Course 1.3Lesson 3 of 3
Humidity is the amount of water vapour in the air, and relative humidity compares it with the most that the air can hold at that temperature. When the humidity is high, evaporation is slow, so sweat and wet clothes dry slowly, and we feel hotter because the body cannot lose heat. Warm air can hold more vapour than cool air. An evaporative cooler works well in dry weather and poorly in humid places. Evaporation and condensation drive the water cycle: water evaporates, the vapour condenses into clouds, and the drops fall as rain.
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On a dry, hot day at , sweat evaporates quickly and we feel less hot. On a humid day at the same temperature, the same sweat stays on the skin and we feel sticky and hotter. The reason is the humidity.
Humidity is the amount of water vapour in the air. The air can hold only a certain amount of water vapour at a given temperature. When the air is close to that limit, it is very humid, and very little more water can evaporate into it.
Weather reports give the relative humidity as a percentage. It compares the water vapour that is in the air with the most that the air can hold at that temperature.
Warm air can hold more water vapour than cool air. This is why the same amount of vapour can make a cold evening feel damp (the percentage is high) and a warm afternoon feel dry (the percentage is low). It is also why dew forms at night. The air cools and can hold less vapour, so the extra vapour condenses on the grass and on cold things, such as a glass of cold water.
You should find that air at with of vapour in each cubic metre is quite dry, yet it forms dew if it cools below about .
The Sun warms the surface of the oceans, rivers and lakes, and water evaporates. The vapour rises. In the cold air above, it condenses into tiny drops of water, and forms clouds. When the drops become large, they fall as rain. This is the water cycle. Evaporation and condensation are the two changes of state that drive it.
Plants add to it too. They take water from the soil, and a large part evaporates from the leaves in a process called transpiration. A big tree can send hundreds of litres of water into the air in one day.
A good example of the cycle in a small place: heat water in a closed jar with a cold lid. The water evaporates, and the vapour condenses on the cold lid as drops, which fall back like rain.
The program follows the air outside after sunset, as it cools while its vapour stays the same.
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