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109 Cards in this Set

  • Front
  • Back

Crosswind calculation

Wind speed x Sin (angle)

Headwind calculation

Wind speed x Cos (angle)

Crosswind rule of thumb

15 degrees 1/4


30 degrees 1/2


45 degrees 3/4


Over 60 degrees same

Aqua planning formula

Speed = 9 x square root of PSI

Calibrated airspeed (CAS)

IAS adjusted for pitot system position and installation error

Equivalent airspeed (EAS)

CAS adjusted for compressibility effects

True airspeed (TAS)

EAS adjusted for air density

TC-TWO

Threats


Charts


Terrain


Weather


Operational

Engine pressure ratio

Intake air pressure VS outlet pressure

Newton's third law

For every force acting on a body there is an equal and opposite force

Gas turbine cycle referred to as

Brayton cycle

Convergent ducts

Increase velocity, decrease pressure and temp

Divergent ducts

Decrease velocity, increase pressure and temp

One stage of an axial flow compressor

A rotor blad and a stator vane

Blade creep

Turbine blades get longer over time due to high temp and centrifugal force

Turbine performance depends on

RPM


airspeed


Altitude


Density


Temperature

Subsonic flow

Convergent increase V, decrease P


Divergent decrease V, increase P



Density remains the same

Supersonic flow

Convergent decrease V, increase P, increase D


Divergent increase V, decrease P, decrease D

LSS formula

39x square root temp (kelvin)

Mach number formula

TAS/LSS

Mach tuck

The C of P moving rearward generating a nose pitch down moment

Airframe design to prevent shockwaves

Wing taper


Aspect ratio


Sweep back


Fuselage area ruling

Lift formula

CL 1/2 pV2 S


CL coefficient of lift


P (rho) value of air density


V velocity of airflow over wing


S surface area of the wing

Types of drag

Parasite drag


Induced drag

M crit

The lowest mach number at which the airflow over some point on the a/c reaches the speed of sound

ILS localiser scale

2.5° full left or right


Ie. 5 °full sweep

ILS glide slope scale

0.35° up or down


0.7° full scale

Arc distance

60/arc = degree per nm


Ie. 60/12 = 5

NSW on a taf

No significant weather

NOSIG on a taf

No significant change

Circling area

Cat A 1.68nm


Cat B 2.66nm


Cat C 4.2nm


Cat D 5.28nm

Factors effecting Mcrit

Weight - higher weight = higher AoA = lower Mcrit


Sweep back - more sweep back = higher Mcrit

Factors effecting Vmcg

Weight


Temp


Density


Runway condition


Power setting


Crosswind

Contaminated runway

More than 25% covered with water/slush/snow 3mm in depth, or ice on any part of the runway surface

Wet runway

Means a runway with sufficient moisture on its surface to cause it to appear reflective but without significant areas of standing water

Types of aqua planning

Dynamic (standing water)


Viscous (damp runway)


Reverted rubber

Horned formula

Aquaplaning V = 9x square root of psi

ROC required

Gradient% x GS x 1.013

Feet per Nm

Vsi x 60 divided by GS

Carbon brakes benifits

Higher efficiency and safety, better service weight and weight consistency

Types of yaw dampers

Parallel - moves rudder pedals aswell (turn off for take off and landing)


Series - works independent (always on)

Dutch roll cause

Strong lateral stability


Weak directional stability


Fixed by yaw damper

Balanced field

TODA=ASDA

Vr

Rotate speed


Must be greater than V1

V1

Speed by which time the decision to continue flight if an engine fails has been made. Ie. Commit to fly speed

V2

Speed at which the airplane will climb in the event of an engine failure. Known as the take off safety speed

Leadership behaviours

Aim high


Passion for people


Step up


Know your customer


Own it

Factors effecting Vmc

Thrust - less thrust, less yaw, lower speed


CofG - forward means greater moment, lower speed


Critical engine - VMC based of crit engine


Weight - little effect


Windmilling prop - increases, VMC based on Windmilling prop

QNE

Question nil elevation


Setting 1013 on the altimeter

QNH

Actual pressure a MSL

QFE

Station level pressure. When set will indicate height above or below the reference pressure point. Ie field

Flying from a high to low

Will overread. Ie saying you are higher than you actually are so very dangerous


High to low look out below

Flying from low to high

Will underread. Ie saying you are lower than you actually are.


