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

Earth Sciences

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

L. Yu, S. Zhong, et al.

Discover how Indo-Pacific Warm Pool warming is driving Arctic sea ice loss in northeastern Canada, revealing a striking correlation where 45% of the observed sea ice reduction is attributable to this phenomenon. This groundbreaking research by Lejiang Yu, Shiyuan Zhong, Timo Vihma, Shuoyi Ding, Cuijuan Sui, and Bo Sun introduces the concept of the 'Arctic capacitor effect of the IPWP'.

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~3 min • Beginner • English
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.
Publisher
npj Climate and Atmospheric Science
Published On
Oct 25, 2024
Authors
Lejiang Yu, Shiyuan Zhong, Timo Vihma, Shuoyi Ding, Cuijuan Sui, Bo Sun
Tags
Indo-Pacific Warm Pool
Arctic sea ice
climate change
greenhouse gases
boreal autumn
planetary wavetrain
Arctic vortex
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