The principle of barometric levelling is based on the relationship between atmospheric pressure and elevation. As one ascends in altitude, the atmospheric pressure decreases. This is because the weight of the air above a given point decreases as the altitude increases. Therefore, the correct description of this relationship is that atmospheric pressure varies inversely with height.
Let's consider the options provided:
- Atmospheric pressure varies inversely with height
- Atmospheric pressure varies proportionately with height
- Atmospheric pressure varies constantly with height
- Atmospheric pressure is zero throughout
The correct option is the first one:
Atmospheric pressure varies inversely with height. This means as height increases, atmospheric pressure decreases.