Meterology Flashcards
Clouds and what-not ;)
Define: Orographicn lift
Air moving up a sloping terrain, such as a moutian side, will continue upward movement especially if unstable
Define: Stratus cloud
forms in horizontal layers and usually forms as a layer of moist air is cooled below its saturation point
Does a land breeze blow at day or night?
Night, land cools and air above cools in turn, the warmer air over the water rises and cool air moves from land to sea to fill in.
The ICAO standard atsmophere is________
pressure-29.92”Hg
Tempurature-15C
Lapse rate-1.98C/1000’
Define: Occlusion
cold air mass catches up with onesself lifting the warmer sector entirely off the ground
Define: Warm front
A mass of warm air advancing on a retreating mass of cold air
List the different types of fog-5
1) Radiation-ground cooled at night, air above ground also cools, if air is moistand cooled below saturation pointfog forms
2) Advection fog-warm damp air blows over cold surface
3) Upslope fog-air cooled by expansionas moves up
4) Steam fog-cold air passes over warm water, evaporation occurs until air is saturated
5) Ice fog-extremely cold tempuratures, fuel combustion and moisture to air
In standard atsmophere the tempurature at 5000’ would be?
5*C
Define Cumuloform clouds
forms in rising air currents and are evidence of unstable air conditions
Define: Pressure altittude
The reading on the altimeter when it is set to standard barometric pressure
During a descent from 200’ AGL to the surface, you will usually find that the winds; Veer/back, increase/decrease?
Back and decrease
Define: Trowal
wedge shaped mass of air overlying an occluded front
Name the different types of high and low clouds
high: Cirrus(Ci)
Low: Alto
what are the two main forces affecting movement of upper level winds?
1) pressure gradient- forces air horizontal from an area of high to low pressure
2) Coriolis force-deflects the flow of air cuasing it to flow parrelel to isobars
* Coriolis force deflects to the right in the northern hemisphere
Define: Sublimation
heating of ice crystals changing them to invisible gas without passing through the visible water droplet stage