Lesson 1.5Lesson 1.5 · The Tools of Climate Analysis
Wind, Rain and the Monsoon Vector
Air has a direction, a speed, and — in India — a season that flips it 180°.
The window that caught the breeze now catches the storm
A coastal Karnataka house opens big windows to the south-west sea breeze — and for eight months it is perfect. Then the monsoon swings hard from the same south-west quarter at 40 km/h, this time carrying horizontal rain, and those generous openings become a fire-hose inlet. Nothing about the house changed. The wind did. The air that cools you in January is the air that floods you in June. So the question is never just "where is the wind?" — it is: which wind, in which season, carrying what?
Which wind, in which season, carrying what? Ask it before you place a single opening.
India's defining event is a direction change
Most of the world's climates have a prevailing wind. India has two — and they point opposite ways.
For roughly half the year the south-west monsoon (June–September) drags moist air off the warming ocean onto the land: it carries both the cooling breeze every building wants and the driving rain every building fears. For the other half — the retreating north-east monsoon and the dry winter (October–May) — the flow runs the other way, land-to-sea, bringing dry air, dust and the winter chill.
This seasonal flip is the monsoon reversal — the subcontinent's defining climatic rhythm. A building on the coast must answer to both winds, because they often arrive from the same compass quarter at opposite times of year.
Read the rose by season, never by the year
A wind rose is a radial diagram: petals reach out from a centre toward each compass direction, their length showing how often the wind blows from there and their banding showing how strongly. It is the working drawing for any ventilation decision.
But for monsoon India there is a trap. An *annual-average* wind rose for a monsoon city is worse than useless — it smears two opposite winds into a meaningless smudge in the middle, hiding the very signal you need. The June south-westerly and the December north-easterly cancel each other on the page, and you end up designing for a wind that never actually blows.
The discipline is simple: always split the rose. Draw one for the monsoon months and one for the dry months. Read each on its own. The prevailing arm swings between them — and your openings have to live with both positions of that arm.
An annual-average wind rose for a monsoon city is a smudge. Split it — one rose for the monsoon, one for the dry.
Two winds, the rain between — design for both
The instinct is to pick the dominant wind and orient to it. On a monsoon coast that fails, because the dominant wind brings the rain too. So you don't choose — you design openings that answer the breeze *and* shed the storm on the same line.
Aim the main openings at the monsoon breeze, then protect them: deep overhangs, a wrapping verandah, louvres set to the local driving-rain angle. When that wind turns to water, the geometry sheds the rain while air still slips through underneath. This is exactly the logic of the Mangalore-tiled coastal house — deep eaves, a shaded verandah on the weather side, never bare glass facing the sea.
And ventilation needs a path, not just an inlet. A windward opening with no leeward escape barely moves air at all — it just presses on the glass. Cross-ventilation lives or dies on the outlet.
Three altitudes on the same idea
Read the band that fits you — or all three.
Ask two plain questions about your site: which direction does the cool breeze come from, and which direction does the driving rain come from? In coastal India the answer is usually the *same* direction — the south-west — at different times of year. So you do want big openings facing that way to catch the air, but they must be protected by a deep verandah or chajja, never left as bare glass staring at the monsoon. The breeze and the storm share a doorway; build the porch.
Pull seasonal wind roses from IMD (not an annual composite), and orient the primary ventilation axis to the monsoon-season breeze. Then layer rain defence on the same façade: size overhang depth to the local driving-rain angle, recess the openings, add operable louvres. Specify the Driving Rain Index for the site per IS 1346 / SP 41 so the protection is sized, not guessed. Above all, give every windward inlet a leeward outlet — an inlet without an escape path barely ventilates, however large it is.
Two relations carry this lesson. Wind pressure across an opening is p = ½ρv² with air density ρ ≈ 1.2 kg/m³: a 3 m/s breeze gives p ≈ 5.4 Pa, while 1.5 m/s gives only ≈ 1.35 Pa — a quarter. Because pressure scales with the *square* of speed, doubling wind speed quadruples the driving pressure, which is why aiming at the stronger wind beats enlarging the window. Rain angle is tan θ = v_wind / v_fall, with raindrop fall speed v_fall ≈ 6–9 m/s: a 9 m/s wind against a 9 m/s fall gives θ ≈ 45°. The overhang must shadow the opening from *that* slanted angle, not from the vertical.
“Bigger windows mean better ventilation — just maximise the opening area.”
Run the method yourself
Run the method once, on your own city, before the module ends.
- 1Find your city's prevailing hot/monsoon-season wind direction from IMD seasonal data.
- 2Mark it on a site plan — your main openings want to face it.
- 3Find the driving-rain direction (usually the monsoon wind). If it matches the breeze, those openings need rain protection on the same face.
- 4Sketch one opening that catches the breeze and sheds the rain, then mark its outlet on the opposite side — without that outlet the inlet barely works.
↳ Use the worksheet below to record your answers.
Take it with you
Wind is a vector with a season
The tools are built; now we use them. Module 2 takes the hot-dry territory — Jaisalmer, Bikaner, the Thar — and turns analysis into construction: thermal mass and time-lag, courtyards and jaalis, evaporative cooling, night flushing, every strategy sized with the instruments you just learned. We begin where the desert taught its builders first: with mass.
