SUMMARY
The discussion focuses on calculating the distance from a storm based on the dispersion relation for long-wavelength surface waves in deep water, specifically using the equation ω=(gk)^(1/2). Waves generated by a storm with a 15-second period arrive at the British coast, and by the next day, the period decreases to 13 seconds. The group velocity is defined as v=(1/2)(g/k)^(1/2), and the time delay between the two wave periods is one day, which is crucial for determining the distance from the storm.
PREREQUISITES
- Understanding of wave mechanics and dispersion relations
- Familiarity with the concepts of group velocity and phase velocity
- Knowledge of the gravitational constant (g) and wave number (k)
- Basic algebra for solving equations involving time and distance
NEXT STEPS
- Calculate the group velocity for different wave periods using v=(1/2)(g/k)^(1/2)
- Explore the implications of wave dispersion in oceanography
- Study the effects of storm distance on wave period changes
- Investigate numerical methods for solving wave propagation problems
USEFUL FOR
Students studying physics, particularly those focusing on wave mechanics, oceanographers analyzing storm impacts, and researchers in fluid dynamics.