InfoDotInc / archive systemEstablished online record · rebuilding deliberately
InfoDotInc

Technical documents, historic paths, and source-backed reference material.

Archive / FAA Rotorcraft Flying Handbook / FAA Rotorcraft Flying Handbook: Chapter 8 — Performance

Chapter 8 — Performance

Chapter 8 — Performance

FAA-H-8083-21 (2000)

Your ability to predict the performance of a helicopter

is extremely important. It allows you to determine

how much weight the helicopter can carry before

takeoff, if your helicopter can safely hover at a spe-

cific altitude and temperature, how far it will take to

climb above obstacles, and what your maximum

climb rate will be.

FACTORS AFFECTING PERFORMANCE

A helicopter’s performance is dependent on the power

output of the engine and the lift production of the

rotors, whether it is the main rotor(s) or tail rotor. Any

factor that affects engine and rotor efficiency affects

performance. The three major factors that affect per-

formance are density altitude, weight, and wind.

DENSITY ALTITUDE

The density of the air directly affects the performance

of the helicopter. As the density of the air increases,

engine power output, rotor efficiency, and aerodynamic

lift all increase. Density altitude is the altitude above

mean sea level at which a given atmospheric density

occurs in the standard atmosphere . It can also be

interpreted as pressure altitude corrected for nonstan-

dard temperature differences.

Pressure altitude is displayed as the height above a

standard datum plane, which, in this case, is a theoret-

ical plane where air pressure is equal to 29.92 in. Hg.

Pressure altitude is the indicated height value on the

altimeter when the altimeter setting is adjusted to

29.92 in. Hg. Pressure altitude, as opposed to true alti-

tude, is an important value for calculating perform-

ance as it more accurately represents the air content at

a particular level. The difference between true altitude

and pressure altitude must be clearly understood. True

altitude means the vertical height above mean sea level

and is displayed on the altimeter when the altimeter is

correctly adjusted to the local setting.

For example, if the local altimeter setting is 30.12 in.

Hg., and the altimeter is adjusted to this value, the

altimeter indicates exact height above sea level.

However, this does not reflect conditions found at this

height under standard conditions. Since the altimeter

setting is more than 29.92 in. Hg., the air in this exam-

ple has a higher pressure, and is more compressed,

indicative of the air found at a lower altitude.

Therefore, the pressure altitude is lower than the actual

height above mean sea level.

To calculate pressure altitude without the use of an

altimeter, remember that the pressure decreases

approximately 1 inch of mercury for every 1,000-foot

increase in altitude. For example, if the current local

altimeter setting at a 4,000-foot elevation is 30.42, the

pressure altitude would be 3,500 feet. (30.42 – 29.92 =

.50 in. Hg. 3 1,000 feet = 500 feet. Subtracting 500 feet

from 4,000 equals 3,500 feet).

The four factors that most affect density altitude are:

atmospheric pressure, altitude, temperature, and the

moisture content of the air.

ATMOSPHERIC PRESSURE

Due to changing weather conditions, atmospheric pres-

sure at a given location changes from day to day. If the

pressure is lower, the air is less dense. This means a

higher density altitude and less helicopter performance.

Density Altitude—Pressure altitude corrected for nonstandard temper-

ature variations. Performance charts for many older aircraft are based

on this value.

Standard Atmosphere—At sea level, the standard atmosphere consists

of a barometric pressure of 29.92 inches of mercury (in. Hg.) or 1013.2

millibars, and a temperature of 15°C (59°F). Pressure and temperature

normally decrease as altitude increases. The standard lapse rate in the

lower atmosphere for each 1,000 feet of altitude is approximately 1 in.

Hg. and 2°C (3.5°F). For example, the standard pressure and tempera-

ture at 3,000 feet mean sea level (MSL) is 26.92 in. Hg. (29.92 – 3) and

9°C (15°C – 6°C).

Pressure Altitude—The height above the standard pressure level of

29.92 in. Hg. It is obtained by setting 29.92 in the barometric pressure

window and reading the altimeter.

