Raw observation arrays are read for the target location and fitted, by least squares, to the trend component of a synthesised wave, so the projection is anchored to what actually happened rather than extrapolated from nothing.
Additional measured signals — surface pressure, dew-point spread and wind — are normalised and folded in as phased contributions with fixed relative weight.
Variance is damped in proportion to how far the projection has stretched from the last real observation, so confidence falls with distance instead of staying flat.
A held window is applied and the projection is collapsed to a single peak date, peak value and confidence figure.
Matched analog years are selected on strength and timing and cross-weighted against the projection.