Climate Change · Part One
Climate Change 1 Syllabus
1.0 - Introduction
2.0 - The Earth's Natural Greenhouse Effect
3.0 The Greenhouse Gases
3.1 - The Role of Carbon Dioxide
3.2 - The Role of Methane
3.3 - Major Uncertainties
4.0 - CO2 Emissions
5.0 - The Earth's Carbon Reservoirs
6.0 - Carbon Cycling: Some Examples
7.0 - Climate and Weather
8.0 - Global Wind Systems
9.0 - Clouds, Storms and Climates
10.0 - Global Ocean Circulation
11.0 - El Niño and the Southern Oscillation
12.0 - Outlook for the Future
Climate Change · Part Two
Introduction to Astronomy
Life in the Universe
Glossary: Climate Change
Glossary: Life in Universe
There are several major uncertainties that come into play when considering the increase in greenhouse gases. One of these factors is the impact of the Sun’s changing brightness. The increase of greenhouse gases in the atmosphere since the industrial revolution (carbon dioxide CO2, methane CH4, nitrogen oxide N2O, various CFC’s) has had roughly the same effect as increasing the energy received from the Sun at the surface of Earth by about one percent. However, there are indications that over time periods of a century the Sun does become brighter or dimmer by 0.5% quite independently of what happens on Earth. In fact, there is evidence that the Sun’s changing brightness may have contributed to part of the warming of the last 150 years.
Another source of uncertainty is the impact of water vapor. Although the physics of the greenhouse effect are relatively simple, the response resulting from an increase in water vapor in the air complicates matters greatly. The true magnitude of global warming depends on the calculated amplification that water vapor will have on the warming, and this can be greatly moderated (or enhanced!) by changes in the formation of clouds, requiring a consideration of changes in the entire water cycle.
When all the other responses of the climate system to greenhouse warming are considered, the problem becomes enormously complex, because right away all kinds of poorly understood dynamics enter the picture: cloud formation, snowfall, precipitation patterns and soil moisture, vegetation response, and ocean circulation. The really big unknowns have to do with the possibility of strong positive feedback from threshold effects: a decrease of the ability of a warming ocean to take up heat and carbon dioxide; methane addition from permafrost regions or from the sea floor; disappearance of snow cover and sea ice (that is, a change in the albedo), and many other such possibilities. Such threshold effects are elusive because we try to suppress them in computer models, to keep the models from going into odd directions. The real Earth may not be so accommodating.
The one thing we cannot assume is that our ignorance about the Earth somehow protects us from future changes in climate. The argument that, “You cannot show conclusively that there will be substantial warming as a result of addition of greenhouse gases” can be juxtaposed by the statement, “Your calculations may well underestimate the warming which results from the addition of greenhouse gases.” In other words, any argument using uncertainty works two ways. Uncertainty does not relieve us from the need to look ahead and to pretend otherwise is foolish.
The reason these seemingly obvious points are stressed here is that the “average” global warming skeptic typically forgets to consider that uncertainty does not mean that nothing is happening. Human-induced warming may be either less important or more important than suggested by our calculations. But only by reducing this uncertainty in our calculations will we learn the answer (not by arguing endlessly back and forth).