Oceanographic environment of the Tsushima Island

CTD (Conductivity-Temperature-Depth profiler) observations and bottom water sampling were conducted at 192 sites in the waters surrounding the Tsushima Island during cruise GB23 from October to November in 2023.The survey area is located around the Tsushima Strait, through which the Tsushima Warm Current flows into the Sea of Japan.The observed sea surface water temperature ranged from 18.9 to 23.9 and salinity ranged from 33.7 to 34.6, suggesting the influence of both the Kyushu Coastal Current and the Tsushima Warm Current.The bottom water temperature generally decreased with increasing depth.In the deeper layers south of the Goto Islands, we observed a water mass thought to be North Pacific Subtropical Mode Water, which flowed to this region from the Goto Canyon.A high-turbidity layer was detected in the coastal waters off Kyushu and north of Tsushima Island, likely influenced by the local topography and ocean currents.

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Journal
BULLETIN OF THE GEOLOGICAL SURVEY OF JAPAN
Published
2025-10-29
DOI
https://doi.org/10.9795/bullgsj.76.4-5_235
Citations
1
Primary Topic
Earthquake and Disaster Impact Studies
Type
article
Field-Weighted Citation Impact
2.18
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article

Oceanographic environment of the Tsushima Island

Naoki Saito, Takuya Itaki, Atsushi Suzuki, Hajime Katayama et al.
1 citations
BULLETIN OF THE GEOLOGICAL SURVEY OF JAPAN
Earthquake and Disaster Impact Studies
2.18
article

Oceanographic environment of the Tsushima Island

Naoki Saito, Takuya Itaki, Atsushi Suzuki, