SLIDE 20 Á.G. Muñoz
H
SAM
L L H
ENSO AMM SAD MJO SACZ
Seasonal drivers Sub-seasonal drivers
Different drivers interacting at different temporal and spatial scales, but their impacts are represented by only 6 weather types Could the WT contain all the information needed to make good forecasts of extreme events?
Interactions
- Meridionally propagating Rossby
waves during El Niño modulate SAM (Silvestri & Vera, 2003)
- This causes anomalous circulations in
SSA and modifies SST patterns in the Southern Atlantic through wind- evaporation-SST feedbacks (Zhou & Carton, 1998).
- It has been shown (Foltz & McPhaden,
2010) that ENSO and AMM can interact through wind-forced equatorial Kelvin and Rossby waves.
- AMM tend to produce meridionally
propagatin Rossby waves extending into South Atlantic (Trzaska et al., 2007), inducing a counterclockwise migration of SST which is consistent with SAD (Nnamchi et al., 2011).
- MJO, SACZ (and SALLJ) also interact
with each other and are modulated by large-scale drivers (Muza et al., 2009; Carvalho et al., 2010). Vertically-integrated moisture advection Rainfall patterns
(3 Examples)
WT4 WT5 WT6 WT4 WT5 WT6 Muñoz et al., 2015
Putting the pieces together
Weather Typing as Tool for Tropical-Extratropical Interactions