Mumbai summer: 32°C, 75% humidity → dew point ~27°C
Oppressive. Sweat doesn't evaporate well. Combined with 32°C air, heat index reaches 42°C. This is why Mumbai summers are notoriously uncomfortable - high dew point, not just high temperature.
Calculate dew point - the temperature at which air becomes saturated and water condenses. Above 65°F (18°C) starts to feel humid; above 75°F (24°C) is oppressive. The Magnus formula gives accurate results across normal weather ranges.
Dew point
24 °C
Oppressive
Oppressive
Most people uncomfortable
Dew point is the absolute measure of moisture in the air - unlike relative humidity which depends on temperature. A 50% RH reading at 30°C means the air holds lots of water (about 13g/kg); the same 50% RH at 5°C holds much less (about 3g/kg). Dew point cuts through this confusion: it tells you the temperature at which air becomes saturated (100% RH) and dew/condensation forms. A dew point of 22°C means the air carries enough moisture that any surface cooler than 22°C will get wet. This is why your cold drink glass 'sweats' on a Mumbai July day - the glass surface (chilled by the drink) drops below the air's dew point.
For Indian users, dew point directly explains the 'feels-like' summer/monsoon discomfort. Coastal cities like Mumbai, Chennai, Kochi have summer dew points often above 25°C - oppressive territory where sweat doesn't evaporate. Delhi and inland North India have lower dew points (15-20°C in summer) - hotter air but drier, which feels less sticky despite being warmer. Bangalore at moderate elevation has comfortable dew points (typically 17-21°C). This calculator uses the Magnus formula, accurate to within 0.4°C across normal weather conditions, and gives both °C and °F output.
Pick units: °C or °F.
Enter air temperature.
Enter relative humidity in %.
Read the dew point.
The Magnus formula computes the actual water-vapour pressure from temperature and humidity, then back-solves for the temperature at which that pressure equals saturation (100% RH).
α = (a·T)/(b + T) + ln(RH/100) Dew point = (b·α) / (a − α) a = 17.27, b = 237.7°C
Magnus formula (also called August-Roche-Magnus): α = (a·T)/(b + T) + ln(RH/100), where a = 17.27 and b = 237.7°C are empirical constants. Dew point Td = (b·α) / (a − α). Derived from the Clausius-Clapeyron relation describing how saturation vapour pressure changes with temperature. The constants are fitted to match measured vapour pressure data.
Why dew point > air temperature is impossible: 100% RH means dew point equals air temperature. Higher dew point than air temperature would imply RH > 100%, which is the supersaturated unstable state that immediately condenses. So dew point is always ≤ air temperature, equal only at fog/dew formation conditions.
Comfort interpretation: dew point below 10°C - dry, comfortable. 10-15°C - comfortable. 15-18°C - somewhat humid but tolerable. 18-21°C - sticky, noticeable discomfort. 21-24°C - oppressive, very humid. Above 24°C - extremely uncomfortable, hard to function outdoors. Indian coastal monsoon dew points routinely exceed 24°C. Air-conditioned spaces typically maintain 15-18°C dew points; reducing room dew point is one reason AC feels so much better than just fans (fans don't reduce humidity).
Oppressive. Sweat doesn't evaporate well. Combined with 32°C air, heat index reaches 42°C. This is why Mumbai summers are notoriously uncomfortable - high dew point, not just high temperature.
Comfortable dew point despite 42°C temperature. Dry heat is more tolerable than humid heat at lower temperatures. Sweat evaporates effectively, providing cooling.
Slightly humid but tolerable. Combined with Bangalore's moderate temperatures, monsoon feels pleasant. Air conditioning rarely needed in homes - natural ventilation suffices.
RH depends on temperature - 50% RH at 30°C feels much more humid than 50% RH at 5°C. Dew point is absolute - it directly tells you how 'sticky' the air is.
Below 50°F (10°C): dry. 50-60°F: comfortable. 60-65°F: noticeable. 65-70°F: sticky. Above 70°F (21°C): oppressive.
Glass surface goes below the air's dew point - water from air condenses on it. Higher humidity means it happens at warmer surface temperatures.
Approximation - accurate to <0.4°C for temperatures −40°C to +50°C and RH 1-100%. Good enough for any weather application.
Date math, password generation, QR codes, IP subnets, base64 encoding, dew point, dice rolls, age calculations - none of these are 'big' problems individually, but they are the small frictions that interrupt your day. This tool runs entirely in your browser, has no popup, no chat widget and no tracking inside the calculation, so you can finish the task and move on.
Many tools in the Daily Utilities category complement each other - date difference + day counter + day-of-the-week, or password generator + QR code + base64 encoder. The related-tool grid links them together so you can move between adjacent problems in a click.
The Dew Point Calculator is part of the Daily Utilities suite on Online Calculator Tools, alongside 6 related calculators. All tools share the same UI patterns, the same privacy-first rendering (nothing is sent to a server), and the same commitment to showing the formula and assumptions behind every result.