Jim Angell’s contributions to understanding the QBO

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Jim Angell’s contributions to Jim Angell’s contributions to understanding the QBO understanding the QBO

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Jim Angell’s contributions to understanding the QBO. Jim Angell’s contributions to understanding the QBO. Jim Angell’s contributions to understanding the QBO. QBO !. discovery of QBO. discovery of QBO. Angell and Korshover 1962, 1963. - PowerPoint PPT Presentation

Transcript of Jim Angell’s contributions to understanding the QBO

Page 1: Jim Angell’s contributions to understanding the QBO

Jim Angell’s contributions toJim Angell’s contributions tounderstanding the QBOunderstanding the QBO

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Jim Angell’s contributions toJim Angell’s contributions tounderstanding the QBOunderstanding the QBO

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Jim Angell’s contributions toJim Angell’s contributions tounderstanding the QBOunderstanding the QBO

QBO !

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discovery of QBO

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discovery of QBO

Angell andKorshover1962, 1963

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Meridional structure of QBOMeridional structure of QBO from Angell and Korshover, 1963 from Angell and Korshover, 1963

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Equatorial QBO derived fromEquatorial QBO derived from radiosondes and rockets radiosondes and rockets

Baldwin et al., 2001

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Schematic of global QBO

Baldwin et al., 2001

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Angell andKorshover (1964) coin the term‘Quasi-BiennialOscillation’

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Naming the QBO was not Naming the QBO was not easy...easy...

kind-of biennial oscillationalmost biennial oscillationnot quite biennial oscillationsomewhat biennial oscillationquasi-biennial oscillation

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50 hPatemps

noteout-of-phase

betweentropics and

midlats

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QBO temperature signal in lower QBO temperature signal in lower stratospherestratosphere

derived from regression with MSU4derived from regression with MSU4

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Snapshot of temperatures and meridional Snapshot of temperatures and meridional circulationcirculation

associated with the QBOassociated with the QBO

note extensioninto winter midlats

February1994

out-of-phasevertical structure

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Equatorial waves

and the QBO

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powerspectra

tropics

subtropics

midlats

strong peak at 10-15 days

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Idealized wave-mean flow interaction in QBO

Kelvin waves only propagatein background easterly winds

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zonal wind

eddypower spectra

Kelvin waves observed during easterly QBO winds

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QBO effects on ‘centers of action’

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Surface signal of QBOSurface signal of QBO

Baldwin et al., 2001

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Holton-Tan effect

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observations1964-1996

SKYHIsimulation(48 years)

Holton-Tan effect (composited QBO E-W)

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Meridional structure of QBOMeridional structure of QBO from Angell and Korshover, 1963 from Angell and Korshover, 1963

evidence ofHolton-Tan

effect

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Ozone QBO

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out of phasebetween tropicsand midlats

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totalinterannualvariability

QBOcomponent

Column ozone from TOMS

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Vertical structure of ozone QBO at equator

2-cellstructure

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QBO signal in nitrogen dioxide (NO2)

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QBO andstratosphericwater vapor

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stratosphericwater vapor

tropical tropopausetemperature

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QBO variations in stratospheric water QBO variations in stratospheric water vapor from HALOE satellite data, 1991-vapor from HALOE satellite data, 1991-20032003

Deseasonalizedanomalies

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Vertical propagation of QBO Vertical propagation of QBO anomaliesanomalies (interannual ‘tape recorder’) (interannual ‘tape recorder’)

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HALOE H2Oanomalies

tropicaltropopausetemperatureanomalies

Stratospheric H2O anomalies are consistent with tropical tropopause temperature changes

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Jim Angell’s contributions span all aspects of the QBO.

* global structure and propagation* ozone* equatorial waves* coupling with troposphere* tropopause and stratospheric H2O

Much of this original research is still relevant today!

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Happy Birthday Jim!

QBO