Radio frequency principles form the foundation of GPS operation. Satellites broadcast precise time signals and orbital information through electromagnetic waves. Receivers calculate their position by measuring the time delay between signal transmission and reception from multiple satellites.
The GPS signal evolution spans several decades of technological advancement. Modern signals incorporate enhanced features for improved accuracy and reliability. Current systems transmit multiple signal types across different frequency bands to serve various applications and user needs.
GPS signals function through a complex network of 24 operational satellites orbiting Earth. Each satellite transmits radio signals at specific frequencies. These signals contain precise time data and satellite position information.
Radio waves from GPS satellites travel at 299,792,458 meters per second through space. The signals reach Earth's surface at significantly reduced power levels of approximately -160 decibel-watts. Ground-based receivers capture these weak signals to calculate position.
Satellite signals travel through multiple atmospheric layers. The ionosphere affects signal propagation between 60-1000 kilometers above Earth. The troposphere impacts signals in the lower 8-13 kilometers of atmosphere.
Signal Components
- Carrier waves at L1 (1575.42 MHz) and L2 (1227.60 MHz) frequencies
- Navigation message with satellite ephemeris data
- Timing codes for distance measurement
- Signal strength indicators for accuracy assessment