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laurens vocab 11
chapter 11 vocab earth science
| Question | Answer |
|---|---|
| Troposphere Section 1 | The layer closest to earth surface. |
| Stratosphere | A layer in which the air temperature mainly increases with altitude an contains the ozone layer. |
| Mesosphere | Layer of earths atmosphere above the stratopause. |
| Thermosphere | Layer of earths atmosphere that is located above the mesopause; oxygen atoms absorb solar radiation causing the temperature to increase in this layer. |
| Exosphere | Outermost layer of earths atmosphere that is located above the thermosphere with no clear boundary at the top;transitional region between earths atmosphere and outer space. |
| Radiation | The transfer of thermal energy electromagnetic waves; the transfer of thermal energy from the sun to earth by radiation. |
| conduction | Is the transfer of thermal energy between objects when their atoms or molecules collide. |
| Convection | Is transfer of thermal energy by the movement of heated material from one place to another. |
| Temperature inversion Section 2 | Is a increase in temperature with height in an atmospheric layer. |
| Humidity | Is the amount of water vapor in the atmosphere at a given content of the atmosphere are relative humidity and dew point. |
| Saturation | Occurs when the amount of water vapor in volume of air has reached the maximum amount. |
| Relative humidity | The amount of water vapor in a volume of air relative t other amount of water vapor needed for that volume of air to reach saturation. |
| Dew point | Is the temperature to which air must be cooled at constant pressure to reach saturation. |
| Latent heat | The extra thermal energy contained in water vapor compared to liquid water. |
| Relative humidity | The amount of water vapor in a volume of air relative t other amount of water vapor needed for that volume of air to reach saturation. |
| Relative humidity | The amount of water vapor in a volume of air relative t other amount of water vapor needed for that volume of air to reach saturation. |
| Relative humidity | The amount of water vapor in a volume of air relative t other amount of water vapor needed for that volume of air to reach saturation. |
| Dew point | Is the temperature to which air must be cooled at constant pressure to reach saturation. |
| Dew point | Is the temperature to which air must be cooled at constant pressure to reach saturation. |
| Latent heat | The extra thermal energy contained in water vapor compared to liquid water. |
| Dew point | Is the temperature to which air must be cooled at constant pressure to reach saturation. |
| Condensation nucleus Section 3 | Is a small particle in the atmosphere around which water droplets can form. |
| Condensation nucleus Section 3 | Is a small particle in the atmosphere around which water droplets can form. |
| Orographic lifting | Occurs when an air mass is forced to rise over a topographic barrier. |
| Cumulus | Clouds are puffy, lumpy-looking clouds that usually occur below 2000 m. |
| Orographic lifting | Occurs when an air mass is forced to rise over a topographic barrier. |
| Cirrus | Often have a wispy, indistinct appearance. |
| Precipitation | All forms of water that full from clouds to the ground are. |
| Coalescence | Occurs when cloud droplets collide and join together to form a larger droplet. |