Initially the air is at a temperature of 35 °C at a relative humidity of 60%
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Then, we cool the air, and calculate the temperature at saturation (that is, the temperature at which the relative humidity is 1).
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We continue cooling along the saturation line until we reach 14 °C (in this process, water condenses out of the air).
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Now we heat the air until it reaches 24 °C.
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Hence the entire thermodynamic cycle can then be plotted.
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![route1 := pointplot([[T__1, hr__1], [T__2, hr__2]], connect = true, thickness = 4):](/view.aspx?SI=154017/8976a203e4a045cbddbdffae137cdf88.gif)
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