Basic Cloud formation
1 ) Air rises (contains water vapour & condensation nuclei)
2 ) Air parcel cools to dew point - Saturation
Convection
1 ) ELR allows warm air to rise
2 ) Dew point temp reached (called condensation level)
Orographic Uplift
1 ) Humid / moist air evaporates
2 ) Wind pushes moist air up mountain
3 ) Expands & cools (hits dew point)
Frontal Uplift
1) Cold & warm air meet
2 ) Heavier cold air stays at surface forcing lighter warm air to rise over it
Convergence Uplift
1 ) 2 airstreams meet head on - both move up
2 ) Slow widespread ascent
3 ) Occurs in Low Pressure system
Turbulence
1 ) Causes friction with surface
2 ) Cloud between condensation & top of turbulent layer -
3 ) Continually forming (rising air expanding- cooling) & dissipating (sinking air compresses- warms)
4 ) Forms mostly over land (land friction)
5 ) Often dissipates at sunset
Latitude heating of cold air mass
1 ) Air moves closer to equator over warmer land mass (changing latitudes -> not solar heating)
2 ) Low level air mass heats while higher air remains cold
3 ) Vigorous convection occurs -> air mass becomes unstable
4 ) Occurs night or day (changing latitudes = temp change
5 ) The faster the air mass moves over surface = greater temp difference between top & bottom layers
6 ) Air becomes increasingly unstable -> CU develops
Then TS
Can occur over land or sea -> day or night
Wishing the cld how do rain drops form ?
1 ) Tiny droplets form & grow within cld
(not heavy enough to fall yet)
2 ) Strong updrafts keep droplets in cloud -> droplets build
3 ) droplets weight increases faster then surface area
= Heavier -> need strong winds to keep in cld