Updated October 2026
These three problems cover the three ways this calculator's "second known value" dropdown can be used — RH, dew point, and wet-bulb — each worked fully by hand using the exact formulas behind the tool, so you can check your own work or follow the method step by step.
Given: Tdb = 25°C, RH = 50%, P = 101.325 kPa.
es(25) = 0.61078 × exp(17.27×25/262.3) ≈ 3.17 kPa.e = 0.50 × 3.17 = 1.58 kPa.W = 0.622 × 1.58 / (101.325−1.58) ≈ 0.00988 kg/kg (9.88 g/kg).ln(1.58/0.61078) = 0.950; Tdp = 237.3×0.950/(17.27−0.950) ≈ 13.9°C.Twb ≈ 18.0°C.h = 1.006×25 + 0.00988×(2501+1.86×25) ≈ 50.3 kJ/kg.v = 0.287×298.15×(1+1.6078×0.00988)/101.325 ≈ 0.858 m³/kg.Given: Tdb = 30°C, Tdp = 15°C, P = 101.325 kPa.
es(30) ≈ 4.24 kPa (saturation at dry-bulb).e = es(15) ≈ 1.71 kPa (dew point's own saturation value is the actual vapor pressure, by definition).e/es(Tdb) = 1.71/4.24 ≈ 40.2%.W = 0.622×1.71/(101.325−1.71) ≈ 0.01065 kg/kg (10.65 g/kg).h = 1.006×30 + 0.01065×(2501+1.86×30) ≈ 57.4 kJ/kg.Given: Tdb = 35°C, Twb = 24°C, P = 101.325 kPa.
e = es(24) − 0.000662×P×(Tdb−Twb).es(24) ≈ 2.98 kPa; correction term 0.000662×101.325×11 ≈ 0.74 kPa.e = 2.98 − 0.74 = 2.25 kPa.es(35) ≈ 5.63 kPa.2.25/5.63 ≈ 40.0%.Notice this is the reverse direction from the normal bisection case — when wet-bulb is already known, the psychrometer equation can be solved directly for e with no iteration required, because Twb is no longer the unknown.
Enter each example's given values into the calculator directly and confirm the outputs match — this is the fastest way to validate hand calculations for an exam or a homework set, and to build intuition for which direction each formula needs to be solved.