Low To high touch the sky

Reactors effecting density

Pressure - directly related, increase P increase D


Temp - inversely related, increase T decrease D


Humidity - inversely related, increase H decrease D (because a water molecule has less mass than an air molecule

Gas to solid

Deposition

Sublimation

Solid to gas

Reason a parcel of air cools as it rises

Expansion

Adiabatic

A change in temp due to a change in pressure, without a change in the total heat energy of an air sample

DALR

3 degrees per 1000ft

SALR

1.5 degrees per 1000ft

Atmospheric stability

When the ELR is less than SALR


Atmospheric instability

When the ELR is greater than the DALR

Conditional instability or stability

ELR is less than DALR but more than SALR

Buys Ballots law

With your back to the wind the low pressure will be on the right (in the southern hemisphere)

Passing of a cold front

Fall in temp


Backing of wind


A rise in pressure

Passing of a warm front

Rise in temp


Backing of the wind


Steady or slight rise

Occluded front

Cold front has caught up with warm front

Types of icing

Hoar frost


Rime ice


Clear ice

Clear ice

Water drops 0 to -15 degrees. Needs to be large drops so usually in cumuliform clouds

Rime ice

Small super cooled water drops -10 to -20 degrees.


Generally forms in stable cloud types

BC

Patches

BL

Blowing

DR

Drifting

MI

Shallow

BR

Mist

DU

Dust

DS

Dust storm

DZ

Drizzle

FC

Funnel cloud

IC

Ice crystals

FU

Smoke

GR

Hail larger than 5mm

GS

Small hail less than 5mm

HZ

Haze

PL

Ice pallets

PO

Dust devils

SA

Sand

SG

Snow grains

SN

Snow

SQ

Squals

SS

Sandstorm

VA

Volcanic ash

VC

Vicinity

PY

Spray

Inter

Intermittent phenomena, expected to occur frequently of periods of less than 30 mins

Tempo

A temporary phenomena, expected to last between 30 and 60 mins

Jet streams

Found at breaks in the tropopause


Less than 100nm wide and a few thousand feet deep

Clear air turbulence (CAT)

Occurs from strong wind shear


Most severe on the polar side and below the level of the core


Also considered to be more severe in winter when the jet streams are stronger, and when the JS is over land and/or curved

Two jet streams

Sub tropical jet - found around 30 degrees


Polar front jet - found just below the tropopause at the polar front

High clouds

Cirrus (ci)


Cirrostratus (Cs)


Cirrocumulus (Cc)

Middle clouds

Altostratus (as) - sheet of middle cloud, may produce rain or virga


Altocumulus (ac) - heaped or lumpy cloud in the middle level, not usually associated with rain

Low clouds

Cumulus (Cu) - heaped or towering, may produce showers of rain or snow


Cumulonimbus (CB) - tower thunderstorm cloud producing heavy showers


Stratus (St) - a low sheet of cloud, may produce drizzle.


Stratocumulus (Sc) - a sheet of heaped or towering cloud, may produce drizzle


Nimbostratus (ns) - a sheet of heavy rain cloud, produces continuous rain or snow

Vertical Separation standards

1000ft below FL290


2000ft above FL290 (can be reduced to 1000ft in rvsm)


Metar ///

Indicates cloud type is not identified

Metar //

When present weather sensor is inop

NCD

Indicates no cloud detected below 10,000ft at AA, CH, WN, or at any level at other aerodromes

Metar ////

Vis not reported

Metar /////////

Cloud not reported


Probably due to a raulty sensor

Splitting a hold left and right hand

Left - inbound plus 70 and reciprocal of that


Right - inbound minus 70 and reciprocal