True Altitude—The actual height of an object above mean sea level.

ALTITUDE

As altitude increases, the air becomes thinner or less

dense. This is because the atmospheric pressure acting

on a given volume of air is less, allowing the air mole-

cules to move further apart. Dense air contains more air

molecules spaced closely together, while thin air con-

tains less air molecules because they are spaced further

apart. As altitude increases, density altitude increases.

TEMPERATURE

Temperature changes have a large affect on density alti-

tude. As warm air expands, the air molecules move fur-

ther apart, creating less dense air. Since cool air

contracts, the air molecules move closer together, cre-

ating denser air. High temperatures cause even low ele-

vations to have high density altitudes.

MOISTURE (HUMIDITY)

The water content of the air also changes air density

because water vapor weighs less than dry air.

Therefore, as the water content of the air increases, the

air becomes less dense, increasing density altitude and

decreasing performance.

Humidity, also called “relative humidity,” refers to the

amount of water vapor contained in the atmosphere,

and is expressed as a percentage of the maximum

amount of water vapor the air can hold. This amount

varies with temperature; warm air can hold more water

vapor, while colder air can hold less. Perfectly dry air

that contains no water vapor has a relative humidity of

0 percent, while saturated air that cannot hold any more

water vapor, has a relative humidity of 100 percent.

Humidity alone is usually not considered an important

factor in calculating density altitude and helicopter per-

formance; however, it does contribute. There are no

rules-of-thumb or charts used to compute the effects of

humidity on density altitude, so you need to take this

into consideration by expecting a decrease in hovering

and takeoff performance in high humidity conditions.

HIGH AND LOW

DENSITY ALTITUDE CONDITIONS

You need to thoroughly understand the terms “high

density altitude” and “low density altitude.” In general,

high density altitude refers to thin air, while low den-

sity altitude refers to dense air. Those conditions that

result in a high density altitude (thin air) are high ele-

vations, low atmospheric pressure, high temperatures,

high humidity, or some combination thereof. Lower

elevations, high atmospheric pressure, low tempera-

tures, and low humidity are more indicative of low

density altitude (dense air). However, high density

altitudes may be present at lower elevations on hot

days, so it is important to calculate the density altitude

and determine performance before a flight.

One of the ways you can determine density altitude is

through the use of charts designed for that purpose.

[Figure 8-1]. For example, assume you are planning to

depart an airport where the field elevation is 1,165 feet

MSL, the altimeter setting is 30.10, and the tempera-

ture is 70°F. What is the density altitude? First, correct

for nonstandard pressure (30.10) by referring to the

right side of the chart, and subtracting 165 feet from

the field elevation. The result is a pressure altitude of

1,000 feet. Then, enter the chart at the bottom, just

above the temperature of 70°F (21°C). Proceed up the

chart vertically until you intercept the diagonal 1,000-

foot pressure altitude line, then move horizontally to

the left and read the density altitude of approximately

2,000 feet. This means your helicopter will perform as

if it were at 2,000 feet MSL on a standard day.

Most performance charts do not require you to com-

pute density altitude. Instead, the computation is built

into the performance chart itself. All you have to do is

enter the chart with the correct pressure altitude and the

temperature.

WEIGHT

Lift is the force that opposes weight. As weight

increases, the power required to produce the lift needed

to compensate for the added weight must also increase.

Most performance charts include weight as one of the

variables. By reducing the weight of the helicopter, you

may find that you are able to safely take off or land at a

location that otherwise would be impossible. However,

if you are ever in doubt about whether you can safely

perform a takeoff or landing, you should delay your

takeoff until more favorable density altitude conditions

exist. If airborne, try to land at a location that has more

favorable conditions, or one where you can make a

landing that does not require a hover.

In addition, at higher gross weights, the increased

power required to hover produces more torque, which

means more antitorque thrust is required. In some heli-

copters, during high altitude operations, the maximum

antitorque produced by the tail rotor during a hover

may not be sufficient to overcome torque even if the

gross weight is within limits.

