Online readings
Introduction to Modern Physics
Thermal Physics
Atomic + Particle Physics
Electricity and Magnetism
Energy, Matter, and radiation
Notes
Characteristics of energy, matter, radiation and heat: Introduction to chapters 3 and 4.
Laws of thermodynamics: Formal definitions of laws governing
energy and heat transfer.
Electromagnetic waves and spectrum Introduction
to electromagnetic radiation.
Radiation lawsThe dreaded mathematical formula!
Stefan-Boltzman law: Higher temperature objects will emit more radiation
Wien's law: Higher temperature objects will emit mostly higher energy, shorter-wavelength electromagnetic waves.
Simulations
Radiation law simulation:
Plots radiation intensity vs. wavelength. Set temperature to 6000 K to simulate sun . Intensity of radiation
goes way up (Stefan-Boltzman law), and peak radiation is emited in visible spectrum (Wien's law). Then set temperature down
to 300 K to simulate temperature of Earth. Intensity of emitted radiation goes way down. You will need to zoom in (+) on
intensity scale to see curve. You will then need to zoom out (-) on wavelength to see curve. Wavelength peaks in long,
infrared portion of spectrum.
Radio Wave simulation
A simulation of elctromagnetic radiation.
Move the electron up or down to create an
electromagnetic pulse. Set "Transmitter movement" at top right of window to "Oscillate" and create smooth waves.
Radiation sources: Sun and earth
The Sun
The Earth:
Everything on Earth radiates at a temperature of 230-330 K. That means it radiates away infrared radiation (IR).
Infrared photographs in at the above link show how variations in temperature lead to variations in IR intensity.
Reading satellite dataGoing through these exercises may
help you on Investigation 3A
Earth-Sun geometryReading this section will help you with Investigation 3B.
Reading maps: Latitude and longitude
Earth's orbit and solar altitude
Incoming solar radiation
Insolation at top of atmosphere
Atmospheric effects on incoming solar radiation
Insolation at surface of the earth
UV Radiation and the ozone layer
Outgoing Longwave Radiation (OLR)
The Greenhouse Effect I
The Greenhouse Effect II
The Greenhouse Effect III
Global energy balance
Permafrost and Methane
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