Ppl Checkride Flashcards
General characteristics of airflow, high as low pressure system.
Low pressure - inward, upward, counterclockwise
High pressure - outward, downward, and clockwise
What are the standard pressure and temp for sea level?
15°C and 29.92” (inches of Mercury) or 59°F 1013.25 hPa (hectopascal)
What are isobars
Isobars are a line on a weather chart which connects areas of equal or constant barometric pressure
if the isobars are relatively close together on a Surface weather chart or a constant pressure chart what information will this provide
Closely spaced isobarsindicate large pressure changes over a small area and suggest strengtheningwinds.Widely spaced isobarsportray a “flat” or weak pressure gradient typical of light-windsituations.
What causes the winds aloft to flow parallel to the isobars
Coriolis force
At what rate does atmospheric pressure decrease with an increase in altitude
1”Hg per 1000’
What does “dew point” mean
Dew point is the temperature to which a sample of air must be cooled to obtain the state of saturation.
List the effects of stable and unstable air on clouds, turbulence, precipitation and visibility.
Clouds: Stable= Stratiform, unstable=Cumuliform
Turbulence: Stable=smooth, Unstable=Rough
Precipitation: Stable=steady, Unstable=Showery
Visibility: Visibility=Fair to poor, Unstable=Good
When significant precipitation is occurring at the surface how thick can you expect the clouds to be
Usually requires clouds to be at least four thousand feet thick. the heavier the precipitation the thicker the clouds are likely to be
During your PreFlight planning what type of meteorology information should you be aware of with respect to icing
Location of fronts
Cloud layers
Freezing levels
Air temperature and pressure
What conditions are necessary for structural icing to occur
Visible moisture and below freezing temperatures at the point moisture strikes the aircraft
Name the main types of icing and aircraft May encounter in flight
Structural, induction system, instrument icing
Name the three types of structural icing that may occur in flight
Clear ice -forms after initial impact with the remaining liquid portion of the drop flows over the aircraft surface, gradually freezing as a smooth sheet of solid ice.
Rime ice - forms when crops are small, such as those in stratified clouds or light drizzle. The liquid portion remaining after initial impact freezes rapidly before the drop has time to spread out over the aircraft system.
Mixed ice- forms when Trump’s vary in size or when liquid drops are intermingled with snow or ice particles. The ice particles become embedded in clear ice, building a very rough accumulation.
What action is recommended if you inadvertently encounter icing conditions?
Leave the area of visible moisture descend to an altitude below the cloud bases, climb to an altitude above the cloud tops, or turn to a different course.
Is Frost considered to be hazardous to flight? Why?
Yes because well Frost does not change the basic aerodynamic shape of the wing, the roughness of its surface spoils the smooth flow of air, thus causing a slowing of airflow. This slowing of the air causes early air flow separation, resulting in a loss of lift. Even a small amount of frost on airfoil May prevent an aircraft from becoming airborne at normal takeoff speed. It is also possible that, once airborne, an aircraft could have insufficient margin of AirSpeed above stall so that the moderate gusts of turning flight could produce incipient or complete stalling.
What factors must be present for a thunderstorm to form?
Sufficient water vapor or moisture
An unstable lapse rate or unstable air
An initial upward boost or uplifting air
What are the three stages of a thunderstorm
Cumulus stage of updrafts cause raindrops increase in size
Mature stage rain at Earth’s surface, it falls through or immediately besides the updrafts, lightning, perhaps roll clouds
Dissipating stage downdrafts and rain began to dissipate
What is a temperature inversion
An inversion is an increase in temperature with height a reversal of the normal decrease with height. A ground-based inversion favors poor visibility by trapping fog, smoke, and other restrictions in to low levels of the atmosphere. The air is stable, with little or no turbulence.
Two basic ways that fog me form
Cooling air to the dew point
Adding moisture to the air near the ground