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IES Exam 1 Lecture 4
Earth's Energy Budget and Temperature Pt. 1
| Term | Definition |
|---|---|
| Shortwave Energy Origin | Sun Atmosphere downwards |
| Longwave Energy Origin | Emitted by Earth and Earth temperature objects Goes off in upward direction |
| Longwave Absorption | Atmosphere is good at absorbing it and radiating it back down to the surface |
| Heat Budget | Energy moving around w/in Earth System |
| emission | Converts Heat energy to EMR |
| Absorption | Converts EMR to heat energy |
| Transmission | Movement of EMR through object w/out changing the subject |
| Water Albedo | Angle dependent 10-60% |
| Snow and Ice Albedo | 80-95% |
| High Angle Water Albedo | High absorption, low albedo |
| Low Angle Water Albedo | High reflectivity, high albedo |
| Direct Radiation | Straight path of radiation from Sun to surface |
| Diffuse Radiation | Light is scattered through atmosphere as it comes down |
| Rayleigh Scattering | Short wavelengths scatter more easily than long |
| Atmospheric Shielding | Due to scattering Dangerous short wavelengths are scattered out to space before making it in |
| Greenhouse Effect | Atmosphere is mostly transparent to visible light and mostly absorptive of infrared EMR Some emitted out, but mostly creates cycle |
| Greenhouse Effect and Earth | Warms Earth to make it habitable (warms ~34 degrees C) |
| Major Atmospheric Components and Greenhouse Effect | DON'T interact w/infrared or contribute to greenhouse effect |
| Trace Gases and Greenhouse Effect | DO contribute |
| Trace Gases Molecules | Polar |
| Polar Molecules and Greenhouse Effect | Polar molecules bind to incoming infrared photons Move faster, generate EM field Absorb passing EMR Raises temperature |
| Atmospheric Absorption | Each gas has its own selective absorption of particular wavelengths Each wavelength is absorbed differently |
| Water Vapor | Primary absorber of CO2 |
| Clouds | Reflect incoming sunlight and trap outgoing longwave radiation |
| High Clouds | Warm the Earth |
| High Cloud Characteristics | Wispy, low albedo Absorbs infrared and holds onto it, since they're colder |
| Low Clouds | Cool the Earth |
| Low Cloud Characteristics | White, puffy Dense and high albedo Absorb energy but they're warm so they radiate it back |
| Net Effect of Clouds | Depends on height, temp, droplet size, density, structure |
| Aerosols Direct Effect | Absorb and scatter shortwave radiation Warms atmosphere Cools surface |
| Aerosols Indirect Effect | Nucleation sites for water droplets -> cloud formation |