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Influence of Arctic Sea Ice Loss in Autumn Compared to That in Winter on the Atmospheric Circulation Russell Blackport James Screen University of Exeter PAMIP Workshop 26 th June 2019 Blackport, R., & Screen, J. A. (2019).Geophysical Research Letters, https://doi.org/10.1029/2018GL081469

Influence of Arctic Sea Ice Loss in Autumn Compared to ... › projects › CMIP6 › PAMIP › workshop › 3...• Z2Cice: As in control, but sea ice albedo modified to achieve year-round

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Page 1: Influence of Arctic Sea Ice Loss in Autumn Compared to ... › projects › CMIP6 › PAMIP › workshop › 3...• Z2Cice: As in control, but sea ice albedo modified to achieve year-round

Influence of Arctic Sea Ice Loss in Autumn Compared to That in Winter on the Atmospheric Circulation

Russell Blackport

James Screen

University of Exeter

PAMIP Workshop 26th June 2019

Blackport, R., & Screen, J. A. (2019).Geophysical Research Letters, https://doi.org/10.1029/2018GL081469

Page 2: Influence of Arctic Sea Ice Loss in Autumn Compared to ... › projects › CMIP6 › PAMIP › workshop › 3...• Z2Cice: As in control, but sea ice albedo modified to achieve year-round

Background

• Winter circulation response to projected year-round sea ice loss in coupled models consistent across models and protocols

Screen et al. 2018

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Question: To what extent is the winter circulation response driven by autumn sea ice loss?

• Relevant for understanding physical mechanisms as well as for seasonal prediction

• Observed correlations indicate winter response may be driven by Autumn sea ice

• Previously addressed in an AGCM (Sun et al. 2015), but ocean coupling may provide additional mechanisms for lagged response

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Model Experiments• HadGEM2-ES model with 1.25° latitude by 1.875° longitude resolution

• 4 ensembles (400 realizations x 5 years):• Present day control: 2008-2012 RCP8.5 forcing

• ‘2C’: 2036-2040 RCP8.5 forcing (target for sea ice loss ensembles)

• ‘2Cice’: As in control, but sea ice albedo modified to achieve year-round sea ice loss similar to ‘2C’ ensemble. Cold deep snow albedo: 0.80 -> 0.05, Snow-free ice albedo: 0.61 -> 0.66

• ‘2CiceASO’: As in control, but sea ice albedo modified to achieve Autumn sea ice loss similar to ‘2C’ ensemble. Cold deep snow albedo: 0.80 -> 0.88, Snow-free ice albedo: 0.61 -> 0.10

Page 5: Influence of Arctic Sea Ice Loss in Autumn Compared to ... › projects › CMIP6 › PAMIP › workshop › 3...• Z2Cice: As in control, but sea ice albedo modified to achieve year-round

Sea Ice Response

Autumn sea ice loss

Year-round sea ice loss

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Surface Air Temperature Response

Year-round sea ice loss

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Surface Air Temperature Response

Autumn sea ice loss

Year-round sea ice loss

• In response to autumn ice loss, high-latitude warming persists into winter despite little change in SIC/SIE

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Zonal Wind Response

Year-round sea ice loss

Page 9: Influence of Arctic Sea Ice Loss in Autumn Compared to ... › projects › CMIP6 › PAMIP › workshop › 3...• Z2Cice: As in control, but sea ice albedo modified to achieve year-round

Zonal Wind Response

Autumn sea ice loss

Year-round sea ice loss

• Winter circulation response not seen in response to sea ice loss in autumn

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U700 Response

Autumn sea ice loss

Year-round sea ice loss

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Sea Level Pressure Response

Autumn sea ice loss

Year-round sea ice loss

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Polar Cap Height Response

Autumn sea ice loss

Year-round sea ice loss

Page 13: Influence of Arctic Sea Ice Loss in Autumn Compared to ... › projects › CMIP6 › PAMIP › workshop › 3...• Z2Cice: As in control, but sea ice albedo modified to achieve year-round

• We find a winter circulation response to year-round sea ice loss similar to previous coupled model experiments

• These are not seen in response to reduced sea ice extent only in autumn

• Our results suggest winter circulation response seen in models is primarily driven by winter sea ice loss

Conclusions

Page 14: Influence of Arctic Sea Ice Loss in Autumn Compared to ... › projects › CMIP6 › PAMIP › workshop › 3...• Z2Cice: As in control, but sea ice albedo modified to achieve year-round

• Only one model used – conclusions could be model dependant

• Pan-Arctic sea ice vs regional sea ice loss

• Are the responses to autumn and winter sea ice loss additive?

• Could test these with additional experiments using PAMIP forcing fields

Caveats and Future Work