atmosfäärirõhul
Atmosfäärirõhul refers to the pressure exerted by the Earth's atmosphere at any given point. This pressure is essentially the weight of the air column above that point, extending all the way to the edge of space. Atmospheric pressure varies depending on altitude, temperature, and weather conditions.
At sea level, the average atmospheric pressure is approximately 101,325 Pascals (Pa), which is equivalent to
Temperature also plays a role. Warmer air is less dense than cooler air, leading to lower atmospheric
Weather systems are closely linked to atmospheric pressure. High-pressure systems are typically associated with stable, clear