The gradient determines the color of the sunburst.
Determines the radial frequency; a value of 0 yields an attractive aurora.
Gives the angular disturbance; 0 gives individual layers.
Defines the speed of the sunburst; 2 doubles it, 0 prevents all movement.
Changes the appearance of the eruption; the higher the value, the more fragmented this region appears.
Defines where the eruption begins, as a percentage of the overall size.
Defines the width of the eruption region relative to the radius.