SUMMARY
The weight of a 100lb man varies significantly based on his location relative to the Earth's center and atmosphere. Using Gauss's law for gravity, the weight can be calculated at various depths and heights. At the Earth's core, the man would experience zero weight due to equal gravitational pull from all directions. As he ascends through the atmosphere, his weight decreases gradually, with specific weights at various altitudes: 99.5lb at the top of the troposphere (10 miles), 98.5lb at the stratosphere (30 miles), 97lb at the mesosphere (55 miles), 82.5lb at the ionosphere (400 miles), and 70lb at the exosphere (800 miles).
PREREQUISITES
- Understanding of Gauss's law for gravity
- Basic knowledge of gravitational force and buoyancy
- Familiarity with weight calculations in physics
- Concept of Earth's layers and atmosphere
NEXT STEPS
- Research the application of Gauss's law in gravitational calculations
- Study the effects of altitude on gravitational force
- Explore buoyancy effects on weight in different mediums
- Learn about the Earth's atmospheric layers and their characteristics
USEFUL FOR
Physics students, educators, meteorologists, and anyone interested in gravitational effects and atmospheric science.