Question

Why is it that with an increase in temperature of the air, the relative humidity will decrease even if the moisture content remains the same?

Answer 1

HintRelative Humidity is the measure of water fume noticeable all around as a level of the aggregate sum that could be held at its ebb and flow temperature. Warm air can hold more dampness than cold air implying that the overall mugginess of cold air would be higher than the warm air if their supreme moistness levels are equivalent.

Complete step-by-step solutionThe relative humidity is the proportion of the measure of water fume present in the climate and the most extreme measure of water vapor the atmosphere can hold. This is because colder air doesn't need as much dampness to get immersed as hotter air. On the off chance that the water fume content remains the equivalent and the temperature drops, the general moistness increments. If the water fume content remains the equivalent and the temperature rises, the overall moistness diminishes. As the temperature expands the capacity of air to hold more water fume (in the too warmed state) is higher, so on the off chance that we have an airstream with a fixed measure of water fume in it, on the off chance that we increment the temperature, the proportion between the fixed measure of atoms of water fume in the stream to the maximum number of particles that a be found is lower in the second case as the denominator gets higher.

NoteLiquid water occurs when H2O particles are fortified firmly. At the point when the air temperature is warm, those H2O atoms are exceptionally dynamic and it is hard for them to become/remain reinforced. This will make the rate of evaporation to increase (liquid water to fume) and condensation to decrease (vapor to liquid water).