Causal Loop Diagrams Causal loop diagrams can be very helpful for explaining the mechanism behind feedback loops and identifying whether the feedback loop.

Slides:



Advertisements
Similar presentations
Causal Loop Diagrams.
Advertisements

Causal Loop Diagrams. Exponential growth of a bank account. The two positive connections between Bank balance and interest added for a positive feedback.
Causal Loop Diagrams. Home Heating Air Resistance.
Homeostasis Walter Cannon 1932 The Wisdom of the Body Jame Lovelock ~1969 Gaia hypothesis (Lovelock, J.E.; Margulis, L. (1974). "Atmospheric homeostasis.
1 MET 112 Global Climate Change MET 112 Global Climate Change - Climate Feedbacks Professor Menglin Jin San Jose State University Outline Stability/instability.
Lecture 8 Climate Feedback Processes GEU Forcing, Response, and Sensitivity Consider a climate forcing (e.g., a change in TOA net radiation balance,
Climate Forcing, Sensitivity and Feedback Processes.
Buffers and Feedback Loops Class Notes 1:6. Buffers and Feedback Loops Buffers are agents or regulatory mechanisms that reduce or minimize fluctuations.
MET 112 Global Climate Change
22.2 Solar Energy and the Atmosphere. What happens to incoming solar radiation? 1.Scattered 2.Reflected 3.Absorbed.
Climate Forcing, Sensitivity and Feedback Processes.
Climate Forcing and Physical Climate Responses Theory of Climate Climate Change (continued)
1 MET 112 Global Climate Change MET 112 Global Climate Change - Climate Feedbacks Professor Menglin Jin San Jose State University Outline  Stability/instability.
EOSC 112: THE FLUID EARTH EARTH’S ENERGY BUDGET AND CLIMATE FEEDBACKS E3 Read: Kump et al. Chap.3, p. 44 (Atm. Comp.), p Check: Key Terms, Review.
PTYS 214 – Spring 2011  Homework #5 available for download at the class website DUE Thursday, Feb. 24  Reminder: Extra Credit Presentations (up to 10pts)
MET 112 Global Climate Change - Lecture 8 Climate Feedbacks Dr. Craig Clements San Jose State University.
MET 112 Global Climate Change - Lecture 8 Climate Feedbacks Dr. Craig Clements San Jose State University 14 October 2008.
1 MET 112 Global Climate Change MET 112 Global Climate Change - Lecture 2 The Earth’s Energy Balance Dr. Craig Clements San José State University Outline.
Evaluation II – The Atmosphere Feedback describes the situation when output from (or information about the result of) an event or phenomenon in the past.
Generalized diagram of the Earth system
EOSC 112: THE FLUID EARTH INTRODUCTION TO EARTH SYSTEMS - SIMPLE CLIMATE SYSTEMS Sys12 Read: Kump et al. Chap.2, p , 26 Check: Key Terms, Rev. Questions,
1 BAESI - Global Warming: Food Climate Connections The Greenhouse Effect Dr. Eugene Cordero San Jose State University Outline  Greenhouse effect  Energy.
GREENHOUSE EFFECT Climate Change. Greenhouse Effect Is a natural process that permits the Earth to retain some of the heat from the sun. Gases in the.
The Greenhouse Effect CLIM 101 // Fall 2012 George Mason University 13 Sep 2012.
Essential Principles Challenge
Climate Forcing Some Basic concepts of Heat, Temperature, Feedbacks, and the idea of a “forcing”
MET 12 Global Climate Change - Lecture 5
CH 24.3 Solar Radiation, Pressure, & Wind. Earth’s Energy Balance Input = Sun’s Energy = (Visible light + some UV) REFLECTED: ~ 25 % by clouds, dust,
1 MET 112 Global Climate Change MET 112 Global Climate Change - Lecture 2 The Earth’s Energy Balance Dr. Eugene Cordero San Jose State University Outline.
1 Met 10 Weather Processes Jeff Gawrych Temperature, Heat Transfer and Earth’s Energy Balance.
Global Climate Change: The Evidence Presentation by: Rosa Jaime.
Climate Change UNIT 3 Chapter 7: Earth’s Climate System
Feedback Loops. FEEDBACK LOOPS Change induces change What happens when you’re hot? What happens when you’re cold? These are examples of negative feedback.
The Greenhouse Effect. What controls climate? Energy from the Sun – Radiation! Consider the 4 inner planets of the solar system: SUN 342 W m W.
Atmospheric Heating.
CH 10 Section 2 Notes Forces - Terminal Velocity Objectives: By the end of this presentation, you should be able to: Describe and explain what is meant.
Drag force Terminal velocity.  We’re always “neglecting air resistance” in physics ◦ Can be difficult to deal with  However air resistance is present.
Radiation balance Any object in the Universe which has a temperature above the temperature "absolute zero" ( degrees Fahrenheit or degrees.
The Atmosphere: Energy Transfer & Properties Weather Unit Science 10.
Conversations with the Earth Tom Burbine
Energy Balance Game Simulation Environment From K. Trenberth, J. Fasullo, and J. Kiehl, EARTH’S GLOBAL ENERGY BUDGET BAMS 2009.
Sun Controls Earth’s Climate System Earth has a global climate system that includes air, land, liquid water, ice, and living things.climate system The.
1 Standards: S6E4b. Relate unequal heating of land and water surfaces to form large global wind systems and weather events such as tornados and thunderstorms.
Cloud-Aerosol-climate feedback
Energy Flows and feedback processes: A systems perspective.
1 MET 112 Global Climate Change MET 112 Global Climate Change - Lecture 3 The Earth’s Energy Balance Dr. Eugene Cordero San Jose State University Outline.
Global Change: Class Exercise Global Energy Balance & Planetary Temperature Mteor/Agron/Envsci/Envst 404/504.
Earth and Space Science TEK 14 a 14) Fluid Earth. The student knows that Earth’s global ocean stores solar energy and is a major driving force for weather.
Energy Flows and feedback processes: A systems perspective.
Temperature, Air Pressure and Wind
Do Now! #2 Draw the water cycle. Draw the water cycle. Describe the following terms: Describe the following terms: Evaporation: Evaporation: Condensation:
1 MET 112 Global Climate Change MET 112 Global Climate Change - Lecture 7 Climate Feedbacks Dr. Eugene Cordero San Jose State University Outline  Stability/instability.
ENERGY IN ECOSYSTEMS Chapter The sun is the source of all energy for the earth and its ecosystems. What happens to the suns energy? What is it used.
1 MET 112 Global Climate Change MET 112 Global Climate Change - Lecture 5 Clouds and the Earth’s energy budget Dr. Eugene Cordero San Jose State University.
Energy Flows and feedback processes: A systems perspective
Introduction To Weather Dynamics
Climate feedbacks: Water vapor, snow/ice albedo, and clouds
Energy flows and feedback processes: A systems perspective
BAESI - Global Warming: Food Climate Connections
How the Greenhouse Effect Works/Feedback factors
Appendix 1 Water vapor feedback
Natural Environments: The Atmosphere
What controls climate? Energy from the Sun – Radiation
GLOBAL ENERGY BUDGET - 2 The Greenhouse Effect.
Global Change: Class Exercise
Climate Change – Causes and Impacts
Climate Earth’s Energy Budget.
3. Local winds and global winds are generally a result of which of the following? A). Earth’s tilted axis. B). Unpredictable changes in the atmosphere.
Global Change: Class Exercise
Global Change: Class Exercise
Presentation transcript:

