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Tim Woollings

Professor of Physical Climate Science

Research theme

  • Climate physics

Sub department

  • Atmospheric, Oceanic and Planetary Physics

Research groups

  • Climate dynamics
Tim.Woollings@physics.ox.ac.uk
Telephone: 01865 (2)82427
Atmospheric Physics Clarendon Laboratory, room 203
  • About
  • Publications

Multi-decadal skill variability in predicting the spatial patterns of ENSO events

(2024)

Authors:

Matthew Wright, Antje Weisheimer, Tim Woollings
More details from the publisher

Predictable decadal forcing of the North Atlantic jet speed by sub-polar North Atlantic sea surface temperatures

Weather and Climate Dynamics Copernicus Publications 4:4 (2023) 853-874

Authors:

Kristian Strommen, Tim Woollings, Paolo Davini, Paolo Ruggieri, Isla R Simpson
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European winter climate response to projected Arctic sea-ice loss strongly shaped by change in the North Atlantic jet

Copernicus Publications (2023)

Authors:

Kunhui Ye, Tim Woollings, James Screen
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Impacts of Atlantic Multi-decadal Variability on the mid-latitude atmosphere

Copernicus Publications (2023)

Authors:

Matthew Patterson, Tim Woollings
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Trends in the atmospheric jet streams are emerging in observations and could be linked to tropical warming

Communications Earth & Environment Springer Nature 4 (2023) 125

Authors:

Tim Woollings, Marie Drouard, Christopher H O’Reilly, David MH Sexton, Carol McSweeney

Abstract:

Climate models predict a weak poleward shift of the jets in response to continuing climate change. Here we revisit observed jet trends using 40 years of satellite-era reanalysis products and find evidence that general poleward shifts are emerging. The significance of these trends is often low and varies between datasets, but the similarity across different seasons and hemispheres is notable. While much recent work has focused on the jet response to amplified Arctic warming, the observed trends are more consistent with the known sensitivity of the circulation to tropical warming. The circulation trends are within the range of historical model simulations but are relatively large compared to the models when the accompanying trends in upper tropospheric temperature gradients are considered. The balance between tropical warming and jet shifts should therefore be closely monitored in the near future. We hypothesise that the sensitivity of the circulation to tropical heating may be one factor affecting this balance.

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