Private Pilot · Unit 3 · 30 min

The Pitot-Static Instruments

Lesson goals

By the end of this lesson you will know:

Three of the instruments in front of you run on nothing but air pressure. They carry no gyroscope and draw no electricity to work. The altimeter tells you how high you are, the vertical speed indicator tells you how fast that height is changing, and the airspeed indicator tells you how fast the wing is moving through the air. All three read from the same two pressure sources, and this lesson explains what each one actually measures, how to read it, and how it fails.

An L-shaped metal pitot tube mounted on a strut under the left wing of a white Cessna, its open front end facing forward into the airflow, with the cabin windows and registration below
The pitot tube under the left wing of a Cessna 172. Its open front end faces forward so that air pressed into it by the airplane's motion reaches the airspeed indicator. Photo: Cjp24 (Wikimedia Commons, CC BY-SA 4.0), resized.

Two pressures, one system

The whole system works from two pressures. The first is static pressure, the ordinary barometric pressure of the air around the airplane. It is present whether the airplane is moving or parked, and it falls as the airplane climbs because there is less air overhead. The second is the pressure the airplane's own motion adds. As the airplane moves forward, air is pressed into a forward-facing probe, and the pressure inside that probe rises above the static value by an amount that depends on how fast the airplane is going. This added pressure is the dynamic pressure, also called ram or impact pressure.

Two openings collect these pressures. The pitot tube is the forward-facing probe under the wing in the photo above; its front opening senses the total of static plus dynamic pressure, and a small drain hole at the back lets moisture escape. The static port is a flush opening on the side of the fuselage, set where the passing air is undisturbed, so it senses static pressure alone. The previous lesson introduced the pitot heat that keeps ice out of that probe in visible moisture near freezing; the probe itself and the instruments it drives are the subject here.

Schematic of a pitot-static system. A forward-facing pitot tube with a drain hole feeds a blue ram line that runs to the airspeed indicator only. A flush static port on the fuselage feeds a tan static line that branches to all three instruments: airspeed indicator, altimeter, and vertical speed indicator. An alternate static valve on the static line branches to the cabin. A legend distinguishes the ram line from the static line.
The pitot tube feeds ram pressure to the airspeed indicator alone, while the static port feeds ambient pressure to all three instruments. The altimeter and vertical speed indicator use static pressure only; the airspeed indicator is the one instrument that uses both.

Keep track of which instrument uses which source; the blockage section at the end of this lesson follows directly from it. The altimeter and the vertical speed indicator connect to the static line only. The airspeed indicator connects to both: it receives the pitot pressure on one side and the static pressure on the other, so that the static pressure cancels and only the dynamic pressure is left to move the needle. This division predicts how each instrument fails.

Airplanes with glass cockpits read the same two probes. An air data computer measures the pitot and static pressures electronically and computes altitude, vertical speed, and airspeed for the display, but the pressures it works from are identical to the ones these mechanical instruments use. The pitot tube and static port on a glass-cockpit airplane are the same hardware you see here.

PHAK Ch 8, "Pitot-Static Flight Instruments"

The altimeter

The altimeter measures static pressure and displays it as a height. Inside the sealed case is a stack of aneroid wafers: thin sealed metal capsules with an internal reference pressure of 29.92 inches of mercury. Static pressure from the port fills the case around the wafers. When the airplane climbs, the surrounding static pressure falls, the wafers expand, and a mechanical linkage turns that expansion into a higher reading. When the airplane descends, the higher static pressure compresses the wafers and the reading falls. The instrument is an aneroid barometer with its face marked in feet rather than in inches of mercury.

Cutaway of an altimeter. Static pressure enters the sealed case and surrounds a stack of aneroid wafers, whose expansion drives gears and three pointers on the dial: a long hundreds pointer, a shorter thousands pointer, and a tens-of-thousands pointer. A barometric scale adjustment knob sets the pressure in the altimeter setting window.
Static pressure surrounds the sealed aneroid wafers; their expansion and contraction drive the three pointers through a gear train, and the knob sets the reference pressure in the window. PHAK Figure 8-2 (FAA).

