We use the formula for the humidity ratio (\(W\)):
\[
W = 0.622 \times \frac{P_w}{P - P_w}
\]
Where:
- \(P_w\) is the partial pressure of water vapor,
- \(P\) is the total atmospheric pressure.
Given:
- Saturation pressure of water vapor \(P_{ws}\) at 37 °C = 6.28 kPa,
- Barometric pressure \(P\) = 101.32 kPa,
- Relative humidity (RH) = 50%.
The partial pressure of water vapor is:
\[
P_w = \text{RH} \times P_{ws} = 0.50 \times 6.28 = 3.14 \, \text{kPa}
\]
Now, substituting into the formula:
\[
W = 0.622 \times \frac{3.14}{101.32 - 3.14} = 0.622 \times \frac{3.14}{98.18} = 0.622 \times 0.032 = 0.020
\]
Thus, the humidity ratio is \(0.020 \, \text{kg water per kg dry air}\).