WINDS

Wind direction and velocity also affect hovering, take-

off, and climb performance. Translational lift occurs

anytime there is relative airflow over the rotor disc.

This occurs whether the relative airflow is caused by

helicopter movement or by the wind. As wind speed

increases, translational lift increases, resulting in less

power required to hover.

The wind direction is also an important consideration.

Headwinds are the most desirable as they contribute to

the most increase in performance. Strong crosswinds

and tailwinds may require the use of more tail rotor

thrust to maintain directional control. This increased

tail rotor thrust absorbs power from the engine, which

means there is less power available to the main rotor

for the production of lift. Some helicopters even have a

critical wind azimuth or maximum safe relative wind

chart. Operating the helicopter beyond these limits

could cause loss of tail rotor effectiveness.

Takeoff and climb performance is greatly affected by

wind. When taking off into a headwind, effective trans-

lational lift is achieved earlier, resulting in more lift and

a steeper climb angle. When taking off with a tailwind,

more distance is required to accelerate through transla-

tion lift.

PERFORMANCE CHARTS

In developing performance charts, aircraft manufactur-

ers make certain assumptions about the condition of the

helicopter and the ability of the pilot. It is assumed that

the helicopter is in good operating condition and the

engine is developing its rated power. The pilot is

assumed to be following normal operating procedures

and to have average flying abilities. Average means a

pilot capable of doing each of the required tasks cor-

rectly and at the appropriate times.

Using these assumptions, the manufacturer devel-

ops performance data for the helicopter based on

actual flight tests. However, they do not test the hel-

icopter under each and every condition shown on a

performance chart. Instead, they evaluate specific

data and mathematically derive the remaining data.

HOVERING PERFORMANCE

Helicopter performance revolves around whether or

not the helicopter can be hovered. More power is

required during the hover than in any other flight

regime. Obstructions aside, if a hover can be maintained,

a takeoff can be made, especially with the additional

benefit of translational lift. Hover charts are provided for

in ground effect (IGE) hoverand out of ground effect

(OGE) hover under various conditions of gross weight,

altitude, temperature, and power. The “in ground effect”

hover ceiling is usually higher than the “out of ground

effect” hover ceiling because of the added lift benefit

produced by ground effect.

)+YR8

)+Y(8

)+Y)8

)+YG8

)+YW8

)+YH8

)+YB8

)+YC8

)+Y+8

)+YK8

)KYR8

)KY(8

)KY)8

)KYG8

)KYW8

)KYH8

)KYB8

)KYC8

)KY+8

)KYK8

)KYK)8

GRYR8

)NO(8

GRY)8

GRYG8

GRYW8

GRYH8

GRYB8

GRYC8

GRY+8

GRYK8

G(YR

(N+)W8

(NC)C8

(NBGR8

(NHGG8

(NWGB8

(NGWR8

(N)WW8

(N(W+8

(NRHG8

KHC8

+BG8

CB+8

BCG8

HCK8

W+H8

GK)8

)K+8

)RH8

(()8

)R8

ICG8

,(WV8

I)HC8

IGW+8

IWWR8

IHG(8

IB))8

IC()8

I+RG8

I+KG8

IK+G

bltimetere

Setting

Pressuree

bltitudee

;onversione

Factor

,(+77

ϒF

ϒ; ,(M

(N

,–

MN

,(

)N

%

%N

(N

VN

(W

WN

M(

–N

M–

+N

)M

KN

OutsideDAirDTemperature

Approximate Density Altitude – Thousands of Feet

(G

()

((

(R

+

)

(

SL

()NRRR

((NRRR

(RNRRR

KNRRR

+NRRR

CNRRR

BNRRR

HNRRR

WNRRR

GNRRR

)NRRR

(NRRR

I(NRRR

Pressure Altitude – Feet

StandardTemperature

SeaLevel

Figure 8-1. Density Altitude Chart.

In Ground Effect (IGE) Hover—Hovering close to the surface (usually

less than one rotor diameter above the surface) under the influence of

ground effect.

