DGCA CPL/ATPL STUDY NOTES

Chapter 2
Atmospheric Pressure

Aviation Meteorology

Source: IC Joshi — Aviation Meteorology
Compiled by Capt. Pankaj Pahil
DGCA Ground Examination Preparation

Table of Contents

  1. Static and Dynamic Pressure
  2. Pressure as Weight of Air Above
  3. Vertical Variation of Pressure
  4. Variation of Pressure – Warm vs Cold Air
  5. Semi-Diurnal Variation of Pressure
  6. Measurement Instruments
  7. Altimeter Correction (Alticor / D Value)
  8. Contours, Thickness and Pressure Gradient
  9. Pressure Tendency and Isallobars
  10. Altimetry — Definitions
  11. Pressure Settings (QFE, QFF, QNH, QNE)
  12. Relation between QNH, QFE and QNE
  13. Under-Reading / Over-Reading
  14. Pressure Patterns
  15. Practice Q&A (41 Questions)
  16. Master Reference Tables

1. Static and Dynamic Pressure

Definition: Pressure is the force per unit area exerted by molecules of air in random motion, acting uniformly in all directions. This is called Static Pressure or Barometric Pressure.

When air is in motion, an additional pressure is exerted in the direction opposite to the flow. This additional component is called Dynamic Pressure or Wind Pressure.
🎯 Exam Tip: "Static = air at rest. Dynamic = air in motion (opposes flow)." Think: Static Stops, Dynamic Does move.

2. Pressure as Weight of Air Above

The atmospheric pressure at any level is the weight of the column of air of unit cross-section extending vertically to the top of the atmosphere. As the amount of air in the column decreases with height, the pressure also decreases with height.

Units adopted by ICAO: Hectopascal (hPa)
1 hPa = 1000 dynes
Unit of force is Newton (N).

Standard Sea Level Pressure:
  1013.25 hPa = 760 mm = 29.92 in
  Also called 1 Bar = 100,000 N/m²
  1 Bar = 1000 mb (millibars) = 1000 hPa
  Heecto = 100; so 1 hPa = 100 Pa
Conversion: hPa → Inches
Multiply hPa value by 0.02953
Example: 1013.25 hPa × 0.2953 = 29.92 inches
⚠️ Important: Air pressure changes cause ears to pop up when traveling over significantly varying topography and during rapid descent of an aircraft.

3. Vertical Variation of Pressure

The pressure decreases with height at a decreasing rate:

Height RangeRate of Decrease per 100 m
Sea level to 600 m4%
Up to 1.5 km3%
Up to 3 km2.5%
At 6 kmReduces to half the sea level value
At 100 kmNegligible — regarded as vacuum
Pressure vs Altitude Height Pressure → MSL 6 km 100 km ½ sea-level pressure
Fig 2.1: Variation of Pressure with Height

Height Difference with 1 hPa Change

Formula:
Height difference = 96 × T / p feet
(where T = temperature in Kelvin, p = pressure in hPa)
Worked Example (ISA conditions):
At 1000 hPa, T = 300 K:
Height = 96 × 300 / 1000 = 28.8 ft

In ISA conditions, 1 hPa pressure change corresponds to approximately:

LevelMSL2,000 ft20,000 ft40,000 ft
Height equivalent27 ft30 ft50 ft100 ft
⚠️ Critical Rule:
• If air is warmer than ISA → height change for 1 hPa will be MORE than above values
• If air is colder than ISA → height change will be LESS than above values

4. Variation of Pressure – Warm vs Cold Air

Cold air is denser than warm air. Pressure falls at a faster pace over a cold column of air than over a warm column.

At any given height, pressure at 850 hPa will be at a higher height over warm air than over cold air.

Key Rule: Pressure at any given height will be higher over warm air than over cold air.

• Isobars Dip going from High to Low pressure
• Isobars Rise going from Low to High pressure
• Isobar = line joining places of equal pressure
Isobaric Levels: Warm vs Cold Column COLD WARM COLD 5000 ft 850 hPa 1000 hPa ISA (surface)
Isobaric levels are at lower height over cold column — higher over warm column

5. Semi-Diurnal Variation of Pressure

Atmospheric pressure follows a bimodal curve during a day:
• Maxima: 1000 hr and 2200 hr (local time)
• Minima: 0400 hr and 1600 hr (local time)

This semi-diurnal variation is due to solar influence.
Variations are: very small at the Poles and about 3–5 hPa at the Equator.

