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Convert to absolute humidity
101,325 kPa at sea level, 89,87 kPa at 1000 m above sea levelAbsolute Humidity Calculator (Celcius)
Absolute Humidity Calculator (Fahrenheit)
Convert to relative humidity
101,325 kPa at sea level, 89,87 kPa at 1000 m above sea levelRelative Humidity Calculator (Celcius)
Relative Humidity Calculator (Fahrenheit)
The Absolute Humidity Calculator
Discover the practicality of our tool doing the conversion of relative humidity to absolute humidity and vice versa. Experience the convenience of obtaining precise conversions effortlessly.
Information on the parameters needed to describe the amount of water in air;
Atmospheric Pressure (kPa)
Atmospheric pressure, measured in kilopascals (kPa), fluctuates with weather conditions. Higher pressure signifies stable, denser air, while lower pressure indicates lighter, rising air, often leading to cloud formation and wind. However, within the desiccant dehumidification industry, calculations typically consider nominal pressure, set at 101,325 kPa at sea level, irrespective of weather conditions.
Altitude plays a crucial role in pressure adjustments, significantly affecting air treatment processes. For instance, regions like parts of Nevada in the USA, Nairobi in Kenya, or Amman in Jordan, situated above 1000 meters altitude, witness notable alterations in flow-chart dynamics. Pre-coolers are commonly employed in dehumidification systems to reduce moisture levels before desiccant rotor drying. For instance, pre-cooling moist outdoor air to 10°C (50°F) at sea level yields an absolute water content of 7.6 g/kg (53.2 gr/lb). Conversely, at an altitude like Nairobi’s 1700 meters, with a nominal pressure of 82.5 kPa, pre-cooling to 10°C yields a reduced absolute water content of 9.4 g/kg (65.8 gr/lb). This impact can be verified using our calculator by adjusting the pressure, inputting 10°C or 50°F, and 100% RH, then clicking “Calculate.”
Table of atmospheric pressure at different altitudes;
- 200m
- 400m
- 600m
- 800m
- 1000m
- 1200m
- 1400m
- 1600m
- 1800m
- 2000m
- 98,95 kPa
- 96,61 kPa
- 94,32 kPa
- 92,08 kPa
- 89,87 kPa
- 87,72 kPa
- 85,60 kPa
- 83,52 kPa
- 81,49 kPa
- 79,50 kPa
Temperature Influence on Humidity Levels
Temperature, expressed in degrees Celsius (°C) or Fahrenheit (°F), is a fundamental parameter dictating air comfort levels. As temperature rises, air can retain more humidity in vapor form, as evidenced by increased moisture content (g/kg or gr/lb) at higher temperatures while maintaining the same relative humidity. This phenomenon stems from the accelerated movement of water molecules in warmer air, reducing their propensity to transition into a liquid phase.
Understanding Relative Humidity
Relative humidity (%RH) is a recognizable parameter affecting human comfort. Lower relative humidity facilitates rapid evaporation of sweat from the skin, aiding in cooling through evaporative processes. Conversely, higher relative humidity diminishes the effectiveness of this cooling mechanism. At 100% RH, water vapor transitions into liquid form, either condensing on cold surfaces or forming mist in the air. This parameter indicates the water partial pressure in the air relative to its saturation point, offering insights into moisture levels.
Absolute humidity (g/kg or gr/lb)
Absolute humidity (g/kg or gr/lb) quantifies the weight of water vapor present in the air relative to the weight of dry air. Unlike relative humidity, absolute humidity remains constant with temperature variations until the condensation threshold is reached. This stability makes it invaluable in air handling processes, facilitating accurate moisture control and condensation calculations.
Dew-point (°Cdp or °Fdp)
The dew-point (°Cdp or °Fdp) signifies the temperature at which air must be cooled to precipitate water vapor into liquid form. Similar to absolute humidity, the dew-point remains constant until reaching the condensation temperature. Maintaining the air’s dew-point below surface temperatures prevents condensation, crucial for various applications, including lithium battery manufacturing, where precise humidity control is paramount.
In conclusion, a thorough understanding of atmospheric parameters such as pressure, temperature, relative humidity, absolute humidity, and dew-point is essential for effective humidity management across diverse industrial and environmental settings. Utilizing tools like the Absolute Humidity Calculator streamlines this process, enabling precise conversions and informed decision-making in humidity control applications.
