The line between two air masses of differing humidity and temperature. Called the dryline because the border creates a line of distinctly dry weather compared to the other side of the line
terminal velocity
velocity precipitation must reach in order to fall from the sky
collision
raindrops or snowflakes collide with each other and grow
aggregation
the growing of precipitation through collision
bergeron process
amount f water vapor in the air keeps supercooled water droplets in equilibrium, but ice grows through deposition as water droplets shrink through evaporation
warm cloud
above freezing
cool cloud
part above part below freezing
cold cloud
entirely below freezing
rimming
supercooled water droplets collide with snow
precipitation measurement tools
rain guage, snow pillow
dynamic air flow
what is happening at the top of the troposphere
mesoscale
few miles to few hundred miles
synoptic scale
few 1000 miles
cutoff low
low pressure area cut off from main storm system
zonal flow
flow is horizontal, covers multiple zones
meridonal flow
vertical flow
doppler radar
allows us to see inside the cloud
tornado recipe
strong differences in pressure over short distances
tornado alley
cold dry air from north meets warm moist air from gulf. high wind shear aloft meets storm front, mesocyclonic storm or supercell