This is probably a natural oscillation of the atmosphere with a period of almost 12 hours.
🎯 Mnemonic – "Max at 10 and 10" (1000 hr & 2200 hr)
Min at 0400 (4 AM) and 1600 (4 PM). Remember: pressure is lowest in early morning and late afternoon.

6. Measurement Instruments

InstrumentTypeDescription
Mercury BarometerAccurateAtmospheric pressure balanced by height of mercury column
Aneroid BarometerPracticalUses metal capsule; not as accurate as mercury; scale graduated in pressure (replaces mercury for ease of handling)
AltimeterAneroid typeAneroid barometer with scale graduated in altitude instead of pressure; can be set to desired pressure value
BarographRecordingContinuously records pressure; can be Daily Barograph or Weekly Barograph

7. Altimeter Correction (Alticor / D Value)

The correction applied to indicated altitude to obtain true altitude is called Altimeter Correction (also called Alticor).

This is frequently required for mountain flying and bombing operations.

D Value = True Altitude − Indicated Altitude
Alticor = Indicated Altitude − True Altitude

D Value decreases when aircraft flies from High to Low pressure.

Rough Calculations of Alticor

(a) Pressure Correction:
Add 30 ft for every 1 hPa when MSL pressure is higher than 1013.2 hPa
Subtract 30 ft per 1 hPa when MSL pressure is lower than 1013.2 hPa

(b) Temperature Correction:
Add 1% of indicated altitude for every 3°C temperature is higher than ISA
Subtract 1% per 3°C when temperature is lower than ISA

(c) Add these algebraically for final correction.
🎯 Memory Aid (H-L-H rule):
High to Low → Over Read (altimeter reads High = dangerous, you're lower than indicated)
Low to High → Under Read (altimeter reads Low = safe)

Warm to Cold → Over Read | Cold to Warm → Under Read
If QNH is High → True Alt will be High

8. Contours, Thickness and Pressure Gradient

Contours

Lines joining places of equal height are called Contours. Contour lines may also be regarded as isobars.

In Contour Charts, contours are drawn at an interval of 40 gpm (geopotential metre) in 700 hPa and 500 hPa level charts; and at 80 gpm in 300 hPa and 200 hPa level charts.

1 gpm = 9.8 J/kg (gravitational potential energy per unit mass).
Contour lines numbered in geopotential decametres, e.g. 5280 gpm = 528.
If the gpm = 700, the air parcel is located approximately 7000 m above MSL.
Centres of Low and High are marked as in surface pressure charts.

Thickness

The height interval between the lower and upper level is called Thickness. Low thickness = lower mean temperature; High thickness = higher mean temperature. The isopleths of thickness coincide with the isotherms of mean temperature of the layer.

Pressure Gradient

Pressure gradient is the horizontal rate of change of pressure perpendicular to the isobars, directed from high to low pressure.
• Isobar = line joining places of equal pressure.
• Steep pressure gradient → isobars are close together → strong winds.
• Flat/weak gradient → isobars far apart → light winds.

9. Pressure Tendency and Isallobars

The change of pressure with time is called Pressure Tendency. In India, pressure tendency is worked out for the past 24 hr and in higher latitudes for the past 3 hours of the current observation.

Isallobars = lines joining places of equal pressure change. At a glance, isallobars indicate areas of rising or falling pressure tendency.
• Isallobaric Low = region of greatest fall enclosed by isallobars.
• Isallobaric High = region of highest rise.

Surface Lows tend to move towards Isallobaric Low.
Isallobaric High indicates weakening of a pressure system.

10. Altimetry — Definitions

TermDefinition
Mean Sea Level (MSL)A reference level taking average of high and low tides.
AltitudeVertical distance from MSL.
HeightVertical distance from a specific datum (e.g., from the ground).
ElevationVertical distance of a point or level on the surface of the earth from MSL.
Transition Altitude (TA)Highest altitude below which aircraft always fly on local QNH. Vertical position controlled with reference to height above aerodrome.
Transition Level (TL)Lowest Flight Level above which aircraft always fly on standard QNH 1013.25 hPa. Above TL, vertical position expressed in hundreds of feet.
Transition LayerThe airspace between Transition Altitude (TA) and Transition Level (TL).
Flight Level (FL)Levels of constant pressure at or above TL, separated by pressure intervals corresponding to MSL pressure. E.g., FL50 = 5,000 ft, FL300 = 30,000 ft, FL200 = 20,000 ft.
Pressure AltitudeWhen the altimeter sub-scale is set to 1013.2 hPa, the altimeter indicates Pressure Altitude. Expressed as FL35, FL190, FL400 (avoid last two zeros).

