The Arctic winter stratosphere in PAMIP atmosphere-only experiments Elisa Manzini ... · 2020. 2....

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Max-Planck-Institut für Meteorologie The Arctic winter stratosphere in PAMIP atmosphere-only experiments Elisa Manzini (Max-Planck-Institut für Meteorologie, Hamburg, Germay) Tido Semmler and Thomas Jung (Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany) Evangelos Tyrlis and Daniela Matei (Max-Planck-Institut für Meteorologie, Hamburg, Germany) Rosie Eade, Steve Hardiman and Doug Smith (Met Office Hadley Centre, Exeter, United Kingdom)

Transcript of The Arctic winter stratosphere in PAMIP atmosphere-only experiments Elisa Manzini ... · 2020. 2....

  • Max-Planck-Institut für Meteorologie

    The Arctic winter stratosphere in PAMIP atmosphere-only experiments

    Elisa Manzini (Max-Planck-Institut für Meteorologie, Hamburg, Germay)

    Tido Semmler and Thomas Jung (Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany)

    Evangelos Tyrlis and Daniela Matei(Max-Planck-Institut für Meteorologie, Hamburg, Germany)

    Rosie Eade, Steve Hardiman and Doug Smith (Met Office Hadley Centre, Exeter, United Kingdom)

  • Max-Planck-Institut für Meteorologie

    Response of the Arctic winter stratosphere to sea ice loss:• surface weather and climate (remote impact)• transport and ozone (local impact)

    Screen et al NG 2018 Stratosphere: active component of the climate response to sea ice loss

    Non stationary response Dependence on sea ice loss location

    Peing and Magnusdottir JC 2014Screen JC 2017 …….

    Representation of the stratosphere

    Sun et al JC 2015Nakamura et al GRL 2016 …..

  • Max-Planck-Institut für Meteorologie

    PAMIP atmosphere-only time slice experiments: 1.1, 1.2, 1.3, 1.6

    • SST&SIC change: pd SST & SIC – pi SST & SIC• pdSIC change: pd – pi SIC, fixed pi SST• SST change: pd – pi SST, fixed pd SIC• futArcSIC change: futArc – pd SIC, fixed pd SST

    • Atmospheric component of the MPI and AWI ESMs: ECHAM6 at T127L95 and ECHAM6 at T63L47 (LR)

    • MET OFFICE MODEL

    • Seasonal evolution of the ensemble an zonally-averaged zonal wind @ 60N. Daily, 5-day smoothed

    • Wave Activity Budget for the Extratropical Lower Stratosphere. Ensemble-average, monthly mean

  • Max-Planck-Institut für Meteorologie

    Wave Activity Budget for the Extratropical Lower Stratosphere

    epfz

    epfy

    Peing and Magnusdottir (2014)

    Kushner Polvani (2004) Sigmond and Scinocca (2010) …….

    ua

  • Max-Planck-Institut für Meteorologie

    Ensemble averaged changes Zonally-averaged Zonal Wind @ 60 N

    exp11 - exp12 ua m/s 60N

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    -4-3

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    -2

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    -1-1-1

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    [hPa

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    exp13 - exp12 ua m/s 60N

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    0.50.5

    1-6-5-4

    -3 -2

    -2

    -2

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    -1 -1

    -1-1 -1

    -1

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    -1

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    1 32 62 93 124 152 183 [1 Jan is day=93]

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    [hPa

    ] stratosphereto

    troposphere

    echam6 T127L95

    OCT NOV DEC JAN FEB MAR APR

    OCT NOV DEC JAN FEB MAR APR

    SST&SIC

    pdSIC

    Shaded: significance at 90%

  • Max-Planck-Institut für Meteorologie

    exp11 - exp13 ua m/s 60N

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    -2-2 -2

    -1

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    -1

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    -0.5

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    exp16 - exp11 ua m/s 60N0.5

