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atsci ch 3
seasonal and daily temperature
| Question | Answer |
|---|---|
| normal sea level pressure: 14.7... | PSI |
| normal sea level pressure: 1013.25... | mb, hPa |
| normal sea level pressure: 29.92... | "Hg |
| how does atmospheric density change with height? | decreases |
| how does atmospheric pressure change with height? | decreases |
| to keep everything in balance the pressure force has to equal what? | the weight of the column above |
| what is the symbol of pressure? | P |
| P = ? | ρRT |
| PV = ? | mRT |
| why do we have seasons? | the earth's tilt |
| incoming solar radiation | insolation |
| summer solstice date | june 21 |
| at what latitude is the sun directly overhead during the summer solstice? | 23.5 degrees |
| what tropic has the sun directly overhead during the summer solstice? | tropic of cancer |
| autumnal equinox date | september 22 |
| at what latitude is the sun directly overhead during the autumnal equinox? | 0 degrees |
| winter solstice date | december 21 |
| at what latitude is the sun directly overhead during the winter solstice? | 23.5 degrees |
| what tropic has the sun directly overhead during the winter solstice? | tropic of capricorn |
| vernal equinox date | march 20 |
| at what latitude is the sun directly overhead during the vernal equinox? | 0 degrees |
| how is heat distributed from the equator to the poles? | water, hurricanes |
| what is seasonal lag? | when the highest / coldest days are later than the solstices because the incoming shortwave exceeds the outgoing IR |
| what is the diurnal cycle? | peak temperature lags after peak insolation because earth continues to warm until outgoing infrared radiation exceeds insolation |
| insolation | the amount of sunlight hitting the surface over the course of the day |
| insolation depends on | the number of daylight hours, the surface's orientation relative to the sun |
| what if the earth had no tilt? | 12 hours of daylight at all altitudes, max insolation at the equator |
| where has the record of the highest temps? | death valley, 134 F |
| what does condensation / dew formation do to temperature? | warms by latent heat release |