Research Article
Study on the Precursor Signal Capturing of Unfavorable Weather: Months/Years in Advance to Ultra-Early Forecast for Hourly Transient Weather Changes during the Beijing Winter Olympics
Figure 5
(a) Hourly distribution of PLAM index and height of mixing layer (H_PML) in Beijing in February 2021, (b) distribution of perturbed daily oscillation variation minimum of H_PML and (c) hourly wet potential temperature variation (δΘe) and the distribution of atmospheric supersaturation (S).