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Climate Forcing

The Earth's climate changes when the amount of energy stored by the climate system is varied. The most significant changes occur when the global energy balance between incoming energy from the Sun and outgoing heat from the Earth is upset. There are a number of natural mechanisms that can upset this balance, for example fluctuations in the Earth's orbit, variations in ocean circulation and changes in the composition of the Earth's atmosphere. In recent times, the latter has been evident as a consequence not of natural processes but of man-made pollution, through emissions of greenhouse gases. By altering the global energy balance, such mechanisms "force" the climate to change. Consequently, scientists call them "climate forcing" mechanisms.

 

Climate Change

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Radiative Forcing
Climate Change Basics
NASA GISS
NASA GISS

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Introduction
Atmosphere
Causes
Climate Forcing
Climate System
Comets
Continental Drift
Earth's Orbit
Energy Balance
Evidence
Feedback
Global Warming
Greenhouse Effect
Greenhouse Gases
Historical Records
Ice Ages
Ice Cores
Instrumental Records
Interglacials
Little Ice Age
Modelling
Mountains
Oceans
Palaeoclimate Change
Palaeoclimate Records
Palaeoclimatology
Sea Sediments
Sun
Time
Tree Rings
Volcanoes

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