Know that microwave radiation of a specific frequency is observed at all points in space around us and is known as cosmic microwave background radiation (CMBR)
6.1 The Earth – Rotation, Tilt and Seasons
1. Rotation
Earth rotates once about its axis every 24 h (≈ 86 400 s).
Result: the regular alternation of day and night.
Linear speed at the equator:
v = 2πR / T ≈ 2π (6.37 × 10⁶ m) / 86 400 s ≈ 465 m s⁻¹
2. Axial tilt
Earth’s axis is tilted 23.5° to the plane of its orbit (the ecliptic).
The tilt, together with the orbital motion, causes the Sun’s apparent height in the sky to change over the year – giving the seasons.
When the Northern Hemisphere is tilted towards the Sun the days are longer and the Sun appears higher → summer; the opposite gives winter.
3. Seasons – quick exam checklist
Identify the season in a given hemisphere by the tilt direction.
Remember: the length of a year (orbital period) is 365 days 6 h 9 min ≈ 1 yr.
Key point for AO1: “The Earth’s rotation causes day/night, its tilt (23.5°) causes the seasons.”
Suggested diagram: Earth‑Sun geometry showing tilt in summer and winter (labelled 23.5°).
6.2 The Solar System
1. Overview
The Sun is at the centre of a system of eight planets, dwarf planets, moons, asteroids and comets. All objects move in (approximately) elliptical orbits due to the Sun’s gravity.
2. Planets – key facts (core IGCSE content)
#
Planet
Type
Mean distance from Sun
Orbital period
Notable feature
1
Mercury
Terrestrial
0.39 AU
88 d
No atmosphere, extreme temperature range
2
Venus
Terrestrial
0.72 AU
225 d
Thick CO₂ atmosphere, surface pressure ≈ 92 bar
3
Earth
Terrestrial
1.00 AU
365 d
Life‑supporting, liquid water
4
Mars
Terrestrial
1.52 AU
687 d
Red surface, thin CO₂ atmosphere
5
Jupiter
Gas giant
5.20 AU
12 yr
Largest planet, strong magnetic field
6
Saturn
Gas giant
9.58 AU
29 yr
Prominent ring system
7
Uranus
Ice giant
19.2 AU
84 yr
Rotates on its side (≈ 98° tilt)
8
Neptune
Ice giant
30.1 AU
165 yr
Strong winds, dark methane clouds
3. Dwarf planets, moons, asteroids & comets
Dwarf planets – bodies that orbit the Sun and are massive enough to be round, but have not cleared their orbital zone. Examples: Pluto, Eris, Ceres.
Moons – natural satellites. Earth has one (the Moon); Jupiter has >70, Saturn >80, etc.
Asteroids – rocky bodies mainly in the asteroid belt between Mars and Jupiter.
Comets – icy bodies from the Kuiper Belt or Oort Cloud that develop a coma and tail when near the Sun.
This material is not required for the core IGCSE exam but is useful for deeper understanding or extension work.
1. What is the CMBR?
A faint, uniform glow of electromagnetic radiation that fills the whole Universe.
Observed in every direction – the same at all points in space.
Remnant “after‑glow” of the hot, dense early Universe (the Big Bang).
2. Key observational facts
Discovered in 1965 by Arno Penzias and Robert Wilson using a horn antenna.
Has an almost perfect black‑body spectrum with an average temperature 2.725 K.
Peak wavelength (Wien’s law)
λmax = b/T ≈ 2.898 × 10⁻³ / 2.725 ≈ 1.06 mm
Corresponding peak frequency
νmax ≈ c/λmax ≈ 2.8 × 10¹¹ Hz ≈ 160 GHz
Falls in the microwave region of the electromagnetic spectrum (≈ 300 MHz – 300 GHz).
Isotropic to about one part in 10⁵; tiny anisotropies map the density fluctuations that later formed galaxies.
3. How is it detected?
Ground‑based radio telescopes with very sensitive microwave receivers (e.g., Atacama Cosmology Telescope).
