Theories of Blocking

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Theories of Blocking Brian Hoskins B. Bolin (1949) in Beggren et al, Tellus 1

description

Theories of Blocking. Brian Hoskins. B. Bolin (1949) in Beggren et al, Tellus 1. What is a block?. Chicago School 1940s Rossby, Bolin, Rex. A block for the westerlies with their weather systems. H. H. Z 500. L. L. A block for the westerlies with their weather systems. +. +. - PowerPoint PPT Presentation

Transcript of Theories of Blocking

Page 1: Theories of Blocking

Theories of BlockingBrian Hoskins

B. Bolin (1949) in Beggren et al, Tellus 1

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What is a block?

Chicago School 1940sRossby, Bolin, Rex

A block for the westerlies with their weather systems

H

L

H

L

Z500

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A block for the westerlies with their weather systems

+

-

+

-

PV on θ

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A block for the westerlies with their weather systems

W

C

W

C

θ on PV2

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Some Theories

•Hydraulic jump, Rossby

•State with amplified Rossby wave ridge e.g Charney & Devore (1979) Mulitiple equilibria in the presence of topography

•Self-stabilisation of a vortex dipole in a westerly flowe.g. Modon (McWilliams, 1980, 1981)

•Soliton

•Instability of a basic wavy westerly flowe.g Frederiksen (1982)

W

C

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Transient eddy feedbacks

Hoskins, James & White (1983)

Shutts (1983)eddy straining

W

C

PV inversion, e.g. HMR (1985)

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Group velocity considerations

•Wave activity leakage, e.g. On uniform westerly flow , U,barotropic stationary waves exist & have eastward group velocity 2U

•Modons constructed by McWilliams on equivalent barotropic westerly flow for which stationary waves do not exist.

•Swanson (2001,2) considered an equivalent barotropic atmosphere with 2 regions of uniform PV separated by a discontinuity:

Possibility of R waves with zero group velocity & phase speed

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Swanson 2002Initial value problem

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Onset

B = north - south

Pelly & H (2003)Tyrlis & H (2008)θ on PV2

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Central latitude: Line of latitude (Tibaldi & Monteni, 1990), mean jet or storm-track latitude (x) (Pelly & H, 2003)

or 2-D e.g. Berrisford et al (2007) for SH, Woollings et al (2008) for NH

Reinforcement By interaction with subsequent weather systemsDrip feed or big meal?

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Importance of diabatic processes?

Erosion of blocking high by radiative damping ~ 1 weekErosion of cut-off low by latent heat release ~ days

Anchoring by underlying surface?

Importance of ambient planetary waves & forcing of them e.g. Rockies but also anomalous SSTs, sea ice,....

How non-linear is the behaviour of blocking? persistence Masato et al (2009)frequency of occurrence Scaife et al (2010)