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Meteorology
| Question | Answer |
|---|---|
| What are the characteristics of a CIRRUS cloud? | High Clouds (20,000ft); Sometimes appear as hooked filaments called “mares’ tails” |
| What are the characteristics of a CIRROSTRATUS cloud? | High Clouds; thin sheet of white; ice crystal clouds give sky a milky look; Produces halo around sun and moon |
| What are the characteristics of a CIRROCUMULUS cloud? | Lowest of the high clouds with a “mackerel” look ( similar to fish scales) |
| What are the characteristics of a ALTOCUMULUS cloud? | middle cloud 6,500-20,000ft; “sheepback” cloud; white to gray |
| What are the characteristics of a ALTOSTRATUS cloud? | middle cloud 6,500-20,000ft; Stratified veil of clouds that produces light precipitation; When thin, sun or moon may produce a light spot, but no halos are produced. |
| What are the characteristics of a STRATUS cloud? | Low clouds 6500ft; Low uniform layer resembling fog but not resting on the ground; May produce drizzle |
| What are the characteristics of a STRATOCUMULUS cloud? | Low clouds 6500ft; Soft, gray clouds in globular patches or roles; Rolls may join together to make a continuous cloud |
| What are the characteristics of a NIMBOSTRATUS cloud? | Low clouds 6500ft; Amorphous layer of dark gray clouds; One of the chief precipitation producing clouds ********** |
| What are the characteristics of a CUMULUS cloud? | Clouds of Vertical Development (Unstable); Dense, billowy often characterized by flat bases; May occur as isolated clouds or closely packed |
| What are the characteristics of a CUMULONIMBUS cloud? | Clouds of Vertical Development (Unstable); Towering cloud, sometimes spreading out on top to form an anvil head. Associated with heavy rainfall/thunder/lightning/hail/tornadoes ************ |
| Why are high clouds always thin in comparison to low and middle clouds? | High Clouds: low temp & small quantity of water vapor makes clouds thin, white, and made primarily of ice crystals; Low & Middle Clouds: because composed primarily of water droplets, cells are more distinct |
| Latent Heat | Situation in which it doesn’t produce a temperature change until a given point (ice in water stays the same temp until the ice is fully melted); Heat is hidden! |
| Heat Transfer (Water) | 1 calorie (heat measurement) is needed to raise the temperature of 1 gram of water by 1 degree Celsius |
| Latent Heat of Melting | Requires 80 calories to melt 1gram of ice |
| Latent Heat of Fusion | When freezing, 80 calories are release for every 1gram |
| Adiabatic temperature changes | Temperature changes in which heat was neither added or subtracted. They result when air is compressed or allowed to expand; When air is allowed to expand it cools; When air is compressed it warms; No heat is transferred in/out of a parcel (body of air) |
| How does Lake breeze develop? | As air over land is warmed, the air expands & becomes less dense; produces a decrease in surface pressure over land; the pressure over water remains nearly constant; pressure gradient between land & water causes air over shoreline to move inland |
| Cold & Warm / Pressure | Cold (dense) – higher pressure; Warm (less dense) – lower pressure |