Applications
- calculating the moisture content when heating air by a specific number of degrees Celsius.
- calculating the temperature at which condensation occurs.
- calculating the humidity deficit at a specific temperature (increase).
- converting a given temperature of humidity deficit to relative humidity and vice versa.
- calculating the final composition of the air after mixing air of 2 different compositions.
Explanation of KlimaCalc and climate properties
When 2 of the 7 climate properties listed below are known, the other climate conditions can be calculated!
Temperature [ °C ]
The temperature (dry bulb) of the environment’s air, measured with a thermometer, psychrometer or electronic meter.
Wet bulb temperature [ °C ]
The temperature of the air, measured with a psychrometer or dry/wet bulb meter. The wet bulb temperature is the lowest temperature achieved by air when so much water has evaporated that the air is saturated.
Dew point [ °C ]
The dew point is the temperature of the air at which condensation occurs.
Energy content [ kJ/kg ]
The energy content of the humid air is also known as the heat content or enthalpy, expressed in kJ/kg. This energy content of humid air can be considered a function of the temperature AND the moisture content of the air. An example of the energy content:
- air at 25.0°C with a high energy content feels clammy and sticky.
- air at 25.0°C with a low energy content feels dry and pleasant.
Relative humidity [ % ]
The relative humidity is the ratio between the prevailing vapour pressure (the actual quantity of moisture in the air, also called the absolute moisture content) and the maximal vapour pressure at the same temperature and air pressure. Vapour pressure is given in %. When the relative air humidity reaches 100%, the invisible water vapour in the air precipitates as drops on colder surfaces.
Mixing ratio [ g/kg ]
The mixing ratio is defined as the number of grams of water vapour found in a kilogram of dry air, or the prevailing vapour pressure. The maximum moisture content depends on the temperature and increases with rising temperature (warm air can hold more moisture than cold air).
Humidity deficit [ g/kg ]
The humidity deficit is the number of grams of moisture that can be added to 1 kilogram of air to bring it up to saturation (RH 100%). Saturated air therefore has a humidity deficit of 0 g/kg and cannot absorb any more water. The drier the air, the higher its humidity deficit.
We do not host Sercom KlimaCalc on our servers. We did not scan it for viruses, adware, spyware or other type of malware. This app is hosted by Galad and passed their terms and conditions to be listed there. We recommend caution when installing it.
The APK Download link for Sercom KlimaCalc is provided to you by apps112.com without any warranties, representations or guarantees of any kind, so access it at your own risk.
If you have questions regarding this particular app contact the publisher directly. For questions about the functionalities of apps112.com contact us.
|
| ||||
| Downloads: 21 | ||||
| Updated At: 2024-04-23 09:49:19 | ||||
| Publisher: Edward de Ridder | ||||
| Operating System: Android | ||||
| License Type: Free |