The present invention proposes a method and
system for inverting the height distribution of
gravity wave disturbance quantity parameters at the top of the
mesosphere. The present invention constructs an
event sequence and height sequence of multiple meteors, and constructs a corresponding
data matrix and drift matrix according to the parameter set of each event; the top of the
mesosphere is equidistantly divided into multiple height intervals, and each meteor event is placed therein; in each height interval, the
data matrix and drift matrix corresponding to all meteor events in the interval are sequentially connected in series to construct a corresponding joint
data matrix and joint drift matrix; in each height interval, according to the corresponding two joint matrices, the corresponding
gravity wave disturbance quantity parameter matrix is obtained by the
least squares method; all
gravity wave disturbance quantity parameter matrices are sequentially connected in series to obtain their height distribution. The height distribution of gravity
wave disturbance quantity parameters at the top of the
mesosphere can be used to quantitatively analyze the changes in gravity
waves and solve the dynamic effects of gravity
waves on the background
atmosphere. The present invention can be widely used in space
physics related industries.