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Learning about Climate

  1. What is the difference between weather and climate?
  2. What factors determine the climate?
  3. How does climate affect vegetation?
  4. How can local climates vary over very short distances?
  5. What is a climate proxy?
  6. How do scientists use ice cores to determine past climates?
  7. What are the causes of climate change?

What are the causes of climate change?

Diagarm showing how air moves on Earth

© NASA

Air moving from a high pressure zone around the poles to lower pressures at the equator would move in a straight line if there were no rotation. But because of the rotation, the air moves to the right of its straight path as it moves equatorward.

Two important things determine the Earth's climate. One is the amount of heat the sun delivers to the Earth. Also important is where the Earth's continents are located relative to the equator. Continental ice sheets cannot develop unless one or more continents are located at high latitudes.

The Earth revolves around the sun once a year. The orbit is almost a circle. If the Earth were the only planet, its orbit around the sun would be almost unchanging. The other planets exert a pull on the Earth. Although the pull is small, it makes the Earth's orbit much more complicated. The orbit changes slightly in several different ways. The changes occur over periods that range from about twenty thousand years to about a hundred thousand years. These changes cause slight differences in how much of the sun's heat the Earth receives, in winter vs. summer and at high latitudes vs. low latitudes.

The astronomical theory of the ice ages holds that the small changes in the Earth's orbit trigger the advance and retreat of ice sheets. Most scientists now accept this theory. The details of how the changes trigger the ice sheets are still only partly understood. For example, the very fast melting of the ice sheets, compared to the long times needed for them to form, is still a mystery.

The astronomical theory is only part of the story. Climate is known to change on time scales as short as centuries, and the cause (or causes) of these changes are still not clear. Here's a big question, and an important one. Has the increase in temperature since the beginning of the twentieth century been caused by human activity, or is it just another natural upward "spike" like several during the past two millennia? Most climatologists think that the upward trend in temperature during the twentieth century is at least partly caused by human activity.

Windmills in California collect wind energy.

© Michael Collier

This view of windmills in the Tehachapi, California area shows one of the world's leading wind energy producers. They offset 1.1 billion pounds of greenhouse gases each year.

Several gases in the Earth's atmosphere are called greenhouse gases. The most important is water vapor, but carbon dioxide is important also. Carbon dioxide has always been part of the Earth's atmosphere, but it has been increasing more and more rapidly in recent times. Coal, oil, and natural gas are called fossil fuels, because they come from plant and animal material that was buried in the Earth's sediments. When they are burned, they add carbon dioxide gas to the atmosphere. Along with the other greenhouse gases, carbon dioxide absorbs some of the heat that the Earth's surface sends out to space, and then sends it back to the surface. That increases the Earth's average surface temperature. The effect is the same as with the glass of a greenhouse, although the process itself is not exactly the same.

Several groups of climatologists have been developing computer models of the Earth's climate. They try to build in all of the important processes of climate into the model. Then they start the model with the present climate and let it run to see what the future climate will be. The models are not perfect, because it is very difficult to build in some of the most important influences on climate. The behavior of clouds is especially tricky to model. The models have one thing in common, though. They predict that the Earth's surface temperature is likely to increase by as much as two degrees Celsius between 2000 and 2050 if the increase in atmospheric carbon dioxide continues. A rise of two degrees would make the Earth's temperature much warmer than during even the warmest periods in human history.

If the predictions about global warming come true, many things about the Earth's climate, aside from just temperature, are likely to change. Some regions will get more rainfall, and other regions will get less. The frequency and strength of severe storms are likely to increase. As the world's glaciers continue to melt, sea level around the world will rise, by as much as half a meter to a meter. That might sound like a lot to you, but think of the flooding that it would cause in coastal cities around the world! Will the predictions of the computer models come true? That is likely, although not certain. All that science can do is try to make likely predictions. How to act upon the predictions is for human society to decide.

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Fossil of the skull of a saber-toothed cat, an extinct mammal that lived in the Pleistocene epoch. Albert Copley © Oklahoma University; Image Courtesy of the Earth Science World Image Bank.  Photo ID: hn81e5

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Last updated:July 23, 2008


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