Precision measurement of ocean tides using cosmic-ray muons
Abstract
Cosmic-ray muons provide a natural probe of the integrated mass along their trajectories. Here we show that cosmic-ray muons can monitor ocean-tide-induced variations in seawater overburden within an underwater tunnel. The observed modulation closely tracks independent tide-gauge measurements, yielding an attenuation response coefficient of k=43.2±1.0~counts/h/m and resolving meter-scale variations in seawater overburden. A spatial muography scan validates the overburden model, confirming that the seawater contribution is essential to reproduce the observed attenuation. Unlike conventional tide gauges that measure sea level locally, muography measures the integrated overburden above the detector. These results demonstrate that muography can quantitatively resolve small, time-dependent variations in environmental overburden, providing a new approach to monitoring dynamic natural systems.
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BibTeX
@misc{seo2026precision,
title = {{Precision measurement of ocean tides using cosmic-ray muons}},
author = {Jiwon Seo and Jongseok Chung and Chang Hyon Ha and TongZhou Huang and Jinyoung Kim and Sooa Kim and Hani Kimku and Byoung-cheol Koh and Minsu Kwak and Sihyun Lee and Yujin Lee},
howpublished = {arXiv},
year = {2026},
month = oct,
doi = {10.48550/arxiv.2610.05294},
eprint = {2610.05294},
archivePrefix = {arXiv},
url = {https://arxiv.org/abs/2610.05294},
}
RIS
TY - UNPB
TI - Precision measurement of ocean tides using cosmic-ray muons
AU - Jiwon Seo
AU - Jongseok Chung
AU - Chang Hyon Ha
AU - TongZhou Huang
AU - Jinyoung Kim
AU - Sooa Kim
AU - Hani Kimku
AU - Byoung-cheol Koh
AU - Minsu Kwak
AU - Sihyun Lee
AU - Yujin Lee
PY - 2026
DA - 2026/10/04
PB - arXiv
DO - 10.48550/arxiv.2610.05294
UR - https://arxiv.org/abs/2610.05294
AB - Cosmic-ray muons provide a natural probe of the integrated mass along their trajectories. Here we show that cosmic-ray muons can monitor ocean-tide-induced variations in seawater overburden within an underwater tunnel. The observed modulation closely tracks independent tide-gauge measurements, yielding an attenuation response coefficient of k=43.2±1.0~counts/h/m and resolving meter-scale variations in seawater overburden. A spatial muography scan validates the overburden model, confirming that the seawater contribution is essential to reproduce the observed attenuation. Unlike conventional tide gauges that measure sea level locally, muography measures the integrated overburden above the detector. These results demonstrate that muography can quantitatively resolve small, time-dependent variations in environmental overburden, providing a new approach to monitoring dynamic natural systems.
ER -