The influence of jet regime on the frequency and distribution of extreme events

Harnik N., 2014: Extreme upper level cyclonic vorticity events in relation to the Southern Hemisphere jet stream. Under revision in Geoph. Reas. Let.  

Understanding how the large scale atmospheric circulation affects the distribution of extreme weather events is clearly important.  Intuitively, we expect the distribution of extreme events to be linked to the large scale flow. In particular, we expect quantities like wind speed  and vorticity to be directly related to the structure of the jet streams and synoptic storms. In particular, we expect the distribution of extreme events to be related differently to the jet under different jet regimes. Since the Southern Hemisphere jet stream undergoes a sharp seasonal transition, from a  dominantly thermally driven subtropical jet during winter, to an eddy driven mid latitude jet during summer [e.g Nakamura et al., 2004], we expect the distribution of extreme events to also vary seasonally. Here we examine extreme values of upper level cyclonic vorticity. We expect this quantity to be more strongly affected by the large scale circulation compared to the more traditional fields used for studying extreme weather events (e.g. surface temperature or precipitation), but at the same time we expect it to be indicative of extreme weather. We  expect extreme vorticity values to be associated with a deep upper level trough, and with  wave breaking and the formation of potential vorticity (PV) streamers, both of which have  been shown to play a role in the formation of extreme weather conditions (e.g. extreme precipitation [Martius et al., 1006, 2013; Romero et al., 1999; Jacobeit , 1987; Krichak et al., 2007; Massacand et al., 1998], Brazilian cold surges [Sprenger et al., 2012]).

 

We are currently writing a book chapter on the relation of extreme events to the jet stream and storm tracks, in which we will describe this relation in the MQG model, in an idealized GCM and in observations.

Harnik N., O. Lachmy, and Chaim GarfinkelThe Influence of Storm Tracks and Jet Stream Dynamics on the Occurrence of Large-Scale Flow Anomalies and Extreme Weather and Climate Conditions’. In, Dynamics and Predictability of Large-Scale, High-Impact Weather and Climate Events. Ed. Li, J., R. Swinbank, H. Volkert and R. Grotjahn. Cambridge University Press