The Role of North American Convective Storms on Jet Stream Dynamics: A Negative Potential Vorticity Perspective

Synoptic-scale filaments of negative potential vorticity (PV) in the northern hemisphere tropopause can form adjacent to the jet stream in the presence of convection and moderate shear (i.e., severe thunderstorm environments). Negative PV originates from strong vorticity in convective updrafts, driven by the horizontal gradient of diabatic heating (O < 10 km). Case-studies have shown that when negative PV grows onto synoptic-scales, it can influence in-situ jet stream dynamics and impinge on jet stream forecast skill.

Nevertheless, little is still known about the characteristics of synoptic-scale negative PV. How frequently is it observed? And what are its ‘typical’ impacts on the jet stream?

Focusing on North America where severe convection is frequent, we design an algorithm that tracks the temporal evolution of closed contours of upper-level, negative PV air using ERA5 data. We composites instances in which it is in close-proximity to (‘interacts with’) the jet stream and assess its dynamical response. The role of negative PV on jet evolution and its downstream response over the Atlantic is facilitated through a combination of lagged composite analysis and K-means clustering.

Our composite results in combination with preliminary high-resolution model simulations highlight the following conclusions. Synoptic-scale bands of negative PV frequently interact with the jet stream, intensify jet wind-speed maxima and can serve as an amplification source for Rossby Wave Packets.