Figure 4
From: Characterizing the dynamics of multi-scale global high impact weather events
Vertical structure of the EFD mode \(\psi ^{(0)}_{v,q}(\varvec{x},t=144)\) at \(122^\circ\) W over West Coast of the Continental US for the Jan 2021 event (Left) and the Mar 2005 event (Right) emphasized the subtle volumetric variations provided by EFD. The scale of the vertical measurements has been exaggerated by a factor of 10 for visibility. Units for pressure are hPa. EFD scale is unitless.