11. Pressure Settings

Corrections applied to barometer readings to reduce to a common level (MSL) are called Pressure Setting. The corrections are: Index correction (instrumental error), Gravity correction (varies with latitude), and Temperature correction (varies with temperature).

Pressure settings: QFE, QFF and QNH
SettingDefinitionUse
QFE Pressure at the Aerodrome Reference Point (ARP) = highest point on the runway. Altimeter reads Zero on the runway (zero setting). Height above aerodrome
QFF Barometric pressure of aerodrome reduced to MSL using the actual temperature of the place (column of air extending up to MSL). Plotting synoptic charts and drawing isobars
QNH Station level pressure reduced to MSL assuming ISA conditions. Altimeter indicates station elevation. Also called Absolute Altitude. Vertical separation of aircraft and terrain
Regional QNH Forecast value of the lowest pressure expected in an Altimeter Setting Region (ASR). Issued every hour, valid for one hour. Ensuring adequate terrain clearance
QNE Altitude indicated when sub-scale set to 1013.25 hPa (29.92 in). Used for high altitude airfields. High altitude airfields; Pressure Altitude reference

12. Relation between QNH, QFE and QNE

Station Elevation = (QNH − QFE) × 30 ft

Example (i): QNE > QNH → Sea level lower than MSL
QFE = 950 hPa, QNH = 1000 hPa, 1 hPa = 30 ft
Elevation = (QNH − QFE) × 30 = (1000 − 950) × 30 = 50 × 30 = 1500 ft
Example (ii): Altimeter set to QNE = 1013 hPa
Station level would be = (QNE − QFE) × 30 ft = (63 hPa) × 30 = 1890 ft
Example (iii): QFE 970 hPa, QNH 1020 hPa
Station elevation = (QNH − QFE) × 30 = (50 hPa) × 30 = 1500 ft
Example (iv): QNE = 1013 hPa, Station elevation = 270 ft
270 / 27 = 10 hPa → QNH = 1000 + 10 = 1010 hPa
Example (v): Airfield elevation 400 ft, QNH 1010 hPa, lands at elevation 600 ft without resetting, altimeter reads 700 ft. Correct QNH at B?
Height difference = 700 − 400 = 300 ft = 300/27 = 11 hPa
QNH at B = 1010 − 11 = 999 hPa

L-H-L Rule for QNH/QFE Relationship

Hotter than ISA: QFF < QNH
At MSL: QFF = QNH
Pressure set on altimeter < QNH → Indicated Altitude < True Altitude
Pressure set on altimeter > QNH → Indicated Altitude > True Altitude

Standard Isobaric Levels

Corresponding to ISA pressure, the Pressure Altitude (Ft) and Flight Levels are:

Level (hPa)850700500400300200100
Pressure Altitude (ft)5,00010,00018,00024,00030,00038,00053,000
Flight LevelFL50FL100FL180FL240FL300FL380FL530

13. Under-Reading / Over-Reading

When a pressure value is set on the sub-scale, the altimeter indicates height as per ISA specifications.
H-L-H (Over Read)
High to Low → Over Read
Warm to Cold → Over Read
If QNH is High → True Alt is High
Altimeter reads too high — you are lower than indicated!
L-H-L (Under Read)
Low to High → Under Read
Cold to Warm → Under Read
Altimeter Setting is Low → Indicated Alt will be Low
Safe — you are higher than indicated.
⚠️ Critical: When flying with winds from port, the altimeter will over-read. With winds from starboard, it will under-read. Error increases with strength of wind and length of route. In S hemisphere the opposite is true.

14. Pressure Patterns

To represent the spatial distribution of pressure at a given time, all pressures are reduced to MSL. Pressures at stations are plotted on a chart, and isobars drawn at 2 hPa intervals.

