Articles | Volume 22, issue 2
https://doi.org/10.5194/os-22-1085-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/os-22-1085-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Polarity and direction dependence of energetic cross-frontal eddy transport in the Southern Ocean's Pacific sector
Huimin Wang
College of Oceanography and Ecological Science, Shanghai Ocean University, Shanghai, China
Lingqiao Cheng
CORRESPONDING AUTHOR
College of Oceanography and Ecological Science, Shanghai Ocean University, Shanghai, China
Center for Polar Research, Shanghai Ocean University, Shanghai, China
Erik Behrens
Earth Sciences New Zealand, Wellington, New Zealand
Zhuang Chen
College of Oceanography and Ecological Science, Shanghai Ocean University, Shanghai, China
College of Marine Living Resource Sciences and Management, Shanghai Ocean University, Shanghai, China
Center for Polar Research, Shanghai Ocean University, Shanghai, China
Jennifer Devine
Earth Sciences New Zealand, Nelson, New Zealand
Guoping Zhu
College of Marine Living Resource Sciences and Management, Shanghai Ocean University, Shanghai, China
Center for Polar Research, Shanghai Ocean University, Shanghai, China
Polar Marine Ecosystem Group, The Key Laboratory of Sustainable Exploitation of Oceanic Fisheries Resources, Ministry of Education, Shanghai, China
International Research Center for Marine Biosciences at Shanghai Ocean University, Ministry of Science and Technology, Shanghai, China
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Christian Lewis, Rachel Corran, Sara E. Mikaloff-Fletcher, Erik Behrens, Rowena Moss, Gordon Brailsford, Andrew Lorrey, Margaret Norris, and Jocelyn Turnbull
Biogeosciences, 22, 4187–4201, https://doi.org/10.5194/bg-22-4187-2025, https://doi.org/10.5194/bg-22-4187-2025, 2025
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The Southern Ocean carbon sink is a balance between two opposing forces: CO2 absorption at mid-latitudes and CO2 outgassing at high latitudes. Radiocarbon analysis can be used to constrain the latter, as upwelling waters outgas old CO2, diluting atmospheric radiocarbon content. We present tree-ring radiocarbon measurements from Aotearoa / New Zealand and Chile. We show that low radiocarbon in Aotearoa / New Zealand’s Motu Ihupuku / Campbell Island is linked to outgassing in the critical Antarctic Southern Zone.
Christopher J. Roach, Joao Marcos A. C. de Souza, Erik Behrens, and Stephen J. Stuart
EGUsphere, https://doi.org/10.5194/egusphere-2024-1962, https://doi.org/10.5194/egusphere-2024-1962, 2024
Preprint archived
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We have used a 5 km regional ocean model for New Zealand forced with a coarser resolution global model to project changes in under medium and high emissions scenarios. This is necessary since the global model is unable to resolve the small scale processes on the continental shelf which determine climate change may influence fisheries and aquaculture. We see the upper ocean warms at similar rates all around New Zealand, but that the deep ocean shows more rapid warming in the west and south.
Yusuf A. Bhatti, Laura E. Revell, Alex J. Schuddeboom, Adrian J. McDonald, Alex T. Archibald, Jonny Williams, Abhijith U. Venugopal, Catherine Hardacre, and Erik Behrens
Atmos. Chem. Phys., 23, 15181–15196, https://doi.org/10.5194/acp-23-15181-2023, https://doi.org/10.5194/acp-23-15181-2023, 2023
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Aerosols are a large source of uncertainty over the Southern Ocean. A dominant source of sulfate aerosol in this region is dimethyl sulfide (DMS), which is poorly simulated by climate models. We show the sensitivity of simulated atmospheric DMS to the choice of oceanic DMS data set and emission scheme. We show that oceanic DMS has twice the influence on atmospheric DMS than the emission scheme. Simulating DMS more accurately in climate models will help to constrain aerosol uncertainty.
Jonny Williams, Erik Behrens, Olaf Morgenstern, Peter Gibson, and Joao Teixeira
EGUsphere, https://doi.org/10.5194/egusphere-2023-1694, https://doi.org/10.5194/egusphere-2023-1694, 2023
Preprint withdrawn
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We use open-source cyclone tracking software and state-of-the-art climate models to characterise present-day tropical cyclones – TCs – in the South Pacific before moving on to estimate how they may change in the future. A robust result of this work is the projection of future intensification of TCs. However, the question of their future occurrence frequency is less clear. Under extreme future warming scenarios, we postulate a possible increase in power dissipation per TC of up to 25 %.
Georgia R. Grant, Jonny H. T. Williams, Sebastian Naeher, Osamu Seki, Erin L. McClymont, Molly O. Patterson, Alan M. Haywood, Erik Behrens, Masanobu Yamamoto, and Katelyn Johnson
Clim. Past, 19, 1359–1381, https://doi.org/10.5194/cp-19-1359-2023, https://doi.org/10.5194/cp-19-1359-2023, 2023
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Regional warming will differ from global warming, and climate models perform poorly in the Southern Ocean. We reconstruct sea surface temperatures in the south-west Pacific during the mid-Pliocene, a time 3 million years ago that represents the long-term outcomes of 3 °C warming, which is expected for the future. Comparing these results to climate model simulations, we show that the south-west Pacific region will warm by 1 °C above the global average if atmospheric CO2 remains above 350 ppm.
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Short summary
This study focused on the cross-frontal eddies (CFEs) in the Pacific sector. By analyzing 23 years of satellite and Argo float data, we found that the behaviors of these CFEs vary according to their polarity and direction. These powerful CFEs play a key role in transporting heat and nutrients meridionally, and helping to counteract the effects of strengthening winds and inhomogeneous warming.
This study focused on the cross-frontal eddies (CFEs) in the Pacific sector. By analyzing 23...