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Earth as a System
The first time people got a glimpse of the whole Earth was December 1968. Apollo 8 astronauts took pictures of the Earth as they traveled to and from the Moon. In their photographs, the Earth looks like a small blue and white marble in a sea of black space. Looking at the planet from that far away makes it easy to see that all its parts – the living things, the air, the water, the ice, and the rocks - are connected. Everything on Earth is in the same boat floating through space - a system.
Since the 1980s, NASA scientists have been studying the Earth as they study other planets – mainly from above with satellites. Based on this way of looking at Earth, they developed the idea of Earth system science.
“From space we can view the Earth as a whole system, observe the net results of complex interactions, and begin to understand how the planet is changing in response to natural and human influences,” NASA explained in a 2003 report.
There are five parts of the Earth system. Each part has its own collection of materials and processes. However, the parts of the Earth system do not operate on their own. They all interact with other parts in many ways.
- The atmosphere extends up from the Earth surface for several hundred kilometers. The lowest part is home to clouds and weather.
- The biosphere is all living things, from single-celled bacteria to plants and animals.
- The geosphere includes all minerals, rocks, molten rock, sediments, and soils (although there are important living components to soils as well).
- The hydrosphere includes the ocean, rivers, lakes, streams, groundwater, water vapor, and even puddles.
- The cryosphere is the frozen part of the Earth system and includes snow, glaciers, and sea ice.
The Sun has a large impact on the Earth and so it is also considered a part of the Earth system. Almost all the energy on Earth comes from the Sun. The factors outside the planet, like the Sun and solar system, which have an impact on the Earth system, are sometimes called the Exosphere.
