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, HβO, 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 β18Β°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 β60Β°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.
β οΈ 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.
π 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, β18Β°C). Enhanced: human emissions increase warming. Factors: solar intensity, albedo, greenhouse gas concentration.
π― 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
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Absorbed = emitted
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Natural greenhouse effect
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Enhanced greenhouse effect
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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
β 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.
π¬ Triple Science Only
Radiation balance and Earth's temperature (HT only, physics only) β not in Combined Science as a quantitative topic.
π― 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?
β How Well Do You Understand This Topic?
Be honest with yourself β this helps you know what to revise!
Don't get itGetting thereNailed it!
π€ Ask Mr Badmus AI
Stuck? Just ask! π¬
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