What is moisture?
Moisture table is a type of graph that compile data regarding temperature to humidity. The transformer of humidity can have more than one form and can contain different types of data. One type refers to the air temperature and the temperature of the wet bulb to be relative humidity. Another type of indices of the moisture table of relative humidity and temperature to provide absolute humidity and dew point.
The first type of humidity table compares the air temperature or the dry bulb temperature and the wet bulb temperature. It is located by taking the air temperature with the thermometer that has its bulb, usually by wrapping in a thin layer of wet fabric. This temperature reflects the humidity in the air. The effect is similar to what happens when human sweats, so the air feels cooler. The wet bulb temperature is always lower if the relative humidity is not maximum or 100%.
Some graphs use air temperature and wet bulb temperature, which refers to finding TON relative humidity. Some other versions of this chart useWhat is called the depression of wet bulbs, which is the difference between the actual air temperature and the wet bulb temperature. Two types of graphs differ in that they use two ways of expressing the same value.
The second type of moisture table uses data from the first chart. The air temperature is crossed with relative humidity and the graph gives absolute humidity and point of dew. Absolute moisture is given as the actual amount of water vapor in the air, expressed as a grams of water per cubic meter (g/m 3 ). The dew point is the temperature at which Rosa begins to form at a given relative humidity.
graphs of this type may vary in used units and layouts, but all are used in the same way. Graphs for Fahrenheit and Celsius can be used depending on the page in which they are read. Some graphs can combine both measuring systems. It is assumed that most VL tablesThe nurses are calibrated for standard atmospheric pressure on the sea level. In some cases, more detailed graphs are used for higher altitudes or take into account changes in atmospheric pressure.