Because the altimeter measures pressure, its reading is only as accurate as the reference pressure you give it. That reference is the altimeter setting, the local pressure corrected to sea level, which you dial into the small window on the face, the Kollsman window. Setting the current local value makes the instrument read height above mean sea level. As pressure varies from place to place, you reset the window along the route so the indicated altitude stays close to your true altitude; the regulations that require this appear in Unit 4, in the Operating Rules for Every Flight lesson.

The three-pointer face is read like a clock with three hands of different weight. The long needle on top reads hundreds of feet, one full turn per thousand. The short, wide needle reads thousands. The long, thin needle with the inverted triangle at its tip reads tens of thousands. An indication with the hundreds pointer at 5 and the thousands pointer between 2 and 3 is two thousand five hundred feet. Misreading the thousands pointer by a full digit is a known error, which is why the numbers are cross-checked against the flight and the terrain rather than read once and trusted.

PHAK Ch 8, "Altimeter" and "Principle of Operation"

The five altitudes and the nonstandard atmosphere

The word altitude means something different depending on what it is measured against, and five kinds matter to you. The atmosphere is the reason they diverge. The standard atmosphere is a reference model in which sea-level pressure is 29.92 inches of mercury, sea-level temperature is 15 degrees Celsius, and both fall at fixed rates with height. The real atmosphere rarely matches it, and every departure from the standard model separates one kind of altitude from another.

Sea level (mean sea level) True altitude (height above mean sea level) Absolute altitude (height above the terrain below) Indicated altitude: the reading on the altimeter face. Pressure and density altitude: computed values, not heights above anything you can see.
Two of the five altitudes are distances you could measure: true altitude down to mean sea level, and absolute altitude down to the terrain directly below. Indicated altitude is whatever the altimeter shows, and pressure and density altitude are computed from 29.92 and temperature, so no arrow can represent them. Airplane drawing by Werneuchen (Wikimedia Commons, public domain).

The gap between indicated and true altitude is where the nonstandard atmosphere becomes a hazard. Setting the current local altimeter setting corrects for the pressure at the reporting station, but it does not correct for temperature, and it goes stale as you fly away from that station. Two situations leave the airplane lower than the altimeter shows. The first is flying from an area of high pressure toward an area of low pressure without resetting the window: the altimeter keeps reading the old, higher pressure as though it were still present, so it overstates your height, and your true altitude is lower than indicated. The second is flying into air colder than standard: cold air is denser, so the pressure levels the altimeter is reading are packed closer to the ground than the standard model assumes, and again your true altitude is lower than indicated.

Warm air (or high pressure) Cold air (or low pressure) constant-pressure surface (the altitude the altimeter reads) true altitude true altitude (higher) (lower) Terrain From high to low, or hot to cold, look out below
Holding a constant indicated altitude means following a surface of constant pressure. Where the air is colder or the pressure lower than the setting assumes, that surface lies closer to the terrain, so true altitude is lower than the altimeter indicates. Airplane drawing by Werneuchen (Wikimedia Commons, public domain).

Both cases share one memory aid: from a high to a low, or from hot to cold, look out below. Both leave the airplane closer to the terrain than the instrument indicates, which is why a colder-than-standard day over mountains calls for a higher indicated altitude to keep the same real clearance, and why you reset the altimeter to each new station along the route.

PHAK Ch 8, "Effect of Nonstandard Pressure and Temperature" and "Types of Altitude"

The vertical speed indicator

The vertical speed indicator (VSI) shows the rate at which the airplane is climbing or descending, in feet per minute. It runs on static pressure alone, but it works by comparing that pressure against a delayed copy of itself. Inside the case is a diaphragm connected directly to the static line. The space around the diaphragm, inside the sealed case, is also connected to the static line, but through a narrow restriction called the calibrated leak.

Cross-section of a vertical speed indicator. A diaphragm inside a sealed case is fed static pressure directly through the static line. The case around the diaphragm is fed the same static line but through a narrow calibrated leak. Linkage runs from the diaphragm to a needle on a dial marked UP and DOWN in hundreds of feet per minute.
The diaphragm receives static pressure at once through the direct line, while the case pressure catches up slowly through the calibrated leak. The difference between the two drives the needle in a climb or descent, and it returns to zero once the pressures equalize in level flight.