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    1 1 1

    2 2-2 -2 -2

    -2

    -1

    -1

    -1

    -1

    -1-1

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    -1

    -1

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    -0.5

    -0.5

    -0.5-0.5

    -0.5

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    -0.5

    -0.5

    1 32 62 93 124 152 183 [1 Jan is day=93]

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    [hPa

    ]

    OCT NOV DEC JAN FEB MAR APR

    SST driven

    mid winterstratosphere

    somewhatunperturbed

    echam6 T127L95

    OCT NOV DEC JAN FEB MAR APR

    SST

    futArcSIC

    Shaded: significance at 90%

    Ensemble averaged changes Zonally-averaged Zonal Wind @ 60 N

  • Max-Planck-Institut für Meteorologie

    90N45N

    100 hPa

    10 hPa

    NOV DEC JAN FEB

    NOV

    DEC

    JAN

    FEB

    Ensemble averaged changes Wave activity budget [104 kg m s-4]

    convergence

    positive: upward epf

    positive: upward epf

    SST&SICpdSICSSTfutArcSIC

    positive: equatorward epf

    echam6 T127L95

  • Max-Planck-Institut für Meteorologie

    echam6 T63L47

    exp11 - exp12 ua m/s 60N

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    -5 -5-4 -4-3 -3-2

    -2

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    -1

    -1

    -1

    -1

    -1

    -1

    -1

    -0.5-0.5

    -0.5

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    exp13 - exp12 ua m/s 60N

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    1 32 62 93 124 152 183 [1 Jan is day=93]

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    ]

    exp11 - exp13 ua m/s 60N

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    -4-3-2-2 -2

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    [hPa

    ]

    exp16 - exp11 ua m/s 60N

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    0.5 0.5 0.5

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    0.5

    0.5

    0.50.51

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    1

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    23 -2-2

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    -1

    -1

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    1 32 62 93 124 152 183 [1 Jan is day=93]

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    [hPa

    ]

    OCT NOV DEC JAN FEB MAR APR

    OCT NOV DEC JAN FEB MAR APR

    OCT NOV DEC JAN FEB MAR APR

    OCT NOV DEC JAN FEB MAR APR

    SIC driven

    Shaded: significance at 90%

    SST driven

    SST&SIC

    pdSIC

    SST

    futArcSIC

    Ensemble averaged changes Zonally-averaged Zonal Wind @ 60 N

  • Max-Planck-Institut für Meteorologie

    90N45N

    100 hPa

    10 hPa

    NOV

    DEC

    JAN

    FEB

    NOV DEC JAN FEB

    convergence

    positive: upward epf

    positive: upward epf

    SST&SICpdSICSSTfutArcSIC

    positive: equatorward epf

    Ensemble averaged changes Wave activity budget [104 kg m s-4]

    echam6 T63L47

  • Max-Planck-Institut für Meteorologie

    exp11 - exp12 ua m/s DJF

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    exp11 - exp13 ua m/s DJF

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    exp13 - exp12 ua m/s DJF

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    -0.1-0.1

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    ]

    exp16 - exp11 ua m/s DJF

    0.1

    0.1 0.1

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    -0.1

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    20 40 60 80 [latitude]

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    exp11 - exp12 ua m/s DJF

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    20 40 60 801000

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    ]

    exp11 - exp13 ua m/s DJF

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    exp13 - exp12 ua m/s DJF

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    20 40 60 80 [latitude]

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    ]

    exp16 - exp11 ua m/s DJF

    0.1

    0.1

    0.1

    0.1

    0.1

    0.5

    0.5

    -3

    -1

    -1-0.5

    -0.5

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    20 40 60 80 [latitude]

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    ]

    METOECHAM6 T127L95

    exp11 - exp12 ua m/s DJF

    0.1

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    0.1

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    exp11 - exp13 ua m/s DJF

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    0.1

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    -1

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    20 40 60 801000

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    ]

    exp13 - exp12 ua m/s DJF

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    0.5

    -3

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    essu

    re [h

    Pa]

    exp16 - exp11 ua m/s DJF

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    exp11 - exp12 ua m/s DJF

