The Physical Environment

                                                       
Contents | Glossary | Atlas |  Index | TPE Daily News | Blog | Podcast | Google Earth | Search

 Earth System

System regulation

Most systems tend toward a state of equilibrium where system inputs are balanced by system outputs. Though natural systems change over long periods of time, on the scale of a human lifetime they appear to be static. In reality, the state of natural systems oscillates around a mean condition a state known as dynamic equilibrium. For instance, the abundance and type of animal species in an ecosystem may fluctuate over a time, but the overall diversity remains constant. The Earth's atmospheric temperature has remained fairly constant through long periods of Earth history, even though at shorter time intervals, geologically speaking, the temperature has risen or fallen. If one or more controlling variables (climate, vegetation, soil, man) imposes a long-term stress to the system it will seek to establish a new state. A steady-state equilibrium is reached when the rates of system inputs and outputs are equal, and the amount of material stored in the system is constant over time.

Steady State Equilibrium

Figure 2.27 System equilibrium over time.

The state of the system is a result of feedback mechanisms between system components.

Previous |Continue  


  

 

Contents |Glossary | Atlas Index  |  Blog | Podcast | Google Earth | Search Updates | Top of page

About TPE | Who's Used TPE |  Earth Online

Please contact the author for inquiries, permissions, corrections or other feedback.

For Citation: Ritter, Michael E. The Physical Environment: an Introduction to Physical Geography.
Date visited.  http://www.uwsp.edu/geo/faculty/ritter/geog101/textbook/title_page.html

©2003 - 2011
Michael Ritter (tpeauthor@mac.com)
Last revised 10/1/09