Absolute Humidity Calculator

Calculate absolute humidity from relative humidity and temperature, or vice versa

Calculate Absolute Humidity

Air temperature for humidity calculation

%

Percentage of maximum moisture air can hold

Humidity Calculation Results

60.0%
Relative Humidity
13.82
Absolute Humidity (g/m³)
Saturation Vapor Pressure
3.17 kPa
Actual Vapor Pressure
1.90 kPa
Temperature
298.1 K

Absolute Humidity Conversions

g/m³:13.822
kg/m³:0.013822
lb/ft³:0.000863
oz/ft³:0.013806

Formula: AH = (RH × Ps) / (Rw × T × 100)

Where: Rw = 461.5 J/(kg⋅K)

Comfort Level: Slightly Humid

Note: Still comfortable for most people

Slightly Humid: Still comfortable for most people

Relative Humidity Comfort Guidelines

0-30%Too Dry (Health issues)
30-50%Optimal (Most comfortable)
50-70%Acceptable (Slightly humid)
70-80%Humid (May feel sticky)
80-100%Very Humid (Uncomfortable)

Example Calculation

Typical Summer Conditions

Air Temperature: 32°C (89.6°F)

Relative Humidity: 60%

Location: Warm, humid climate

Step-by-Step Solution

1. T = 32°C = 305.15 K

2. Ps = 4,755 Pa (saturation vapor pressure)

3. Pa = 0.6 × 4,755 = 2,853 Pa

4. AH = (60 × 4,755) / (461.5 × 305.15 × 100)

5. AH = 20.28 g/m³

Types of Humidity

Absolute Humidity

Mass of water vapor per unit volume (g/m³)

Relative Humidity

Percentage of maximum moisture capacity (%)

Specific Humidity

Mass of water vapor per unit mass of air

Mixing Ratio

Mass of water vapor per unit mass of dry air

Physical Constants

Water vapor gas constant (Rw)461.5 J/(kg⋅K)
Critical temperature (Tc)647.096 K
Critical pressure (Pc)22.064 MPa
Standard temperature25°C (298.15 K)

Applications

HVAC system design and control

Weather forecasting and meteorology

Agricultural and greenhouse management

Industrial process control

Building moisture management

Understanding Absolute Humidity and Atmospheric Physics

What is Absolute Humidity?

Absolute humidity is the actual amount of water vapor present in a given volume of air, expressed as mass per unit volume (g/m³ or kg/m³). Unlike relative humidity, it doesn't depend on temperature and provides a direct measure of atmospheric moisture content.

Key Differences

  • Absolute Humidity: Temperature-independent, actual moisture
  • Relative Humidity: Temperature-dependent, percentage of capacity
  • Units: AH in g/m³, RH in percentage
  • Applications: AH for processes, RH for comfort

Mathematical Formulation

AH = (RH × Ps) / (Rw × T × 100)

RH = (AH × Rw × T × 100) / Ps

Ps = Pc × exp[(Tc/T) × Σ(ai × τⁱ)]

  • AH: Absolute humidity (kg/m³)
  • RH: Relative humidity (%)
  • Ps: Saturation vapor pressure (Pa)
  • Rw: Water vapor gas constant (461.5 J/(kg⋅K))
  • T: Temperature (K)
  • τ: Reduced temperature (1 - T/Tc)

Note: The Wagner-Pruss equation provides high accuracy for saturation vapor pressure calculations.