Method for compensating boresight error in low earth orbit satellite antenna

A method for compensating a boresight error in a low earth orbit (LEO) satellite antenna by considering a nonhomogeneous propagation environment due to a meteorological condition on a path of an electromagnetic wave reaching a ground station from the antenna of a moving LEO satellite, the method comprises the steps of:

• a) converting a communication point of the LEO satellite and the location of the ground station into the geocentric coordinate system, and setting an incidence angle of the electromagnetic wave radiated from the LEO satellite antenna;
• b) calculating a meteorological condition at a specific altitude interval by applying a specific formula to a measured meteorological condition;
• c) calculating the calculated meteorological condition at a specific altitude interval as an effective refractive index at a specific altitude interval;
• d) dividing the atmosphere into layers at the specific altitude intervals, and calculating an arrival coordinate of the electromagnetic wave for which the atmospheric environment is considered by using the calculated effective refractive index and a specific technique;
• e) calculating an error between the location of the ground station and the arrival coordinate of the electromagnetic wave as a zenith angle and an azimuth angle of the geocentric coordinate system;
• f) determining whether the error between the location of the ground station and the arrival coordinate of the electromagnetic wave is less than a target error or not, and when the error is not less than the target error, adding the error to the incidence angle of the electromagnetic wave and returning to step d);
• and
• g) in step f), when the error between the location of the ground station and the arrival coordinate of the electromagnetic wave is less than the target error, deciding a compensation angle for the incidence angle of the electromagnetic wave,
• wherein the specific formula in step b) is the Piecewise Cubic Hermite Interpolating Polynomial (PCHIP), and
• wherein, in step c), the effective refractive index is calculated by applying a Millimeter-wave Propagation Model (MPM) to the meteorological data which is calculated by applying a two-dimensional interpolation method to the meteorological data at a specific altitude interval (h0, h1, . . . hn).