Out of Ground Effect (OGE) Hover—Hovering greater than one rotor

diameter distance above the surface. Because induced drag is greater

while hovering out of ground effect, it takes more power to achieve a

hover. See Chapter 3—Aerodynamics of Flight for more details on IGE

and OGE hover.

Since the gross weight of your helicopter is less than

this, you can safely hover with these conditions.

SAMPLE PROBLEM 2

Once you reach the remote location in the previous

problem, you will need to hover out of ground effect

for some of the pictures. The pressure altitude at the

remote site is 9,000 feet, and you will use 50 pounds

of fuel getting there. (The new gross weight is now

1,200 pounds.) The temperature will remain at +15°C.

Using figure 8-3, can you accomplish the mission?

Enter the chart at 9,000 feet (point A) and proceed to

point B (+15°C). From there determine that the maxi-

mum gross weight to hover out of ground effect is

approximately 1,130 pounds (point C). Since your

gross weight is higher than this value, you will not be

able to hover with these conditions. To accomplish the

mission, you will have to remove approximately 70

pounds before you begin the flight.

These two sample problems emphasize the importance of

determining the gross weight and hover ceiling throughout

DENSITYDALTITUDE9

()NBRRDFT

STANDARDDDAY

LPointDAP

KRR (NRRR (N(RR (N)RR (NGRR (NWRR

GROSSDWEIGHTDIDLBSY

W)H WHR WCH HRR H)H HHR HCH(W

(G

()

((

(R

+

)

(

PRESSURE bLTITUDE , Hp X (XNNN FTO

OAT

ϒC ϒF

– )R –DDDDW

E (W

E G)

E HR

E B+

E +B

E (RW

– (R

E (R

E )R

E GR

E WR

OUT7OF7GROUND7EFFE;Te

FULL7THROTTLE7I7OR7LIMIT7MbNIFOLDe

PRESSURED7bND7(N%U7RPM

GROSSDWEIGHTDIDKGSY

MbX7;ONTO7OR7FULL7THROTTLEe

OGE7HOVER7;EILING7VSO7GROSS7WEIGHT

BRRDDDB)H

–MN

–(N

p(N

pMNp)N

p%N

ObT

ϒ;

LPointDBP

LPointDCP

Figure 8-3. Out of Ground Effect Hover Ceiling versus Gross

Weight Chart.

As density altitude increases, more power is required to

hover. At some point, the power required is equal to the

power available. This establishes the hovering ceiling

under the existing conditions. Any adjustment to the

gross weight by varying fuel, payload, or both, affects

the hovering ceiling. The heavier the gross weight, the

lower the hovering ceiling. As gross weight is

decreased, the hover ceiling increases.

SAMPLE PROBLEM 1

You are to fly a photographer to a remote location to

take pictures of the local wildlife. Using figure 8-2, can

you safely hover in ground effect at your departure

point with the following conditions?

Pressure Altitude..................................8,000 feet

Temperature...............................................+15°C

Takeoff Gross Weight.....................1,250 pounds

R.P.M..........................................................104%

First enter the chart at 8,000 feet pressure altitude

(point A), then move right until reaching a point mid-

way between the +10°C and +20°C lines (point B).

From that point, proceed down to find the maximum

gross weight where a 2 foot hover can be achieved. In

this case, it is approximately 1,280 pounds (point C).

DENSITYDALTITUDE9

()NBRRDFT

STANDARDDDAY

(NGCR

LPointDAP

LPointDBP

KRR (NRRR (N(RR (N)RR (NGRR (NWRR

GROSSDWEIGHTDIDLBSY

W)H WHR WCH HRR H)H HHR HCH(W

(G

()

((

(R

+

)

(

ObT

ϒ;

PRESSURE bLTITUDE , Hp X (XNNN FTO

OAT

ϒC ϒF

– )R –DDDDW

E (W

E G)