In level flight the diaphragm pressure and the case pressure are equal and the needle rests at zero. When the airplane begins to climb, the static pressure falls, and the pressure inside the diaphragm follows immediately while the case pressure lags behind through the leak. The difference between the two pushes the needle to show a climb; in a descent the difference reverses and the needle shows a descent. Because the case pressure needs a moment to catch up through the leak, the instrument has a built-in lag: the needle moves at once to show the direction of change, but the steady value it settles on, the actual rate, is only trustworthy after roughly six to nine seconds of stable flight. The first movement is a trend; the settled reading is a rate.

PHAK Ch 8, "Vertical Speed Indicator"

The airspeed indicator

The airspeed indicator (ASI) is a differential pressure gauge. It admits the total pressure from the pitot tube to one side of a diaphragm and the static pressure from the port to the other side. The static pressure common to both cancels, and what remains to deflect the diaphragm is the dynamic pressure, the pressure the airplane's motion adds. Dynamic pressure is exactly the quantity the wing responds to when it makes lift, so the airspeed indicator reads, in effect, how hard the air is pressing on the airframe.

This is why the airspeed a wing stalls at is quoted as an indicated airspeed. Stalls and Spins established that the wing stalls at a fixed angle of attack, not at a fixed speed, and that the stall speed is simply the speed at which steady flight demands that angle. Because both the wing and the airspeed indicator respond to the same dynamic pressure, the indicated airspeed at the stall stays nearly constant regardless of altitude, even though the airplane is moving faster through the air up high. The four airspeeds you need to keep straight are these:

True airspeed pulls ahead of indicated airspeed as you climb. The engine lesson noted that the air thins with altitude; thinner air produces less dynamic pressure at a given true speed, so to build the same dynamic pressure the airplane must move faster through the thinner air. The airspeed indicator reads dynamic pressure, so for a given calibrated airspeed (in a trainer, nearly the same as indicated) true airspeed grows by roughly two percent per thousand feet. At altitude the wing feels the indicated airspeed while the airplane covers ground at the higher true airspeed, which is the number you use for flight planning.

PHAK Ch 8, "Airspeed Indicator"

Airspeed markings and V-speeds

The colored arcs on the dial turn several structural and aerodynamic limits into marks you can read at a glance. Each boundary is a certificated speed, a V-speed, and the arcs place them where the needle passes.

An airspeed indicator dial in knots with color-coded arcs and a legend. A white arc runs from Vs0 through Vfe, a green arc from Vs1 through Vno, a yellow arc from Vno to a red line at Vne. Callout labels mark Vs0, Vs1, Vfe, Vno, and Vne at the arc boundaries.
The colored arcs and the red line on the airspeed indicator. The white arc is the flap operating range, the green arc the normal operating range, the yellow arc a caution range for smooth air only, and the red line the never-exceed speed.

One important speed is deliberately absent from the dial. Maneuvering speed (VA), which Load Factor and Turns introduced as the speed below which a full control deflection stalls the wing before it can overload the structure, is not marked because it changes with weight: it is lower when the airplane is light and higher when it is heavy. A fixed mark on the dial would be wrong at every weight but one, so maneuvering speed is given on a placard and in the airplane's Pilot's Operating Handbook (POH) instead. You look it up for the day's weight.

PHAK Ch 8, "Airspeed Indicator Markings" and "Other Airspeed Limitations"

Blockages

Because the readings come from pressures in tubes, a blocked tube produces a steady, wrong indication rather than an obviously failed instrument. Blockages come from ice, dirt, or insects, which is why the pitot tube and static ports are checked on every preflight and why the pitot cover is removed before flight. The way an instrument fails depends on which opening blocks, and it follows directly from the plumbing in the first figure.