High, dry sites or space platforms are chosen to minimise atmospheric absorption.
Satellites – COBE, WMAP and Planck – have measured the spectrum and temperature with high precision.
4. Numerical summary (quick revision)
Property
Symbol / Value
Units
Notes
Average temperature
T = 2.725
K
COBE FIRAS measurement
Peak wavelength
λmax ≈ 1.06
mm
Wien’s law λmax=b/T
Peak frequency
νmax ≈ 160
GHz
c = λν
Temperature anisotropy
ΔT/T ≈ 10⁻⁵
–
WMAP & Planck maps
5. Using Wien’s law – exam skill (AO2)
Wien’s displacement law for wavelength: λmax = b/T, where b = 2.898 × 10⁻³ m·K.
Example – Find λmax for T = 2.7 K
λmax = (2.898 × 10⁻³ m·K) / 2.7 K
≈ 1.07 × 10⁻³ m = 1.07 mm
Then obtain the frequency: νmax = c/λmax ≈ 3.00 × 10⁸ m s⁻¹ / 1.07 × 10⁻³ m ≈ 2.8 × 10¹¹ Hz (≈ 160 GHz).
6. Why it supports the Big‑Bang model (AO1)
The hot‑big‑bang theory predicted a relic radiation field; its discovery confirmed the prediction.
The observed black‑body spectrum matches the theoretical Planck curve for 2.7 K.
Measured anisotropies provide the seeds for later galaxy formation.
Suggested diagram: Black‑body curve peaking at ~160 GHz with the CMBR spectrum highlighted.
4 Practical Skills linked to Space Physics (AO3)
Activity 1 – Modelling Earth’s tilt and the seasons
Materials: a bright lamp (Sun), a white ball (Earth), a protractor, a marker.
Fix the ball on a stand so it can rotate. Tilt the axis to 23.5°.
Rotate the ball once while keeping the lamp fixed; observe which hemisphere receives more light at different positions.
Record observations and label the four seasons for each hemisphere.
Safety: do not look directly at the lamp when it is on; keep the lamp away from flammable materials.
Activity 2 – Measuring the apparent diameter of the Moon
Use a simple “pinhole camera” (a cardboard box with a small circular hole) and a sheet of white paper as a screen.
During a clear night, point the camera at the Moon and measure the diameter of the projected image with a ruler.
Calculate the Moon’s angular size using θ ≈ (image diameter / distance to screen) (radians) and convert to degrees (1 rad ≈ 57.3°).
Compare your result with the accepted value ≈ 0.5°.
Safety: never look directly at the Sun through the pinhole camera.
Link to assessment objectives
AO1 – Knowledge: recall facts about Earth’s rotation, tilt, planetary order, and (if chosen) the CMBR.
AO2 – Application: use formulas such as v = 2πr/T for Earth’s equatorial speed, or θ = s/D for angular size.
AO3 – Practical/experimental: design, carry out and analyse the two activities above; present results in a simple table or graph.
Exam Revision Checklist (IGCSE 0625 – Space Physics)
State that the Earth rotates once every 24 h → day/night.
State the axial tilt (23.5°) and explain how it produces the seasons.
List the eight planets in order, give one key feature for each, and know the difference between terrestrial and giant planets.
Define dwarf planets, moons, asteroids and comets.
Be able to calculate:
Linear speed at the equator (v = 2πR/T).
Orbital speed of the Moon (v = 2πr/T, with r ≈ 3.84 × 10⁸ m, T ≈ 2.36 × 10⁶ s → v ≈ 1.02 km s⁻¹).
Peak wavelength of a black‑body using Wien’s law (extension only).
Remember the practical safety points when working with bright lamps or the Sun.
If you attempt the extension material, be ready to state:
What the CMBR is and why it is called “microwave” (λ ≈ 1 mm, ν ≈ 160 GHz).
How its discovery supports the Big‑Bang theory.
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