E HR

E B+

E +B

E (RW

– (R

E (R

E )R

E GR

E WR

IN7GROUND7EFFE;T7bT7M7FOOT7SKID7;LEbRbN;Ee

FULL7THROTTLE7bND7(N%U7RPM

GROSSDWEIGHTDIDKGSY

–MN

–(N

p(N

pMN

p)N

p%N

IGE7HOVER7;EILING7VSO7GROSS7WEIGHT

LPointDCP

Figure 8-2. In Ground Effect Hover Ceiling versus Gross

Weight Chart.

the entire flight operation. Being able to hover at the take-

off location with a certain gross weight does not ensure the

same performance at the landing point. If the destination

point is at a higher density altitude because of higher ele-

vation, temperature, and/or relative humidity, more power

is required to hover. You should be able to predict whether

hovering power will be available at the destination by

knowing the temperature and wind conditions, using the

performance charts in the helicopter flight manual, and

making certain power checks during hover and in flight

prior to commencing the approach and landing.

TAKEOFF PERFORMANCE

If takeoff charts are included in the rotorcraft flight man-

ual, they usually indicate the distance it takes to clear a 50-

foot obstacle based on various conditions of weight,

pressure altitude, and temperature. In addition, the values

computed in the takeoff charts usually assume that the

flight profile is per the applicable height-velocity diagram.

SAMPLE PROBLEM 3

In this example, determine the distance to clear a 50-

foot obstacle with the following conditions:

Pressure Altitude..................................5,000 feet

Takeoff Gross Weight.....................2,850 pounds

Temperature .................................................95°F

Using figure 8-4, locate 2,850 pounds in the first col-

umn. Since the pressure altitude of 5,000 feet is not one

of the choices in column two, you have to interpolate

between the values from the 4,000- and 6,000-foot

lines. Follow each of these rows out to the column

headed by 95°F. The values are 1,102 feet and 1,538

feet. Since 5,000 is halfway between 4,000 and 6,000,

the interpolated value should be halfway between these

two values or 1,320 feet ([1,102 + 1,538] 4 2 = 1,320).

CLIMB PERFORMANCE

Most of the factors affecting hover and takeoff per-

formance also affect climb performance. In addition,

turbulent air, pilot techniques, and overall condition of

the helicopter can cause climb performance to vary.

A helicopter flown at the “best rate-of-climb” speed

will obtain the greatest gain in altitude over a given

period of time. This speed is normally used during the

climb after all obstacles have been cleared and is usu-

ally maintained until reaching cruise altitude. Rate of

climb must not be confused with angle of climb.

Angle of climb is a function of altitude gained over a

given distance. The best rate-of-climb speed results in

the highest climb rate, but not the steepest climb angle

and may not be sufficient to clear obstructions. The

“best angle-of-climb” speed depends upon the power

available. If there is a surplus of power available, the

helicopter can climb vertically, so the best angle-of-

climb speed is zero.

Wind direction and speed have an effect on climb per-

formance, but it is often misunderstood. Airspeed is

the speed at which the helicopter is moving through

the atmosphere and is unaffected by wind.

Atmospheric wind affects only the groundspeed, or

speed at which the helicopter is moving over the

earth’s surface. Thus, the only climb performance

Grosse

Weighte

Pounds

Pressuree

bltitudee

Feet

bte

–()ϒF

–MVϒ;

bte

M)ϒF

–Vϒ;

bte

VKϒF

(Vϒ;

bte

KVϒF

)Vϒ;

TbKE,OFF7DISTbN;E7IFEET7TO7;LEbR7VN7FOOT7OySTb;LED

GCG9

WRR9

W)+9

WB(9

HBC9

HG(9

HB+9

B((9

BHW9

+((9

CWG9

CCR9

+B(9

KGK9

(N)R(

WR(9

WGW9

WB)9

H(R9

BCW9

HBK9

B(W9

BBR9

C)C9

KCH9

+RB9

+CB9

KWR9

(NRBW9

(NH)C

WGR9

WB(9

WKW9

H+H9

CCK9

B(G9

BBR9

CRK9

+W+9

(N(WW9

+BW9

K)K9

(NR(C9

(N)HH9

9– –

)N(HR9

)NHRR9

)N+HR

WH+9

WK(9

H)C9

BCC9

+KB9

BH)9

CR(9

CHK9

K+B9

(NGHH9

K)K9

(NR((9

(N(R)9

(NHG+9

(NG)R

SL9

)NRRR9

WNRRR9

BNRRR9

+NRRR9

SL9

)NRRR9

WNRRR9

BNRRR9

+NRRR9

SL9

)NRRR9

WNRRR9

BNRRR9

+NRRR

Figure 8-4. Takeoff Distance Chart.

