SUMMARY
The Moon's gravity does affect atmospheric tides, but its impact is significantly smaller than that of solar radiation. Analysis of barometric pressure data over time reveals tidal signatures corresponding to both solar and lunar influences, with the lunar contribution being approximately 1/20th that of the solar effect. Fourier analysis is essential for distinguishing these contributions, as it allows for the identification of driving forces that are only 1-2% of the dominant solar heating effect. The largest amplitude observed is from solar heating, with distinct lunar diurnal and semidiurnal peaks also present.
PREREQUISITES
- Understanding of Fourier transforms and their application in data analysis
- Familiarity with barometric pressure measurement techniques
- Knowledge of atmospheric dynamics and tidal theory
- Basic grasp of solar and lunar influences on Earth's atmosphere
NEXT STEPS
- Learn how to perform Fourier transforms on time series data using Python or MATLAB
- Research the effects of solar radiation on atmospheric tides
- Study the dynamics of atmospheric tides in detail through MIT OpenCourseWare resources
- Explore historical barometric pressure datasets for tidal analysis
USEFUL FOR
Atmospheric scientists, meteorologists, data analysts, and anyone interested in the interaction between celestial bodies and Earth's atmospheric dynamics.