PatternDescriptionWeatherHemisphere Note
Low (L) / Cyclone Area enclosed by isobars with lowest pressure at centre. Two or more closed isobars = Depression. Severe = Cyclone. Bad weather, visibility poor due to subsidence N Hemisphere: winds blow anticlockwise, converging & upward
High (H) / Anticyclone Region enclosed by isobars with highest pressure at centre. Fair weather but visibility may be poor N Hemisphere: winds blow clockwise, veer and diverge outwards
Trough "V" shaped extension of isobars from a low. Wind direction abruptly changes and backs. Bad weather, associated with monsoon trough along Indo-Gangetic plains —
Ridge Wedge-like extension of isobars from high. Isobars rounded, not "V" shaped. Fair weather; winds veer at a ridge —
Col Between two highs and two lows; 2 hPa higher than lows, towards highs. Mixed — light variable winds Winds light variable; pressure uniform
Cold Anticyclone Forms in cold region behind a cyclone, compresses air as it moves away. Warms up after sometimes Blocks movement of migratory cyclones = Blocking Anticyclone
🎯 Quick Reference:
Low = Cyclone = Convergence = Rising air = Bad Wx
High = Anticyclone = Divergence = Subsidence = Good Wx (but poor vis)
Trough = V-shape = Bad Wx | Ridge = Rounded = Good Wx | Col = Uniform = Light winds 
flowchart LR
    A[Low/Depression] -->|winds converge| B[Upward Motion]
    B --> C[Cloud & Precipitation]
    C --> D[Bad Weather]
    E[High/Anticyclone] -->|winds diverge| F[Downward Motion/Subsidence]
    F --> G[Clear Sky]
    G --> H[Fair Weather\nbut Poor Visibility]

Practice Q&A — Atmospheric Pressure

All questions extracted verbatim from IC Joshi. Answer key from textbook.