affected by atmospheric wind is the angle of climb and

not the rate of climb.

SAMPLE PROBLEM 4

Determine the best rate of climb using figure 8-5. Use

the following conditions:

Pressure Altitude................................12,000 feet

Outside Air Temperature ...........................+10°C

Gross Weight..................................3,000 pounds

Power ...........................................Takeoff Power

Anti-ice ..........................................................ON

Indicated Airspeed .................................52 knots

With this chart, first locate the temperature of +10°C

(point A). Then proceed up the chart to the 12,000-foot

pressure altitude line (point B). From there, move hori-

zontally to the right until you intersect the 3,000-foot

line (point C). With this performance chart, you must

now determine the rate of climb with anti-ice off and

then subtract the rate of climb change with it on. From

point C, go to the bottom of the chart and find that the

maximum rate of climb with anti-ice off is approxi-

mately 890 feet per minute. Then, go back to point C

and up to the anti-ice-on line (point D). Proceed hori-

zontally to the right and read approximately 240 feet

per minute change (point E). Now subtract 240 from

890 to get a maximum rate of climb, with anti-ice on,

of 650 feet per minute.

Other rate-of-climb charts use density altitude as a

starting point. [Figure 8-6] While it cleans up the chart

somewhat, you must first determine density altitude.

Notice also that this chart requires a change in the indi-

cated airspeed with a change in altitude.

RbTE7OF7;LIMy7—7MbXIMUM e

TbKEOFF7POWER7

–%N –MN N MN %N N M % W + (N (M (% (W (+ MN MM M% MW M+ )N )M

ObT7—7ϒ ; bNTI,I;E7OFF7RbTE7OF7;LIMy7—7FTOGMINO7IX7(NND

(RR

)RR

GRR

WRR

HRR

RUCorrection — FTYUMINY

This7;hart7is7yased7onhe

7Indicated7birspeed7WN7MPH7VM7KNOTSe

NM7ENGINE7RPM7(NNU

PRESSURE

ALTITUDE

—

FTY

)RNRRR

(+NRRR

(BNRRR

(WNRRR

()NRRR

(RNRRR

BNRRR

WNRRR

)NRRR

SYLY

GROSSWEIGHT

POUNDS

)NRRR)N)RR)NWRR)NBRR)N+RRGNRRRGN)RR

+NRRR

IPoint7bD

IPoint7yD IPoint7;D

IPoint7DD

IPoint7ED

+KN7ftGminOe

– M%N7ftGminOe

7 WVN7ftGminO

HOTe

DbY

bNTI,I;E7ON

Figure 8-5. Maximum Rate-of-Climb Chart.

%NN7777777WNN777777+NN77777(XNNN7777(XMNN777(X%NN

(MXNNNe

(NXNNNe

+XNNNe

WXNNNe

%XNNNe

MXNNNe

Rate7of7;limbX7Feet7Per7Minute

Density bltitude — Feet

RbTE7OF7;LIMyGDENSITY7bLTITUDEe

MX)VN7LySO7GROSS7WEIGHTe

yEST7RbTE7OF7;LIMy7SPEED7VbRIES7WITHe

bLTITUDEB7V–7MPH7bT7SOLO7DE;REbSING7TO7%Ke

MPHX7IbS7bT7(MXNNN7FTO

Figure 8-6. This chart uses density altitude in determining

maximum rate of climb.

Original source PDFPublished from pages 62–67 of the recorded source chapter.
Open source PDF ↗