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Ocean Surface Topography from Space
OVERVIEW
Climate

Climate is the long-term state of the atmosphere at a particular location--in a sense, the "average weather" over a long period of time. Climate varies significantly around the globe, and not randomly.

At the end of the last ice age, about 12,000 years ago, glaciers covered much of Europe and North America. Fed by ocean waters, the polar ice caps thickened and expanded, causing global sea level to drop far below its current level. Still recovering from the Ice Age, the Earth is about 5°C (9° F) warmer today than it was then, and global sea level continues to rise. The past century alone has seen global temperature increase by 0.6° C (1° F), and the average global sea level over the past decade has risen steadily. Is this the result of Global Warming or Global Climate Change?

Here is what we know about the Earth's climate:

  • At the poles, it's bitterly cold--below freezing all the time, and very dry.
  • At the equator (at sea level), it's always hot and usually rainy, but it never freezes.
  • At mid latitudes, climates are in between these two extremes --temperate--but
    • Climates on the east coasts of continents are wet, with cold winters and hot summers,
    • Climates on the interior parts of continents are dry, with even colder winters and hotter summers,
    • And climates on continental west coasts are mild, with rainy winters and dry summers.
United States Map featuring San Francisco CA Wichita KS and Norfolk VA

How do we account for these phenomena? Several factors are of paramount importance:

  • The spherical shape of the Earth,
  • The movement of Earth through space,
  • The physical properties of water,
  • The physical properties of air,
  • And the configuration of the oceans and continents.

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