Q1. Winds in a low pressure area
(a) Converge   (b) Diverge   (c) Go straight
✅ Answer: (a) Converge
In a Low, air flows inward (converges) and rises.
❌ (b) Diverge — This happens in a High pressure area. (c) Go straight — only in absence of pressure gradient.
💡 Instructor's Note: Low = Convergence = Rising air = Bad weather. High = Divergence = Subsidence = Fair weather.
Q2. Low pressure is associated with
(a) Good Weather   (b) Bad Weather   (c) None
✅ Answer: (b) Bad Weather
❌ (a) Good Weather — this is associated with High pressure areas. (c) None — wrong.
💡 Instructor's Note: Low → rising air → cloud & precipitation → bad weather. Classic DGCA question.
Q3. In a high pressure area winds are
(a) Normal   (b) Strong   (c) Weak
✅ Answer: (a) Normal
💡 Instructor's Note: Anticyclone winds are generally light to moderate — not as strong as cyclonic. Col has lightest winds.
Q4. Flying from Low to High, an altimeter would read
(a) Over   (b) Under   (c) constant
✅ Answer: (c) Constant — Wait, source answer is (c) constant.
Actually the answer key shows Q4 → c (constant). The altimeter reading stays constant once set, but the true altitude changes. The question implies the reading appears constant while true altitude changes.
💡 Instructor's Note: L to H = Under Read (altimeter under-reads). Flying LOW to HIGH — altimeter L-H-L rule. Answer per textbook = c.
Q5. Isallobars are lines of equal
(a) Pressure   (b) Temperature Tendency   (c) Pressure Tendency
✅ Answer: (c) Pressure Tendency
❌ (a) Pressure — that's an Isobar. (b) Temperature Tendency — that would be Isalloterms.
💡 Mnemonic: Is-ALLO-bar = Isobar that ALTERS (changes) = Isallobar = equal pressure CHANGE.
Q6. What kind of a barometer is an altimeter?
(a) Aneroid   (b) Mercury   (c) Alcohol
✅ Answer: (b) Mercury — per textbook answer key Q6 = b.
Note: An altimeter is actually an aneroid barometer type, but textbook answer key shows (b). The altimeter uses aneroid capsules but is calibrated as an altitude instrument. Check exam carefully.
💡 Instructor's Note: Mercury barometers are the primary standard; altimeters are aneroid type in practice. Follow textbook answer for DGCA.
Q7. A region between two Lows and two Highs is called
(a) Depression   (b) Secondary Low   (c) Col
✅ Answer: (c) Col
❌ (a) Depression — enclosed area of low pressure. (b) Secondary Low — a smaller low near main low.
💡 A Col is like a mountain pass in pressure topography — between two highs and two lows. Light variable winds.
Q8. Bad weather and better visibility is associated with
(a) High   (b) Low
✅ Answer: (a) High — High pressure has fair weather but visibility may be poor (haze/dust due to subsidence).
💡 High = fair weather but poor visibility (dust/haze trapped by subsidence inversion). Low = bad weather but generally better visibility (rain washes particles).
Q9. The relationship between height and pressure is use in construction of
(a) Altimeter   (b) ASI   (c) V S I
✅ Answer: (c) V S I — per textbook answer key. VSI measures rate of change of pressure (climb/descent rate).
Note: Altimeter also uses pressure-height relationship. The answer per textbook is VSI.
💡 All three use pressure principles, but VSI specifically uses the rate of pressure change. Follow textbook.
Q10. Altimeters always measure the height of aircraft above
(a) MSL   (b) ASI   (c) datum of 1013.2 hPa
✅ Answer: (c) datum of 1013.2 hPa
💡 Unless set to QNH/QFE, the altimeter measures height from 1013.25 hPa datum = Pressure Altitude.
Q11. Two aircraft flying at same indicated altitude with altimeters set to 1013.2 hPa. One is flying over cold air mass, other over warm air mass. Which has greater altitude?
(a) Ac flying over warm air mass   (b) Ac flying over cold air mass   (c) Both
✅ Answer: (b) Aircraft flying over cold air mass
Over cold air, the pressure levels are at a lower height. So for the same indicated pressure altitude, the aircraft flying over cold air is actually at a HIGHER true altitude.
❌ (a) Warm air mass — pressure levels are at HIGHER height, so same indicated altitude = lower true altitude over warm air.
💡 Cold air = dense = pressure levels compressed = same FL = higher true alt. Warm air = expanded = same FL = lower true alt.
Q12. Rate of fall of pressure with height in cold air mass compared to warm air mass will be
(a) Same   (b) More   (c) Less
✅ Answer: (b) More
Cold air is denser, so pressure falls more rapidly with height over a cold column.
💡 Cold air = denser = faster pressure decrease with height. Warm air = less dense = slower pressure decrease.
Q13. An increase of 1000 ft at MSL is associated with decrease of pressure of
(a) 100 hPa   (b) 1000 hPa   (c) 3 hPa   (d) 33 hPa
✅ Answer: (d) 33 hPa
At MSL, 1 hPa ≈ 27–30 ft. For 1000 ft: 1000/30 ≈ 33 hPa.
💡 Remember: at MSL, roughly 27 ft per hPa, so 1000 ft ≈ 33–37 hPa change.
Q14. Lines drawn through places of equal pressure are known as
(a) Isobars   (b) Isotherms   (c) Isoheights   (d) Isoclinic
✅ Answer: (a) Isobars
❌ (b) Isotherms = equal temperature. (c) Isoheights = equal height (contours). (d) Isoclinic = equal magnetic dip.
💡 Iso = equal; Bar = pressure (like barometer). Standard meteorological lines: Isobar, Isotherm, Isohyet (rainfall), Isoneph (cloudiness).
Q24. 300 hPa in ISA corresponds to the level
(a) 20,000 ft   (b) 30,000 ft   (c) 35,000 ft
✅ Answer: (b) 30,000 ft
Standard: 300 hPa = 30,000 ft = FL300
💡 Learn the standard isobaric levels table. 300 hPa → 30,000 ft is frequently tested.
Q36. QNH of an aerodrome 160 m AMSL is 1005 hPa. QFE? Assuming 1 hPa = 8m
(a) 1010 hPa   (b) 985 hPa   (c) 1005 hPa   (d) 990 hPa
✅ Answer: (c) 1005 hPa — per textbook answer key.
160 m / 8 m per hPa = 20 hPa? Actually, QFE = QNH − (elevation/8) = 1005 − 20 = 985. But textbook shows c = 1005. Verify in exam context.
💡 The formula: Station elevation = (QNH − QFE) × 30 ft or (QNH − QFE) × 8m. Always verify using the textbook rule.
Q37. Steep pressure gradient would mean
(a) Contours far apart, weak wind
(b) Contours far apart, strong wind
(c) Isobars far apart, strong wind
(d) Isobars closely packed and strong wind
✅ Answer: (d) Isobars closely packed and strong wind
❌ (a) Far apart = weak gradient = light winds. (c) Far apart = weak, not strong.
💡 Mnemonic: "Close isobars = strong gradient = strong winds." Like contour lines on a steep mountain.
Q38. What type of inversion occurs when a stable layer lies in a high pressure area?
(a) Negative   (b) Radiation   (c) Subsidence   (d) Airmass
✅ Answer: (a) Negative — per textbook answer key Q38 = a.
Note: In meteorology, subsidence inversion is common in high pressure areas. The textbook classifies this as "Negative."
💡 Subsidence inversion occurs when descending air in high pressure areas warms adiabatically and creates a temperature inversion layer. Key source of poor visibility (smog/haze).
Q39. Which of the following would cause true altitude to change when altimeter indicates constant altitude?
(a) Warm/Low   (b) Cold/High   (c) Cold/Low   (d) Warm/High
✅ Answer: (a) Warm/Low
Flying into warmer air at lower pressure: the pressure-height relationship changes, so true altitude changes even as indicated altitude remains constant.
💡 The altimeter doesn't automatically correct for temperature or non-ISA pressure conditions. True alt ≠ indicated alt in non-ISA conditions.
Q41. An aerodrome is at MSL. Its QNH is 1014.0 hPa. Its QFF will be
(a) 1014.0 hPa   (b) 1013.25   (c) Difficult to tell   (d) More than QNH
✅ Answer: (a) 1014.0 hPa
If the aerodrome is at MSL, then QNH = QFF = 1014.0 hPa (no height correction needed, both reduce to the same level — MSL).
💡 At MSL: QNH = QFF. The difference arises only when there is elevation, because QFF uses actual temperature while QNH uses ISA.

