Atmospheric pressure is the force exerted by the weight of the air in Earth's atmosphere. At sea level, this pressure is approximately 101,325 pascals (Pa) or 14.7 psi. Such pressure results from the densely packed molecules, primarily nitrogen and oxygen, that make up our atmosphere.
This dense molecular packing enables numerous life-supporting activities, such as breathing and weather systems. However, when compared to the near-vacuum of interplanetary space, this pressure is immense. The huge difference in pressure explains why the thin fabric of interplanetary regions is considered a vacuum. In essence, interplanetary space lacks the atmospheric molecules that are abundant at sea level, providing a nearly resistance-free path for celestial phenomena to occur.
- Key Role: It affects weather systems and flight dynamics on Earth.
- Comparison: Helps explain the difficulties and considerations in space travel and satellite launching.