Cloud Precip Vis And Fog Flashcards
Cloud formation
Saturated air cooled to the point where moisture must be released in the form of condensation
Requires hygroscopic nuclei
Cloud layers
High cloud 20000’ to tropopause
Middle cloud 6500’ to 20000’
Low clouds SFC -6500’
Orographic lifting
Air travels up and over terrain
Causes mountain waves (multi layered cloud on windward side, lenticular or rotor cloud on leeward side)
Unstable mountain waves look stable but with embedded CB AND TS
Slow widespread ascent
Convergence of air spiralling towards centre of low p causing lifting over vast area
All cloud types are likely to be found
Mechanical lifting
Air tumbling over obstacles like buildings and terrain
Stable atmos with sufficient lifting can cause stratocumulus
unstable can cause fair weather cumulus to TS depending on instability
Convective lifting
Hot SFC warms air above causing it to rise
Can cause fair weather cumulus to TS
Water drops
Bigger than cloud drop
Form via cooling
Either freeze and stay in place of fall
Buoyancy
Tendency of air parcel to sick or rise due to temperature gradient between surrounding air
Cloud drop vs rain drop
Cloud drop 100 micrometer
Raindrops 1-2mm or larger
Cloud drops can only be virga
Look at cloud types
Look
Precipitation
Liquid or solid water from cloud to ground
Virga does not reach ground
Precipitation types
Rain
Drizzle (smaller than rain usually from low stratus cloud)
Snow
Hail frozen balls (associated with CB)
Sleet (rain and snow)
Precipitation types (continuous intermittent)
Continuous
Large widespread will not clear soon (Stratiform or nimbostratus)
Intermittent
Continuous from thin layer clouds
Showers
Passing Burt’s from cu type cloud
Light less than 1mm per hour
Mod 1-10mm per hour
Heavy more than 10mm per hour
Visibility
Km
Prevailing vis is greatest horizontal vis covering at least half of horizon
Rain intensity vis
Light same vis
Mod 3000m-10km vis
Heavy less than 3000m vis