Both are reported in g/kg, which is exactly why they get muddled — but they divide the vapour by different things. Mixing ratio (w) is grams of vapour per kilogram of the dry air alone. Specific humidity (q) is grams of vapour per kilogram of the whole moist air — dry air plus the vapour itself. Because q's denominator includes that vapour, q is always a shade smaller than w.
How much smaller? Negligible when it's dry, growing with moisture: about 0.5% apart at 5 g/kg, ~2% at 20 g/kg, ~3% at 30 g/kg. So for everyday comfort talk they're interchangeable — but in precise energy balances, or in hot humid and tropical air, the gap is real. Rule of thumb: HVAC engineers use mixing ratio (they call it humidity ratio) because kit adds or removes water from a fixed stream of dry air; meteorologists prefer specific humidity because the total mass of a moving air parcel is what's conserved.
q = w / (1 + w) · both ≈ 622 · e / P when humidity is lowWhat a normal thermometer reads — the air temperature, full stop. It's the horizontal axis of the chart and the single biggest lever on how much vapour the air can hold. Every other moisture quantity is "relative to" this number in some way.
Vapour present as a fraction of saturation at the current temperature. Useful for comfort, mould risk and condensation, but temperature-dependent — quote it with a temperature or it's nearly meaningless. 100% means the air is saturated; push further and water condenses out.
Mass of vapour per mass of the dry air carrying it. The chart's vertical axis. Conserved under heating and cooling, which makes it the cleanest measure of "how much moisture is in this air" and the natural currency for HVAC and meteorology.
Almost the same idea, but per kilogram of the total (moist) air rather than just the dry part. Always a touch smaller than mixing ratio. Meteorologists often prefer it because total air mass is what's physically conserved in a parcel.
Cool the air, holding moisture fixed, and this is the temperature at which it first saturates and dew forms. Because it tracks the actual vapour amount, dew point is a far better "mugginess" gauge than RH: above ~16 °C feels sticky, above ~21 °C feels oppressive. On the chart it's where a horizontal line from your point meets the saturation curve.
What a thermometer reads with a wet wick around it, cooled by evaporation. It's the lowest temperature reachable by evaporative cooling — the limit a swamp cooler or sweating body can hit. When wet-bulb approaches skin temperature (~35 °C), the body can no longer shed heat: a hard survival limit. Always sits between dew point and dry-bulb.
Mass of vapour per cubic metre of air — a density rather than a ratio. Handy when volume matters (drying, museums, growing). Unlike mixing ratio it does drift with temperature and pressure, because the air's volume changes, so it's less common in thermodynamic work.
The slice of total air pressure contributed by water vapour alone (e), against its saturation value (e_s) — the most the air could sustain before condensing. RH is literally these two divided. Everything else on the chart is derived from e.
Total heat content of the air — sensible heat (its temperature) plus the latent heat locked in its vapour. This is what an air-conditioner actually has to remove, and why drying humid air is so energy-hungry: most of the work is condensing water, not lowering temperature.
The psychrometric chart plots dry-bulb (across) against mixing ratio (up). The bright cyan saturation curve is the 100%-RH ceiling — air can't exist above it; a faint dotted copy stays put so the line is always legible even while the glowing one draws in. Dashed lines are constant RH; the green box is a rough thermal-comfort zone.
Pick a city under Climate overlay and its twelve monthly-mean states are plotted and joined into an annual loop, coloured cool-to-warm by month. The shape tells the story: maritime places like London or San Francisco trace a tight, near-vertical loop (mild all year, moisture doing most of the moving); continental places like Minneapolis or Moscow sweep a long diagonal (cold-dry winter to warm-humid summer); monsoon climates like Mumbai hook sharply upward as the rains arrive. Step to a month — or hit Play year — and the calculator loads that month's mean, with a whisker showing the average daily low-to-high range (nearly horizontal, because the moisture barely changes between night and afternoon).