Three panels of pitot-static blockages. Left: the pitot tube is blocked with a red mark while its drain hole stays open, and the airspeed needle falls to zero. Center: both the pitot tube and its drain are blocked while the static port stays clear, and the airspeed indicator behaves like an altimeter, its needle moving with altitude. Right: the static port is blocked with a clear pitot, and the altimeter freezes, the VSI reads zero, and the airspeed indicator becomes unreliable; the fix is to open the alternate static source.
Three blockage cases. A blocked pitot with an open drain zeroes the airspeed indicator; a blocked pitot and drain together turn it into an altimeter; a blocked static system freezes the altimeter, zeroes the vertical speed indicator, and corrupts the airspeed indicator.

Pitot tube blocked, drain hole clear. Ram air can no longer enter, and the pressure already trapped in the line escapes through the open drain until it falls to the ambient static value. With the same static pressure now on both sides of the diaphragm, the airspeed indicator senses no dynamic pressure and the reading falls to zero. The altimeter and vertical speed indicator, which do not use the pitot tube, are unaffected.

Pitot tube and drain both blocked. Now the pressure in the pitot line is sealed in and cannot change. The static side, still open, keeps responding to altitude. So the airspeed indicator responds only to changes in static pressure: climb and the static pressure falls while the trapped pitot pressure holds, so the needle reads higher; descend and it reads lower. The instrument behaves like an altimeter, moving with altitude and ignoring actual airspeed.

Static ports blocked, pitot clear. This is the worst case because it disables all three static instruments. The altimeter freezes at the altitude where the blockage occurred, because the trapped static pressure can no longer change. The vertical speed indicator reads a constant zero, since the diaphragm and case pressures can never differ. The airspeed indicator keeps moving but reads wrong: it indicates low above the blockage altitude and high below it. The defense is the alternate static source, a valve that admits static pressure from inside the cabin. Cabin pressure is slightly lower than the outside static pressure, so on the alternate source the altimeter reads a little high and the airspeed a little fast. The errors are repeatable properties of the airframe, so the manufacturer measures them and publishes the corrections in the POH. In an airplane without an alternate source, breaking the glass face of the vertical speed indicator vents the static system to the cabin as a last resort, at the cost of that instrument.

Two defenses cover these failures. The pitot heat introduced in the previous lesson keeps ice out of the probe, and the alternate static source restores the static instruments when the ports block. Both are checklist items with procedures in the POH. Knowing which instruments each one restores lets you diagnose a bad reading in flight.

PHAK Ch 8, "Blockage of the Pitot-Static System"

Why this matters in the airplane Three habits follow from how these instruments work. Reset the altimeter to each new station and add clearance on cold days over high terrain, because from a high to a low or from hot to cold your true altitude is lower than the dial shows. Fly the colored arcs by memory, so a glance places the airplane in the flap range, the normal range, or the caution range without reading a number. And when one instrument disagrees with the others, name the blocked opening from the pattern: a zeroed airspeed points at the pitot, a frozen altimeter and dead vertical speed point at the static ports and call for the alternate source.

Check your understanding

Answer from memory, without scrolling back up. Recalling it yourself is what makes it stick.

Which instruments use static pressure only, and which needs both sources?

Standard sea-level conditions in the reference atmosphere are?

How do you read pressure altitude off the altimeter?

Flying from high pressure to low without resetting the altimeter means?

When you begin a climb, the vertical speed indicator shows?

The white and green arcs on the airspeed indicator run?

Why is maneuvering speed missing from the airspeed dial?

If the pitot tube and its drain both block, the airspeed indicator?

A blocked static system with a clear pitot means?

As you climb, true airspeed compared with indicated airspeed?

Go deeper (primary source): read the "Pitot-Static Flight Instruments," "Altimeter," "Vertical Speed Indicator," "Airspeed Indicator," and "Blockage of the Pitot-Static System" sections of PHAK Chapter 8. The gyroscopic instruments and the magnetic compass, which close this unit, come next in The Gyroscopic Instruments and Compass.

Stuck or curious? On your next preflight, ask your instructor to point out the pitot tube, its drain hole, and the static ports, and to show you the alternate static valve in the cockpit. Then, on the takeoff roll, watch the airspeed indicator come alive as ram air first reaches the pitot tube.