns the marks

    • Gravitational force provides the centripetal force: GMm/r² = mv²/r, so v = √(GM/r).
    • Period relation: T² = 4π²r³/(GM), so r³ = GMT²/(4π²).
    • Low orbit: smaller r gives larger v and shorter T; typical periods are about 90 minutes, used for Earth observation and imaging.
    • Geostationary orbit: T = 24 h = 8.64 × 10⁴ s, equatorial plane, same sense as Earth's rotation.
    • Radius from centre r ≈ 4.22 × 10⁷ m; height above surface ≈ 3.6 × 10⁷ m.
    • Geostationary satellites are used for communication and weather monitoring because the ground antenna can be fixed.

    Common mistakes and how to put them right

    • Using the height above the surface as r in GMm/r² or T² = 4π²r³/(GM).

      Put it right by adding Earth's radius, 6.37 × 10⁶ m, to the height.

    • Treating a geostationary orbit as merely any 24-hour orbit.

      Put it right by stating it must also be equatorial and in the same sense as Earth's rotation.

    • Assuming a polar low-Earth orbit is geostationary.

      Put it right by noting that a polar orbit does not keep a fixed position over the equator.

    Exam tips

    • Start orbital calculations by writing the force equation before substituting numbers, so the physics is clear.
    • Convert 24 hours to seconds before using T² = 4π²r³/(GM).
    • When asked for height, subtract Earth's radius from the orbital radius and state the unit.
    • Use a clear sketch to show r measured from Earth's centre and the equatorial plane.

    Try the lesson

    The start of the Orbits of planets and satellites (A-level only): Use of satellites in low orbits and geostationary orbits, to include plane and radius of geostationary orbit. lesson, made from checked teaching notes for this specification point.

    Have a go first

    Which statement describes the orbit of a geostationary satellite?

    Listen

    Satellites stay in orbit because gravity supplies the centripetal force. For a circular orbit, equate GMm/r² to mv²/r, giving v = √(GM/r) and T² = 4π²r³/(GM). A low orbit has a small radius, so it is fast and has a short period; these are used for Earth observation, imaging, and weather monitoring. A geostationary orbit has T = 24 hours, lies in the equatorial plane, and moves west to east so the satellite appears fixed above one point. Substituting T = 8.64 × 10⁴ s and GM = 3.99 × 10¹⁴ m³ s⁻² gives r ≈ 4.22 × 10⁷ m from Earth's centre, so the height above the surface is about 3.6 × 10⁷ m. The plane must contain the equator; any inclined orbit would drift north and south. A strong answer earns marks for these points. Gravitational force provides the centripetal force: GMm/r² = mv²/r, so v = √(GM/r). Period relation: T² = 4π²r³/(GM), so r³ = GMT²/(4π²). Low orbit: smaller r gives larger v and shorter T; typical periods are about 90 minutes, used for Earth observation and imaging. Geostationary orbit: T = 24 h = 8.64 × 10⁴ s, equatorial plane, same sense as Earth's rotation. A common slip: Using the height above the surface as r in GMm/r² or T² = 4π²r³/(GM). Instead, adding Earth's radius, 6.37 × 10⁶ m, to the height. Exam tip: Start orbital calculations by writing the force equation before substituting numbers, so the physics is clear.

    See it

    A top-down flowchart. At the top, a node states that gravity supplies the centripetal force, GMm/r² = mv²/r. This branches into two equation nodes: v = √(GM/r) and T² = 4π²r³/(GM). From the period equation, one branch leads to a low orbit with small r, which gives larger v and shorter T, and these are used for Earth observation, imaging and weather monitoring. The other branch leads to a geostationary orbit with T = 24 h, which lies in the equatorial plane and moves in the same sense as Earth's rotation, so the satellite appears fixed above one point; these are used for communication and weather monitoring.
    How the orbital equations lead to the contrasting properties and uses of low and geostationary orbits.

    Key words

    Say what each word means before you turn the card.

    Low orbit

    Try answering aloud or in your head before turning the card.

    Geostationary orbit

    Try answering aloud or in your head before turning the card.

    Radius of geostationary orbit

    Try answering aloud or in your head before turning the card.

    Equatorial plane

    Try answering aloud or in your head before turning the card.

    See every definition
    Low orbit
    A small radius orbit, so it is fast and has a short period, used for Earth observation, imaging, and weather monitoring.
    Geostationary orbit
    Has T = 24 hours, lies in the equatorial plane, and moves west to east so the satellite appears fixed above one point.
    Radius of geostationary orbit
    Substituting T = 8.64 × 10⁴ s and GM = 3.99 × 10¹⁴ m³ s⁻² gives r ≈ 4.22 × 10⁷ m from Earth's centre.
    Equatorial plane
    The plane must contain the equator; any inclined orbit would drift north and south.

    Label the diagram

    Some boxes have lost their names. Pick the right name for each number.

    The diagram again, with 3 boxes numbered instead of named. A top-down flowchart. At the top, a node states that gravity supplies the centripetal force, GMm/r² = mv²/r. This branches into two equation nodes: v = √(GM/r) and T² = 4π²r³/(GM). From the period equation, one branch leads to a low orbit with small r, which gives larger v and shorter T, and these are used for Earth observation, imaging and weather monitoring. The other branch leads to a geostationary orbit with T = 24 h, which lies in the equatorial plane and moves in the same sense as Earth's rotation, so the satellite appears fixed above one point; these are used for communication and weather monitoring.
    • 1Box 1

    • 2Box 2

    • 3Box 3

    0 of 3 labelled

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