Anthropogenic Iodine‐129 Traces Complex Inflows of Atlantic and Pacific Waters Into the Western Arctic

Abstract Changes in Atlantic and Pacific inflows into the Arctic are contributing to Arctic warming and reshaping water circulation. However, knowledge gaps remain regarding circulation pathways in the western Arctic Ocean, where Arctic Atlantic Water (AAW) and Pacific Water interact. Here, we repor...

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Main Authors: Yuanzhi Qi, Xinru Xu, Qiuyu Yang, Takeyasu Yamagata, Hiroyuki Matsuzaki, Hisao Nagai, Yuichiro Kumamoto
Format: Article
Language:English
Published: Wiley 2025-04-01
Series:Geophysical Research Letters
Subjects:
Online Access:https://doi.org/10.1029/2025GL114687
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author Yuanzhi Qi
Xinru Xu
Qiuyu Yang
Takeyasu Yamagata
Hiroyuki Matsuzaki
Hisao Nagai
Yuichiro Kumamoto
author_facet Yuanzhi Qi
Xinru Xu
Qiuyu Yang
Takeyasu Yamagata
Hiroyuki Matsuzaki
Hisao Nagai
Yuichiro Kumamoto
author_sort Yuanzhi Qi
collection DOAJ
description Abstract Changes in Atlantic and Pacific inflows into the Arctic are contributing to Arctic warming and reshaping water circulation. However, knowledge gaps remain regarding circulation pathways in the western Arctic Ocean, where Arctic Atlantic Water (AAW) and Pacific Water interact. Here, we report iodine‐129 (129I) concentrations in seawater collected from the western Arctic Ocean and Bering Sea in 2021. The wide range of 129I concentrations (1–355 × 107 atoms/L) highlights its value as a tracer for identifying water masses and deciphering circulation patterns. Depth profiles of 129I reveal that AAW enters the western Arctic via multiple pathways, with the top layer potentially diverging from the boundary flow and dispersing throughout the region. This previously unreported feature suggests a broader AAW influence on the western Arctic. Additionally, 129I concentrations provide direct evidence that the cold halocline effectively limits the upward transfer of matter from AAW to the Arctic surface.
format Article
id doaj-art-15aba58a3e9549e1a900d61eddc7abf7
institution Kabale University
issn 0094-8276
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language English
publishDate 2025-04-01
publisher Wiley
record_format Article
series Geophysical Research Letters
spelling doaj-art-15aba58a3e9549e1a900d61eddc7abf72025-08-20T03:49:45ZengWileyGeophysical Research Letters0094-82761944-80072025-04-01527n/an/a10.1029/2025GL114687Anthropogenic Iodine‐129 Traces Complex Inflows of Atlantic and Pacific Waters Into the Western ArcticYuanzhi Qi0Xinru Xu1Qiuyu Yang2Takeyasu Yamagata3Hiroyuki Matsuzaki4Hisao Nagai5Yuichiro Kumamoto6Micro Analysis Laboratory Tandem Accelerator The University Museum The University of Tokyo Bunkyo City Tokyo JapanDepartment of Nuclear Engineering and Management The University of Tokyo Bunkyo City Tokyo JapanDepartment of Nuclear Engineering and Management The University of Tokyo Bunkyo City Tokyo JapanMicro Analysis Laboratory Tandem Accelerator The University Museum The University of Tokyo Bunkyo City Tokyo JapanMicro Analysis Laboratory Tandem Accelerator The University Museum The University of Tokyo Bunkyo City Tokyo JapanMicro Analysis Laboratory Tandem Accelerator The University Museum The University of Tokyo Bunkyo City Tokyo JapanResearch Institute for Global Change Japan Agency for Marine‐Earth Science and Technology Yokosuka Kanagawa JapanAbstract Changes in Atlantic and Pacific inflows into the Arctic are contributing to Arctic warming and reshaping water circulation. However, knowledge gaps remain regarding circulation pathways in the western Arctic Ocean, where Arctic Atlantic Water (AAW) and Pacific Water interact. Here, we report iodine‐129 (129I) concentrations in seawater collected from the western Arctic Ocean and Bering Sea in 2021. The wide range of 129I concentrations (1–355 × 107 atoms/L) highlights its value as a tracer for identifying water masses and deciphering circulation patterns. Depth profiles of 129I reveal that AAW enters the western Arctic via multiple pathways, with the top layer potentially diverging from the boundary flow and dispersing throughout the region. This previously unreported feature suggests a broader AAW influence on the western Arctic. Additionally, 129I concentrations provide direct evidence that the cold halocline effectively limits the upward transfer of matter from AAW to the Arctic surface.https://doi.org/10.1029/2025GL114687Arctic Oceaniodine‐129ocean currents
spellingShingle Yuanzhi Qi
Xinru Xu
Qiuyu Yang
Takeyasu Yamagata
Hiroyuki Matsuzaki
Hisao Nagai
Yuichiro Kumamoto
Anthropogenic Iodine‐129 Traces Complex Inflows of Atlantic and Pacific Waters Into the Western Arctic
Geophysical Research Letters
Arctic Ocean
iodine‐129
ocean currents
title Anthropogenic Iodine‐129 Traces Complex Inflows of Atlantic and Pacific Waters Into the Western Arctic
title_full Anthropogenic Iodine‐129 Traces Complex Inflows of Atlantic and Pacific Waters Into the Western Arctic
title_fullStr Anthropogenic Iodine‐129 Traces Complex Inflows of Atlantic and Pacific Waters Into the Western Arctic
title_full_unstemmed Anthropogenic Iodine‐129 Traces Complex Inflows of Atlantic and Pacific Waters Into the Western Arctic
title_short Anthropogenic Iodine‐129 Traces Complex Inflows of Atlantic and Pacific Waters Into the Western Arctic
title_sort anthropogenic iodine 129 traces complex inflows of atlantic and pacific waters into the western arctic
topic Arctic Ocean
iodine‐129
ocean currents
url https://doi.org/10.1029/2025GL114687
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