explore • inspire • engage
The Warmer the Object, the More Heat Emitted Objects above absolute zero emit EM radiation (usually IR) Stefan-Boltzmann Law tells how much energy emitted
Stefan-Boltzmann Law in LSOP Activity
Stefan-Boltzmann Law in LSOP Activity
Modeling Planetary Energy Balance Calculate theoretical temperature of a planet with some simple math Discover that Earth would be frozen without the greenhouse effect Science Topics Blackbody Radiator and the Stefan-Boltzman Law Conservation of Energy (Energy In = Energy Out) Albedo
Let’s add some atmosphere… How will this change the behavior of our model?
LSOP Model - Atmosphere
Turn 1 – Radiate Phase
Turn 1 – Absorb Phase
Change – Initial State to Turn 1
Net Energy Budget: Energy In – Energy Out
Change from Initial State to Turn 1 Energy In – Energy Out = 3 – 1 = +2 +2 -1 +1
Turn 1 – Radiate, then Absorb
Turn 2 – Radiate, then Absorb
Turn 3 – Radiate, then Absorb
Graph of Spinup to Equilibrium
What is “wrong” with this model?
Turn 4 – Radiate, then Absorb
Turn 5 – Radiate, then Absorb
Net Energy Budget?
Net Change After 2 Turns of Night
Spinup to Dynamic Equilibrium
Show Movies Model Spinup Equilibrium Spinup – with day/night cycle Dynamic Equilibrium
LSOP Model – No Atmosphere
Turn 1 – Radiate Phase
Turn 1 – Absorb Phase
Turn 2 – Radiate Phase
Turn 2 – Absorb Phase
Turn 3 – Radiate Phase
Turn 3 – Absorb Phase
Turn 4 – Radiate Phase
Turn 4 – Absorb Phase
Graph of “data” from model run “experiment”
Turn 4 – Radiate Phase - Night
Turn 4 – Absorb Phase - Night
No Atmosphere Spinup to Equilibrium