QNH, QFE, QFF & QNE Explained Simply — Part 3 | DGCA CPL ATPL Meteorology Ch 2 | Sleepy Notes
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QNH, QFE, QFF & QNE Explained Simply — Part 3 | DGCA CPL ATPL Meteorology Ch 2 | Sleepy Notes
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Capt.CoalField
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Chapter 2 — Atmospheric Pressure, Pressure Systems & Altimetry | PART 3
Part 1 built pressure from the ground up. Part 2 put it on the weather map. This
part gets to the instrument on your panel.
Your altimeter does not measure height. It measures pressure, then guesses the
height using an atmosphere that does not exist. Once that lands, the four settings
stop being four things to memorise and become four sensible answers to four
different questions.
Reference: ICJ (IC Joshi Meteorology), Chapter 2.
═══ COVERED IN PART 3 ═══
PRESSURE GRADIENT
Horizontal rate of change, perpendicular to isobars, High to Low
Isobars close together = steep = strong wind. Far apart = weak.
Gradient sets the wind's SPEED, Coriolis sets the DIRECTION
THE "ISO-" FAMILY
Isobar, Isotherm, Isallobar, Contour/Isohypse — plus Isogonal and Isoclinal,
the two Navigation lines DGCA slips into Met papers
CONTOURS AND THICKNESS
Why surface charts plot pressure but upper-air charts plot height
Contour intervals — 40 gpm at 700 and 500 hPa, 80 gpm at 300 and 200 hPa
Geopotential metre — what it is, and why you can treat it as a metre
THICKNESS is really a THERMOMETER. Warm air stretched = high thickness.
Cold air squashed = low thickness.
TENDENCY AND ISALLOBARS
Isobar = where pressure IS. Isallobar = where it is GOING.
Isallobaric Low — surface Lows move towards it and intensify
Why India works tendency over 24 hours, higher latitudes over 3
MEASUREMENT
Mercury barometer, aneroid barometer, altimeter, barograph
The rule that settles half the exam questions: "-meter" measures,
"-graph" records
ALTIMETRY FOUNDATIONS
Your altimeter is an aneroid barometer with a dial relabelled in feet
It assumes ISA. The real day is never ISA.
HEIGHT, ALTITUDE, ELEVATION, FLIGHT LEVEL — the vocabulary that must be exact
THE FOUR PRESSURE SETTINGS
Index, gravity and temperature corrections applied before any setting is issued
QFE — zero on the runway. Height above the aerodrome.
QNH — reduced to MSL assuming ISA. Reads aerodrome elevation on the ground.
QFF — reduced using the ACTUAL temperature. Why forecasters use it for synoptic
charts, and why pilots do not set it.
QNE — 1013.25 hPa. Pressure altitude and Flight Levels.
Hotter than ISA gives a QFF LOWER than QNH. At MSL the two are equal.
Regional QNH — the forecast LOWEST pressure in the region, and why that is
deliberately safe
TRANSITION
Transition Altitude, Transition Level, Transition Layer
Down low use the LOCAL pressure so you agree with the GROUND. Up high use the
SAME pressure so you agree with EACH OTHER.
STANDARD ISOBARIC LEVELS
850 to 5,000 · 700 to 10,000 · 500 to 18,000 · 400 to 24,000 · 300 to 30,000 ·
200 to 38,000 · 100 to 53,000
How to hold the table in three chunks instead of seven separate facts
═══ STILL TO COME ═══
Over-reading and under-reading (H-L-H and L-H-L) · "High to Low, look out below" ·
Alticor and D-value · Wind drift, altimeter error and Buys Ballot's Law ·
Semi-diurnal variation
Recap of Parts 1 and 2
Pressure gradient
The "iso-" family
Contours and gpm
Thickness
Tendency and isallobars
Barometers and barograph
What your altimeter actually is
Height, Altitude, Elevation, Flight Level
QFE
QNH
QFF
QNE and 1013.2
Regional QNH
Transition Altitude and Level
Standard isobaric levels
Recap
═══ QUESTION BANK ═══
The question bank for this chapter is in a SEPARATE playlist. Every question is
worked the same way — the correct answer, why it is correct, why each other option
is wrong, and the concept it links back to. Notes first, then the QB.
═══ DISCLAIMER ═══
Feel free to share this. No terms, no conditions, nothing to sign. Aviation
training in India needs to be decentralised, and that only happens if material
moves freely.
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Please do not learn this by heart. Ask Why, ask What, ask How. And do not rely on
AI alone — verify against your book and your instructor. Including this.
═══ LAST WORD ═══
Feedback and corrections: capt.coalfield@gmail.com
Replies are slow. Digital detox is a real thing and I am bad at email.
If this helped you, help someone else — a colleague, a friend, a stranger in the
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your parents especially. The syllabus will still be here tomorrow.
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