← Back to Waves

⚑ Radiation Balance and Earth's Temperature

Spec 6.6.5.4 (HT only) πŸ“™ Higher
πŸ“– In-Depth Theory

Radiation Balance

The TEMPERATURE of any object, including Earth, is determined by the BALANCE between incoming and outgoing radiation.
EQUILIBRIUM CONDITION:
Temperature stays CONSTANT when rate of energy absorbed = rate of energy emitted.
If absorbed > emitted β†’ temperature RISES.
If emitted > absorbed β†’ temperature FALLS.
EARTH'S RADIATION BALANCE:
INPUT: solar radiation (mostly visible light and UV from the Sun).
Earth absorbs solar radiation β†’ warms up β†’ emits infrared (longer wavelength β€” Earth is much cooler than Sun).
OUTPUT: infrared radiation emitted by Earth to space.
At equilibrium: incoming solar power = outgoing infrared power.
This determines Earth's average surface temperature (~15Β°C currently).

The Greenhouse Effect

GREENHOUSE GASES (COβ‚‚, Hβ‚‚O, CHβ‚„) in the atmosphere absorb outgoing infrared radiation.
NATURAL GREENHOUSE EFFECT:
Sun emits visible light β†’ passes through atmosphere (not absorbed) β†’ absorbed by Earth's surface β†’ Earth warms β†’ emits infrared.
Infrared partially absorbed by greenhouse gases β†’ atmosphere warms β†’ re-emits radiation in all directions (including back to Earth).
This RAISES Earth's temperature above what it would be without the atmosphere.
Without any greenhouse effect: Earth's average temperature would be about βˆ’18Β°C.
ENHANCED GREENHOUSE EFFECT:
Human activities increase concentrations of greenhouse gases (burning fossil fuels β†’ COβ‚‚; livestock β†’ CHβ‚„).
More infrared absorbed β†’ more re-emitted back to Earth β†’ warming β†’ GLOBAL WARMING.
CLIMATE CHANGE EFFECTS:
Melting ice caps β†’ rising sea levels.
Extreme weather events more frequent.
Shifting ecosystems and agricultural zones.

Earth's Temperature and Radiation

FACTORS AFFECTING EARTH'S TEMPERATURE:
1. SOLAR INTENSITY: distance from Sun β†’ amount of solar radiation reaching Earth.
2. ALBEDO: reflectivity of Earth's surface (ice and snow reflect more; oceans and forests absorb more).
3. GREENHOUSE GAS CONCENTRATION: more gases β†’ more insulation.
4. VOLCANIC ACTIVITY: releases COβ‚‚ and sulfur dioxide (short-term cooling from aerosols).
PLANET TEMPERATURES:
MERCURY: close to Sun but no atmosphere β†’ extreme temperature swings, no greenhouse effect.
VENUS: similar distance to Earth but thick COβ‚‚ atmosphere β†’ 465Β°C (extreme greenhouse effect).
MARS: thin atmosphere β†’ βˆ’60Β°C average.
A BODY RADIATES MOST AT WAVELENGTH determined by its temperature:
Hotter β†’ peak at shorter wavelength.
Sun (~5500Β°C) β†’ visible light.
Earth (~15Β°C) β†’ infrared.
This wavelength difference is why greenhouse gases (which absorb IR but not visible) are key to climate.
⚠️ Common Mistake

Earth emits INFRARED radiation β€” not the same as the visible light from the Sun. Greenhouse gases absorb INFRARED (outgoing from Earth) not visible light (incoming from Sun). The natural greenhouse effect is beneficial β€” without it, Earth would be too cold for life. The ENHANCED greenhouse effect from human emissions is the problem.

πŸ“Œ Key Note

Radiation balance: absorbed energy = emitted energy β†’ constant temperature. Earth absorbs solar (visible), emits IR. Greenhouse gases absorb outgoing IR β†’ re-emit β†’ warming. Natural greenhouse: necessary (without it, βˆ’18Β°C). Enhanced: human emissions increase warming. Factors: solar intensity, albedo, greenhouse gas concentration.

🎯 Matching Activity β€” Radiation Balance

Match each statement to the correct radiation balance concept. β€” drag the symbols on the right to match the component names on the left.

Absorbed > emitted
Drop here
Absorbed = emitted
Drop here
Natural greenhouse effect
Drop here
Enhanced greenhouse effect
Drop here
Greenhouse gases absorb outgoing IR and re-emit β€” raises Earth's temperature to ~15Β°C
Object temperature rises β€” radiation imbalance causing warming
Object at constant temperature β€” thermal equilibrium
Increased COβ‚‚ from fossil fuels β†’ more IR absorbed β†’ global warming
⭐ Higher Tier Only

HT only β€” explain how radiation balance determines temperature. Explain the greenhouse effect mechanistically β€” why greenhouse gases warm Earth. Evaluate the effects of increasing greenhouse gas concentrations on Earth's radiation balance and temperature.

πŸ”¬ Triple Science Only

Radiation balance and Earth's temperature (HT only, physics only) β€” not in Combined Science as a quantitative topic.

🎯 Test Yourself
Question 1 of 2
1. Why do greenhouse gases absorb outgoing infrared from Earth but not incoming solar visible light?
2. Without any greenhouse effect, what would Earth's average temperature be?
⭐ How Well Do You Understand This Topic?

Be honest with yourself β€” this helps you know what to revise!

Don't get it Getting there Nailed it!
πŸ€– Ask Mr Badmus AI

Stuck? Just ask! πŸ’¬

I'll use FIFA for calculations and flag Higher/Triple content clearly.

πŸ“‹ All Waves subtopics

Mr. Badmus AI

GCSE Science Tutor

preview