Preprints
https://doi.org/10.5194/egusphere-2025-2212
https://doi.org/10.5194/egusphere-2025-2212
20 May 2025
 | 20 May 2025

Response of Northern Hemisphere Rossby wave breaking to changes in sea surface temperature and sea ice cover

Sara Tahvonen, Daniel Köhler, Petri Räisänen, and Victoria Anne Sinclair

Abstract. Although well-researched in the present climate, it is poorly understood how Rossby wave breaking (RWB) may change in a warmer future climate. In this study, we examine how large changes in sea ice cover (SIC) and sea surface temperature (SST) affect the frequency and spatial distribution of Rossby wave breaking in the Northern Hemisphere during the boreal winter (December–February) and summer (June–August) seasons. Our experiment setup consists of eight 40-year atmosphere-only simulations from two models (OpenIFS and EC-Earth) that use different combinations of prescribed present-day and future SIC and SST values under the SSP5-8.5 scenario.

We find present-day RWB frequencies that correspond well with previous literature. Our models are generally in good agreement with regards to the spatial distribution of RWB. The effects of SSP5-8.5 SST on RWB are substantial, while simulations using future SIC and present-day SSTs do not exhibit statistically significant changes compared to the present. In simulations with SST changes, anticyclonic wave breaking (AWB) frequencies show large decreases during both winter and summer, while the primary change to cyclonic wave breaking (CWB) are small increases of varying magnitude in winter. The winter changes are notably collocated with changes in the strength and location of jet streams. The largest changes occur over the North Pacific, where winter AWB decrease by 60–70 % over the East Pacific and summer AWB decrease by roughly 50 % over the West Pacific and East Asia. Over the western North Atlantic, decreases of 10–30 % in winter AWB are collocated with a stronger eddy-driven jet, which may suggest an eastward shift in AWB. In summer, AWB decreases by about 50 % over North America but increases slightly over Europe. As with related previous studies of future changes in blocking and jet stream waviness, there are uncertainties in our results, and especially determining the impact of SIC changes likely requires longer simulations than those used in this study. This study demonstrates that particularly SST changes are an important component for changes to RWB in future climates.

Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this paper. While Copernicus Publications makes every effort to include appropriate place names, the final responsibility lies with the authors. Views expressed in the text are those of the authors and do not necessarily reflect the views of the publisher.
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Sara Tahvonen, Daniel Köhler, Petri Räisänen, and Victoria Anne Sinclair

Status: final response (author comments only)

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2025-2212', Anonymous Referee #1, 03 Jun 2025
    • AC1: 'Reply on RC1', Sara Tahvonen, 22 Aug 2025
  • RC2: 'Comment on egusphere-2025-2212', Anonymous Referee #2, 17 Jun 2025
    • AC2: 'Reply on RC2', Sara Tahvonen, 22 Aug 2025
  • RC3: 'Comment on egusphere-2025-2212', Anonymous Referee #3, 17 Jun 2025
    • AC3: 'Reply on RC3', Sara Tahvonen, 22 Aug 2025
Sara Tahvonen, Daniel Köhler, Petri Räisänen, and Victoria Anne Sinclair

Model code and software

Rossby wave breaking detection algorithm Sara Tahvonen https://doi.org/10.5281/zenodo.15357272

Sara Tahvonen, Daniel Köhler, Petri Räisänen, and Victoria Anne Sinclair

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Short summary
Rossby wave breaking (RWB) influences weather at a large scale and can contribute to extreme weather events, but it is not known if climate change will have an effect on where and how often RWB occurs. We investigate how extreme sea ice loss and warming of the sea surface effect RWB. Our results show that sea surface temperatures significantly change local RWB frequencies and the closely related upper atmospheric jet streams, but that sea ice changes have no noticeable effect.
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