11.3
The use of GPS signals to estimate turbulence intensity in the troposphere and stratosphere
The theoretical underpinnings for this problem are taken from weak-scattering theory for electromagnetic wave propagation in random media. These techniques are modified to deal with a transmitter and receiver moving relative to each other, as well as considering the more realistic situation of a defined patch of turbulence. The standard approaches in the literature are based upon space-filling turbulence (i.e., between the transmitter and receiver), or an infinitely thin screen. A simulation method is then used to evaluate the performance of estimators to calculate the intensity and location of the turbulence. Results from real GPS-COSMIC links will be presented to show that the methodology works with real-world data.