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    0.1

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    exp11 - exp13 ua m/s DJF0.1

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    1-1

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    ]

    exp13 - exp12 ua m/s DJF

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    -1

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    -0.5-0.1-0.1

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    exp16 - exp11 ua m/s DJF

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    pdSIC change: pd – pi SIC, fixed pi SST

    futArcSIC change: futArc – pd SIC, fixed pd SST

    Ensemble averaged changes DJF Zonally-averaged Zonal Wind

  • Max-Planck-Institut für Meteorologie

    EP-flux bottom

    1 2 3 4 5 6 7 8-3

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    -1

    0

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    45-

    90N

    @ 1

    00hP

    a EP

    Z [1

    04 k

    g m

    s4 ]

    EP-flux bottom

    1 2 3 4 5 6 7 8-3

    -2

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    90N

    @ 1

    00hP

    a EP

    Z [1

    04 k

    g m

    s4 ]

    NOV DEC JAN FEB NOV DEC JAN FEB

    METOECHAM6 T127L95

    SST&SICpdSICSSTfutArcSIC

    45-90N @ 100 hPa upward EP flux [104 kg m s-4]

  • Max-Planck-Institut für Meteorologie

    exp11 T63 ua m/s EQ

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    10-30-25-20

    -15-15

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    -1

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    [hPa

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    exp11 T127 ua m/s EQ

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    10

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    1520

    25-20-20 -15

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    -5

    -5-5

    -5

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    -1

    -1

    -1

    -1-1

    -1

    1 2 3 4 5 6 7 8 9 10 11 12 13 14 [Jan is mt=10]

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    exp11 METO ua m/s EQ

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    1010

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    15 15

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    2020

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    -5

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    [hPa

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    METOECHAM6 T127L95

    DJF DJF

    Ensemble and zonally-averaged zonal wind at the Equator, pd SST & SIC

    months, from IC

  • Max-Planck-Institut für Meteorologie

    SUMMARY

    Arctic winter stratosphere in PAMIP atmos-only experiments

    Impact of sea ice loss: • Potential for a weaker stratospheric vortex, by increased wave activity • Seasonal timing of response varies: mid winter / early and late winter• Dependence to the forcing varies: past to present / present to future

    Differences: Originating in the troposphere? What is the role of local thermal response to SIC? Tropospheric stationary waves?

    SST impact: • Mixed: weaker / stronger stratospheric vortex

    Role of initialization: • Coherent QBO for all members, from the initialization• Another ensemble with a different IC QBO phase?

  • Max-Planck-Institut für Meteorologie

    pamip11 mean ua m/s JJA

    0.5

    0.5

    0.5 0.50.5

    0.5

    0.5

    1 1

    1

    1

    2

    2

    2

    3

    3456789101216

    1820

    -2-1

    -1

    -1

    -0.5

    -0.5

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    [hPa

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    pamip11 mean ua m/s SON

    0.5

    0.5

    0.5

    0.5

    0.5

    1

    11

    1

    22

    345678910121618

    -5-4

    -4

    -3

    -3

    -2

    -2

    -2

    -1

    -1 -1

    -1

    -1

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    -0.5

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    [hPa

    ]

    pamip11 mean ua m/s DJF

    0.5

    0.5

    0.5

    0.5

    1

    1

    1

    12

    2

    2

    3

    3

    3

    4

    4

    4

    5

    5

    5

    6

    6

    67

    7 78

    89

    910

    1012

    12

    16-12-10-9-8-7-6-5-4-3

    -2 -2

    -2-1

    -1 -1

    -0.5

    -0.5

    -0.5

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    [hPa

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    pamip11 mean ua m/s MAM

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    0.5

    0.5

    0.5

    1

    11

    1

    1

    2

    2

    2

    2

    2

    3

    3

    3456

    -4-3-2

    -1

    -1

    -1

    -1

    -0.5

    -0.5

    -0.5

    20 40 60 80500

    200

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    pres

    sure

    [hPa

    ]

    METO minus ECHAM6 T127L95