The IPWP as a capacitor for autumn sea ice loss in Northeastern Canada

The Indo-Pacific Warm Pool (IPWP) has been warming due largely to increasing greenhouse gas emissions, but its impact on Arctic sea ice remains unclear. Our study finds a significant negative correlation between the IPWP index and sea ice concentration in northeastern Canada during boreal autumn (October-December). Our results suggest that IPWP warming statistically accounts for 45% of sea ice loss observed in this region. We introduce the “Arctic capacitor effect of the IPWP”, a novel concept that expounds upon the distant connection between greenhouse gas emissions and Arctic sea ice loss. Specifically, as greenhouse gases elevate temperatures in the IPWP, increasing temperature gradient and tropical convection, a planetary wavetrain is initiated. This wavetrain, along with transit eddy feedback, traverses towards the Arctic and thereby influences the strength of the Arctic vortex and its associated effects on Arctic sea ice. Our findings highlight the crucial role of tropical oceans in the broader context of global climate change, emphasizing the necessity of accounting for their impact on polar climate.

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Publication Details

Journal
npj Climate and Atmospheric Science
Published
2024-10-25
DOI
https://doi.org/10.1038/s41612-024-00798-9
Citations
4
Primary Topic
Arctic and Antarctic ice dynamics
Type
article
Field-Weighted Citation Impact
1.51
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article

The IPWP as a capacitor for autumn sea ice loss in Northeastern Canada

Timo Vihma, Cuijuan Sui, Lejiang Yu, Shuoyi Ding et al.
4 citations
npj Climate and Atmospheric Science
Arctic and Antarctic ice dynamics
1.51
article

The IPWP as a capacitor for autumn sea ice loss in Northeastern Canada

Timo Vihma, Cuijuan Sui, Lejiang Yu, Shuoyi Ding, Shiyuan Zhong, Bo Sun
article en
4 citations

Abstract

The Indo-Pacific Warm Pool (IPWP) has been warming due largely to increasing greenhouse gas emissions, but its impact on Arctic sea ice remains unclear. Our study finds a significant negative correlation between the IPWP index and sea ice concentration in northeastern Canada during boreal autumn (October-December). Our results suggest that IPWP warming statistically accounts for 45% of sea ice loss observed in this region. We introduce the “Arctic capacitor effect of the IPWP”, a novel concept that expounds upon the distant connection between greenhouse gas emissions and Arctic sea ice loss. Specifically, as greenhouse gases elevate temperatures in the IPWP, increasing temperature gradient and tropical convection, a planetary wavetrain is initiated. This wavetrain, along with transit eddy feedback, traverses towards the Arctic and thereby influences the strength of the Arctic vortex and its associated effects on Arctic sea ice. Our findings highlight the crucial role of tropical oceans in the broader context of global climate change, emphasizing the necessity of accounting for their impact on polar climate.

npj Climate and Atmospheric ScienceVol. 7(1)
Finnish Meteorological Institute (FI), Polar Research Institute of China (CN), Fudan University (CN), National Marine Environmental Forecasting Center (CN), Michigan State University (US)
Life below water
Openalex Percentile: Top 19%
Arctic and Antarctic ice dynamics
1.51
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The IPWP as a capacitor for autumn sea ice loss in Northeastern Canada — Timo Vihma, Cuijuan Sui, et al. · npj Climate and Atmospheric Science (2024) | TGRS Research Map | TGRS