One notable observation from the data is that the relationship between relative humidity and humidity values shows variability, especially with higher temperatures. For instance, at 82°F with 84% relative humidity, the absolute humidity is 22.6 g/m³, while at 88°F with a lower relative humidity of 70%, the absolute humidity is still 22.6 g/m³, yet it corresponds to a much higher saturation amount, indicating that warmer air can hold more moisture than cooler air. This emphasizes the importance of temperature in determining moisture capacity and highlights the differences in how relative humidity affects absolute humidity at different temperatures.
Temperature (°F)
Relative Humidity
Humidity (g/m^3)
Saturation Amount (g/m^3)
82
84%
22.6
22.6 / (0.84) = 26.9
79
94%
23.0
23.0 / (0.94) = 24.5
81
89%
23.2
23.2 / (0.89) = 27.0
84
84%
24.0
24.0 / (0.84) = 28.6
88
70%
22.6
22.6 / (0.7) = 32.3
90
62%
21.2
21.2 / (0.62) = 34.2
86
70%
21.3
21.3 / (0.7) = 30.4
77
100%
23.0
23.0 / (1) = 23.0
80
62%
15.7
15.7 / (0.62) = 25.3
89
83%
27.6
27.6 / (0.83) = 33.3
what is one thing that stands out
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