Here's the osculating inclination before and after the maneuver.
The variation of the inclination during one orbit is caused by the Earth's flattening.
Δi:
deg (variation of the osculating inclination).
The J2000 ISS state contained in the NASA data file is converted to the TEME reference frame, then the osculating inclination is calculated. The inclination shown in the graph, therefore, is to the true (instantaneous) equator.
The graph shows the 1-orbit averaged radius vector (or semi-major axis) and orbital speed.
ΔV =
m/s
Δsma =
m (variation of the semi-major axis)
Here are the perigee and apogee radius vector.
For any given TLE, the program calculates the ISS orbital period
T. Then the smallest and the biggest radius vector is found from the TLE epoch minus
T/2 to the TLE epoch plus
T/2.
Δperigee:
m
Δapogee:
m