NDA Geography · Climatology, Atmosphere and Weather
Insolation, Temperature and Solar Geometry
Insolation is the incoming solar energy; how much a place receives depends on the angle of the Sun's rays, the day length and the surface beneath — and crucially the air is warmed from BELOW, by the Earth re-radiating heat, not directly by sunlight.
Why this matters
5 PYQs but conceptually load-bearing — these ideas underpin the whole chapter. Two facts are tested repeatedly: the atmosphere is heated chiefly by LONG-WAVE terrestrial radiation (from the warmed ground, not directly by the Sun), and temperature inversion (when the normal lapse rate flips and air gets warmer with height). The solar-geometry questions reward picturing where the Sun's rays strike most slanted.
Concept 1 of 4
How the atmosphere is heated
Intuition
Definition
- Incoming sunlight (insolation) is short-wave radiation and passes largely through the atmosphere.
- It is absorbed by the Earth's surface, which warms and re-emits energy as long-wave terrestrial radiation.
- The atmosphere is heated mainly by this long-wave terrestrial (ground) radiation, not directly by the Sun's short-wave rays — which is why the troposphere is warmest at the bottom and cools upward.
- The amount of insolation a place receives varies with the rotation of the Earth, the length of the day, and the distribution of land and water (and the angle of the Sun's rays).
Worked example
Practice this conceptself-check · 3 quick reps
From the bank · past-year question
[Q63 · Sep · 2021]
Air is warmed from BELOW
Concept 2 of 4
Measuring air temperature and the lapse rate
Intuition
Definition
- Standard air temperature is measured at about 1.2 m (4 feet) above the ground.
- The average rate at which temperature decreases with height is the environmental (normal) temperature lapse rate — roughly 6.5 degrees C per km.
- This lapse rate is what makes mountain tops colder than valleys at the same latitude.
Worked example
Practice this concept2 quick reps
From the bank · past-year question
[Q110 · Apr · 2024]
Concept 3 of 4
Temperature inversion
Intuition
Definition
- A temperature inversion happens when the normal lapse rate is reversed — temperature INCREASES with height instead of decreasing (cold air trapped beneath warm air).
- It is favoured by long, calm, CLEAR winter nights (the ground radiates heat away rapidly under clear skies). Cloudy skies block this, so cloudy nights do NOT favour inversion.
- Polar areas experience inversion through much of the year (persistent cold surface).
- 'Inversion of rainfall' (in temperate cyclones) is a related but distinct idea — there the front lifts warm air over cold.
Worked example
Practice this conceptself-check · 3 quick reps
From the bank · past-year question
[Q107 · Apr · 2026]
CLOUDY nights do NOT favour inversion
Concept 4 of 4
The angle of the Sun's rays and the solstice
Intuition
Definition
- The Sun's energy is most concentrated where its rays strike vertically and weakest where they strike at a low (minimum) angle.
- At the June Solstice (summer in the Northern Hemisphere), the Sun is overhead at the Tropic of Cancer; the Southern Hemisphere is tilted away.
- So the minimum angle of the Sun's rays at that moment falls on a southern latitude — the Tropic of Capricorn receives the most slanting rays.
Worked example
Practice this concept2 quick reps
From the bank · past-year question
[Q90 · Apr · 2025]
Summary — formulas & gotchas at a glance
A revision cheat-sheet for the formulas and gotchas above. Click any concept name to jump back to its full explanation.
Watch out for (2)
- Air is warmed from BELOW→ How the atmosphere is heated
- CLOUDY nights do NOT favour inversion→ Temperature inversion
Drill every past-year question on this subtopic
6 questions from the bank — paginated, with cart and Word-export support.