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Systems Theory Explained

  Intro to Physical Geography
            Chapter 1
Systems Theory
• Systems are any ordered, interrelated set of
  things and their attributes, linked by flows of
  energy and matter, as distinct from the
  surrounding environment outside the system.

• Open systems
• Closed systems
Open System
Open System
Feedback
• Systems generate information as they operate
  that influence their own operations (feedback
  loops).
• If feedback info discourages a response, it’s
  negative feedback, and can decrease growth.
• If feedback info encourages increased
  response, it is positive feedback, and can
  stimulate growth.
System Equilibrium
• Most of the time a system will maintain its
  structure…you’ll see this especially as we start
  talking about the atmosphere.
• Steady-state equilibrium-rates of inputs and
  outputs are equal and energy storage is
  constant.
• Dynamic equilibrium-changing trend over
  time, often gradually.
Steady-State Equilibrium
Dynamic Equilibrium
The Tipping Point
• A system can reach a threshold if too many
  pressures are put upon it.
• An abrupt change occurs in the system, and the
  system reaches what’s called a metastable
  equilibrium.

• Examples: Huge iceberg broke of Greenland in
  August of 2010.
  Earthquakes!
Systems in the Abstract
Examples
of Systems
Systems Theory Explained

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Systems Theory Explained

  • 1. Systems Theory Explained Intro to Physical Geography Chapter 1
  • 2. Systems Theory • Systems are any ordered, interrelated set of things and their attributes, linked by flows of energy and matter, as distinct from the surrounding environment outside the system. • Open systems • Closed systems
  • 5. Feedback • Systems generate information as they operate that influence their own operations (feedback loops). • If feedback info discourages a response, it’s negative feedback, and can decrease growth. • If feedback info encourages increased response, it is positive feedback, and can stimulate growth.
  • 6. System Equilibrium • Most of the time a system will maintain its structure…you’ll see this especially as we start talking about the atmosphere. • Steady-state equilibrium-rates of inputs and outputs are equal and energy storage is constant. • Dynamic equilibrium-changing trend over time, often gradually.
  • 9. The Tipping Point • A system can reach a threshold if too many pressures are put upon it. • An abrupt change occurs in the system, and the system reaches what’s called a metastable equilibrium. • Examples: Huge iceberg broke of Greenland in August of 2010. Earthquakes!
  • 10. Systems in the Abstract

Editor's Notes

  1. We use this as an analytical tool.Open systems are not contained, as in nature. Inputs of energy and matter flow into the system, and outputs of energy and matter flow from the system. Our Earth is an open system in terms of energy because solar energy enters freely and heat energy leaves.Closed systems-is self-contained. The Earth is a closed system in that we have a finite amount of physical matter and resources. There is only so much air, water, and material resources.
  2. Inputs of energy and matter undergo conversions and are stored as the system operates. Outputs include energy and matter and heat energy that flow from the system.
  3. A natural open system-In photosynthesis plants use light, water, CO2 and nutrients, and produce oxygen, and carbohydrates to store energy, and outputs water and oxygen.Plant respiration reverses the process and expends CO2 and water, and uses oxygen to consume the stored carbohydrates.Other ideas of open systems?
  4. Negative feedback-bad movies-bad reviews, less people go!Think about how much easier it can be to continue working out after you’ve been doing it for awhile and are seeing results for positive feedback.
  5. Systems don’t want to change. They want to maintain balance
  6. It is the size of Manhattan!
  7. Three abiotic spheres make up the Earth’s environment.