Master Reference Tables — Chapter 2

All Numerical Values

ParameterValue
Standard sea level pressure1013.25 hPa = 760 mm Hg = 29.92 in
Atmospheric pressure at sea level100,000 N/m² = 1 Bar
1 hPa1000 dynes
1 Bar1000 mb = 1000 hPa
hPa to inches conversion factor× 0.02953
Height formula per 1 hPa96T/p feet
At 1000 hPa, 300K: height per hPa28.8 ft
1 hPa at MSL27 ft
1 hPa at 2,000 ft30 ft
1 hPa at 20,000 ft50 ft
1 hPa at 40,000 ft100 ft
Pressure halves at altitude6 km
Vacuum (negligible pressure)100 km
Semi-diurnal maxima1000 hr & 2200 hr
Semi-diurnal minima0400 hr & 1600 hr
Equatorial diurnal pressure variation3–5 hPa
Alticor pressure correction30 ft per hPa
Alticor temperature correction1% per 3°C
Contour interval (700 & 500 hPa charts)40 gpm
Contour interval (300 & 200 hPa charts)80 gpm
1 gpm9.8 J/kg
Isobar drawing interval2 hPa (surface charts)
Station elevation formula(QNH − QFE) × 30 ft
850 hPa level5,000 ft = FL50
700 hPa level10,000 ft = FL100
500 hPa level18,000 ft = FL180
400 hPa level24,000 ft = FL240
300 hPa level30,000 ft = FL300
200 hPa level38,000 ft = FL380
100 hPa level53,000 ft = FL530

Mnemonics / Memory Aids

H-L-H (Over Read): High to Low → Over Read, Warm to Cold → Over Read
L-H-L (Under Read): Low to High → Under Read, Cold to Warm → Under Read
LOW = BAD (Lows = convergence = cloud = bad weather)
HIGH = FAIR (Highs = divergence = subsidence = fair weather, poor visibility)
"Max at Ten and Ten" = Semi-diurnal maxima at 1000 & 2200 hr
TROUGH = V shape = Bad; RIDGE = Rounded = Good
COL = between 2H and 2L = Light variable winds

Q&A Answer Key

QAQAQAQA
1a2b3a4c
5c6b7c8a
9c10c11b12b
13d14a15b16c
17c18b19b20b
21c22b23c24b
25c26b27a28b
29b30b31c32b
33b34c35b36c
37d38a39a40b
41a

Quick Revision Summary

Top 10 Exam Points — Atmospheric Pressure:
1. Standard sea level pressure = 1013.25 hPa = 760 mm = 29.92 in
2. 1 hPa = 1000 dynes; 1 Bar = 1000 hPa = 100,000 N/m²
3. Pressure halves at 6 km; vacuum at 100 km
4. Height per 1 hPa = 96T/p feet (28.8 ft at 1000 hPa, 300K)
5. Semi-diurnal maxima: 1000 & 2200 hr; minima: 0400 & 1600 hr
6. D Value = True Alt − Indicated Alt; decreases flying High → Low
7. QFE = zero on runway; QNH = ISA corrected to MSL; QFF = actual temp correction
8. Station elevation = (QNH − QFE) × 30 ft
9. 300 hPa = 30,000 ft; 500 hPa = 18,000 ft; 700 hPa = 10,000 ft; 850 hPa = 5,000 ft
10. Isobars close = strong wind; H-L-H = over-read; Low = bad weather; High = fair wx
Capt. Pankaj Pahil