Hi all,
I am facing a quite weird behaviour while trying to convert osculating to mean orbits using DSST. For a given osculating orbit (LEO one), I propagate it numerically using a geopotential only force model with a given time step (1 minute) over roughly one orbital period (2h) and convert each osculating state into mean using the same degree/order for the geopotential.
I was expecting to get a very approximate result in each case (the force model being the same between the osculating propagated orbit and the mean one). This is not the case (cf. below) and more annoyingly, increasing the degree/order seems to worsen the mean semi major-axis (less flat for 16x16 than for 2x2). Does this mean that DSST reduction is less efficient for high geopotential degree/order ?
Please find attached the code which generated the plots.
Thanks in advance for your feedback.
François

