Weether Theory Flashcards
Atmosphere composition
78% N2
21% O2
Argon/ co2/ others
Levels of atmosphere
Troposphere 0-20000
Stratosphere 20000 - 160000
Mesosphere 160000-280000
Thermosphere 350 miles
Temperature and pressure lapse rate
Temp 2 degrees c per 1000 ft
Pressure 1 inch per 1000 ft
Coriolanus force directs air
To the right in northern hemisphere
To the left in Southern Hemisphere
Standard atmosphere
29.92 or 1013.2mb or 14.7 lb/in^2
Wind flows from
High pressure to low pressure
High pressure air rotates:
Low pressure air rotates
Clockwise away from the center
Counter clockwise toward the center
Sea breeze
Land breeze
Cool air from over water that moves over land heats up and cycles back to the water
Cool air over land that moves over water heats up and cycles back to land.
Temp inversions
Shallow smooth layers stable close to the ground. Temp increases to top of inversion. Top acts as a lid trapping weather and pollutants below. If humidity is high you can get reduced visibility in the later. Formed on cool clear nights when the ground cools the surface air faster than the rest.
How much water can the air hold
20 degrees f doubles the airs capacity.
What happens when the temp is reduced to the dew point?
The air is completely saturated and moisture begins to condense out of the air
Radiation fog
Usually formed in low lying areas like mountain valleys.
Occurs when ground cools rapidly due to terrestrial radiation and the surrounding air reaches its dew point.
< 20 ft thick it’s ground fog
Advection fog
When warm moist air moves over a cold surface. Requires wind to form up to 15kts. Common in costal areas where sea breezes can blow the air over cooler land masses.
Upslope dog
Moist stable air forced up sloping land “mountains”
Steam fog/ sea fog
Cold dry air moves over warm water water evaporates causing steam of fog