Causal Loop Diagrams Causal loop diagrams can be very helpful for explaining the mechanism behind feedback loops and identifying whether the feedback loop structure is a positive or negative feedback loop.

Earth’s Energy Balance is used here to develop and explain causal loop diagrams.

Connections (+ or - ??)* Absorbed SunlightEarth’s Mean Temperature Emitted Infrared Earth’s Mean Temperature Cloud Cover Earth’s Mean Temperature Volcanic aerosol Earth’s Mean Temperature CO2 use nouns * A connection is positive if when the first increases the second also increases, and a connection is negative (opposite) if when the first increases the second decreases Earth’s Mean Temperature Water Vapor Planetary albedoEarth’s Mean Temperature

Connections (+ or - ??) Absorbed SunlightEarth’s Mean Temperature Emitted Infrared Earth’s Mean Temperature Cloud Cover* Earth’s Mean Temperature Volcanic aerosol Earth’s Mean Temperature CO2 use nouns * The effect of cloud cover is complicated because they reduce sunlight be day but provide warming at night. High thin ciro stratus clouds also influence the Earth system differently than low thick stratus clouds. Earth’s Mean Temperature Water Vapor Planetary albedoEarth’s Mean Temperature or

Example Draw a causal loop diagram to describe the following: The sun becomes brighter causing Earth to warm. As the Earth warms it gives off more longwave radiation until it settles into a new equilibrium temperature.

Answer Draw a causal loop diagram to describe the following: The sun becomes brighter causing Earth to warm to a new equilibrium temperature. sunlight Earth’s mean Temperature Emitted infrared energy Notice that the sun is not within the feedback loop structure. This negative feedback loop is always present in the Earth System and helps limit the runaway effects of positive feedback processes.

Ice albedo feedbck process Draw a causal loop diagram capturing the essence of the feedback process decribed below. As Earth’s temperature increases from an increase in solar output there will be less snow and ice cover globally. This decreases the planetary albedo causing even more sunlight to be absorbed by the climate system resulting in amplified warming.

What are the polarities of each connection?

What are the polarities of each connection? What is the sign of this feedback loop?

What is the sign of this feedback loop?

Air Resistance

Connections (+ or - ??) Size (area) of carAir resistance force Air temperature Air resistance force Speed of car Remember use nouns Air resistance force

Connections (+ or - ??) Size (area) of carAir resistance force Air temperature Air resistance force** Speed of car Remember use nouns **Warmer air is thinner air Air resistance force + + -

weight Air resistance Net downward Force

Connections (+ or - ??) Size of parachuetAir resistance force AltitudeAir resistance force Jumper’s speed Remember use nouns Air resistance force

Connections (+ or - ??) Size of parachuetAir resistance force AltitudeAir resistance force Jumper’s speed Remember use nouns Air resistance force Note: our text uses For an opposite connection o

Draw a causal loop diagram to describe the following: As the sky diver falls she travels faster and faster until reaching a terminal velocity. Include diver’s speed, air resistance, weight, and net downward force in your diagram.

Whenever the number of negative (opposite) connection is odd The loop is a negative feedback loop.