Atmosphere Thinking Sheet 1/30/18 or 1/31/18

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Presentation transcript:

Atmosphere Thinking Sheet 1/30/18 or 1/31/18 What do you believe the word “insolation” means? (FYI: Insulation is the pink stuff you put in the walls and attic of your house…it’s a completely different word!)

Insolation Vocabulary! The amount of incoming solar radiation on the Earth Insolation Earth receives about 342 W/m2

Solar Energy

What is Solar Energy? Sunlight travels to earth as electromagnetic radiation UV VIS IR wavelength λ (μm) Emitted power (W/m2) The Sun emits mostly visible light, but also some UV (ultraviolet) and IR (infrared) light.

Heat The Earth deals with three types of heat: Radiation: waves traveling at speed of light Convection: hot material “rises” and cold material “sinks” Conduction: collisions between atoms or molecules

Solar Constant We can measure solar radiation in Watts per Meter-Squared (W/m2). Earth receives about 342 W/m2 of energy

Solar energy reflected Reflection Change in direction of radiation. Radiation leaves in one direction.

Solar energy absorbed Absorption Transfer of solar energy to a substance (like the ground or water). This process changes UV light into HEAT!

Absorption UV radiation is almost completely absorbed by Ozone (O3), O2, and N2 This protects us from harmful radiation that causes skin cancer.

Solar energy scattered Scattering Change in direction of radiation. Radiation leaves in many directions.

Role of atmosphere Objects in the atmosphere (like clouds) cause reflecting of solar energy back into space.

Role of atmosphere Particles in the atmosphere (like CO2 and H2O) absorb solar energy and hold it as heat. We call these “greenhouse gases.”

Role of atmosphere Particles in the atmosphere (like N2, O3,and O2 molecules) cause scattering of solar energy.

Solar Scattering The scattering of solar radiation in the atmosphere makes the sky look blue and the clouds look white. Equal scattering makes the sky look blue in color! Unequal scattering makes clouds look white in color!

Role of oceans Depending on the angle of the sun, oceans can reflect solar energy or absorb solar energy and hold it as heat.

Role of dry land Dry land absorbs solar energy and traps it in the form of heat. A small amount is reflected

Role of ice and glaciers Ice and glaciers reflect solar energy

Global energy balance: energy flow Source: Kiehl and Trenberth, 1997

Global energy balance: energy flow Source: Kiehl and Trenberth, 1997

Predict: What would happen if the amount of dry land on earth DECREASED?

Predict: What would happen if the amount of ice on earth INCREASED?

Predict: What would happen if the number of clouds in the atmosphere was DOUBLED?

Solar Energy Math