north atlantic eddy-driven jet and circulation patterns: structures, preferred paths and transitions...
DESCRIPTION
The NAO essentially describes variations in the latitude of the North Atlantic eddy-driven jet. The North Atlantic region is special: split of the jet. Woollings et al (2009) J. Clim.TRANSCRIPT
North Atlantic eddy-driven jet and circulation patterns: Structures, preferred paths and transitions
Abdel Hannachi
Department of Meteorology
1. Background
2. Jet positions and circulation patterns
3. Preferred paths and transitions
4. Summary
Tim Woollings & Brian Hoskins
Background
Linearity + random noise normality of the PDF Observed large scale flow is non-normal
Non-Gaussian grid points (1%) of NH winter SLP
NH winter MSLP skewness
Rennert & Wallace, J. Clim, 2009
Hannachiet al (2009)J. Clim.
Origin: (i) Nonlinearity/regime behaviour; (ii) Multiplicative noise; (iii) Cross-frequency coupling
• The NAO essentially describes variations in the latitude of the North Atlantic eddy-driven jet.
• The North Atlantic region is special: split of the jet.
Woollingset al (2009)J. Clim.
4
Variation/persistence of the jet latitude with time(0-60W, 925-700mb)
(Woollings et al. 2010, QJ)
• Much of extratropical weather/climate variability is associated with jet stream.
• Link between jet stream and circulation patterns (regimes).
• Importance for climate change effect on large scale flow
(ERA40)
5
Z500 anomaly pattern associated with the preferred jet locations -NAO
~+EA
~-EA
PDF of North Atlantic jet latitude (three modes)
Jet positions and circulation regimes
Greenland blocking
Jet preferred locations
The leading two/three EOFs of ERA40 Z500 are used Skewness is interpreted via the mixture model of the PDF
K: is estimated using arguments from order statistics Other parameters are estimated using the EM algorithm
)μ(xΣ)μ(x
21exp
|Σ|1α)(2=f(x) k
1k
Tk
K
1=k1/2
kk
d/2
number of components
proportions covariancescentres
Circulation regimes
7
Scatter plot within EOFs 1 and 2 and the three component mixture model(colours refer to latitude anomalies)
Only three components are found Very good agreement between the regime centres and jet
composites and between covariances and jet latitudes
Preferred paths and transition probabilities
• Growth/decay and preferred paths in state space are studied via the mixture model using the extended data (delay space).
),...,,( 11x Mtttt xxx
Embedding dimension
• A regime centroid becomes a trunk of a trajectory (length M)
We get the most persistent regimes :3KFor
:3KFor We start getting preferred paths Between regimes in state space
Preferred paths
Day 1 105
15
30
20 25
35 40
Sequence of the fourthregime centroid in a mixture with K=4, and delay parameter of 40 days
Preferred path towards GB regime (southern jet position)
Z500, contour interval 10 m
Transition path (GB) and wave-breaking
Blocking index: reversal in on PV2 surface φθ
Day 1 5 10
15 20 25
30 35 40Mean state of blocking index (delay space) associated with transition path toward WB
B = north - south
Example: on PV2 surface for 20 Jan – 28 Feb 1986 θ
24/120/1 29/1
3/2 8/2 13/2
18/2 23/2 28/2
Ko
Transition probability)Rin wasx|Rin Pr(xp i1tjtij Transition probability:
Computed using the mixture model:
)μ,Σ,(x)gμ,Σ,(xgα)x,h(x kktkkk1t
K
1kkk1tt
Multivariate normal
Probability model: no need to classify each datum
C
S N38% 28%
32%
55%
52%
51%
C
S N30%
32%
42%
51%
38%36%
Two EOFs Three EOFs
Summary
• Non-normality of large scale flow
• Importance of jet stream in much of extratropical weather/climate variability
• Latitudinal position of the NA jet: trimodal (N, S, C)
• Very good agreement with regimes from mixture model: N/-EA; C/+EA; S/-NAO/GB
• Mixture model with the delay space: preferred paths. Path to S: wave breaking
• Transition: S C N N S: through baroclinic instability