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SAGES Scottish Alliance for Geoscience, Environment & Society. Observing and Modelling Climate Change Simon Tett, Chair of Earth System Dynamics & Modelling, University of Edinburgh. Greenhouse Gas changes.
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SAGESScottish Alliance for Geoscience, Environment & Society Observing and Modelling Climate Change Simon Tett, Chair of Earth System Dynamics & Modelling, University of Edinburgh
Greenhouse Gas changes Global atmospheric concentrations of CO2, methane and N2O have increased as a result of human activity since 1750 • Far exceed pre-industrial values. CO2 increase primarily due to fossil fuel use and land-use change
Global Mean Temperature Red bars show annual average. Grey bars the possible range. Blue line is smoothed to show slow change From Brohan et al, 2006
The longer perspective Recent warming unprecedented
What are we trying to understand? How might the earth system evolve in the future? How and why did it evolve in the past? Image created by Reto Stockli with the help of Alan Nelson, under the leadership of Fritz Hasler
The Earth is Dynamic Shows weather. Weather what you get, Climate is what you expect From Space Science and Engineering Center, University of Wisconsin-Madison
Greenhouse Effect Energy from Sun Cooling at about 6.5 o C/Km Heat Energy escapes to space. At balance energy in from sun is the same as heat energy to space Surface
Adding more Greenhouse gases to the atmosphere Energy from Sun Cooling at about 6.5 o C/Km Same Heat Energy escapes to space but from higher in the atmosphere Surface Surface Temperature warms
Feedbacks • Act to amplify (or damp) warming from changes in carbon dioxide,other greenhouse gases and other climate drivers. • Water vapour – warmer atmosphere can store more water vapour. Water vapour absorbs “heat” radiation so is a Greenhouse gas. • Warmer world will have more moisture in the atmosphere and so will trap more heat. Increases warming • Clouds have two main effects: • Trap heat energy so add to the greenhouse effect • Reflect energy from sun back to space so cool climate • Relative importance of these two effects uncertain. High clouds tend to warm while low clouds cool. How relative proportions change as climate changes is a large uncertainty in estimates of future climate change • Ice/Snow feedback. • Ice and snow are white and reflect solar energy back to space. • Melting ice and snow will cause more solar radiation to be absorbed which in turn will warms the climate.
Snow/Ice Feedback Image courtesy NASA/GSFC/JPL, MISR Team. See http://visibleearth.nasa.gov/ Summer Winter
Climate Modelling • Modelling of the atmospheric flow has long history – first attempts, using computers, made in 1950’s. • General Circulation Models developed from computer models used to forecast weather • These models represent atmosphere, ocean, ice, land-surface, carbon cycle, chemistry…
General Circulation Models • Three dimensional model of the circulation of the atmosphere and ocean • Build on fundamental equations but approximately solved by breaking space and time into cells. • Cells are roughly 100 by 100 miles (150 by 150 Km) in size. • Many processes occurring that are not resolved with cells this big so their average effect needs to be approximated. How to do this is uncertain.
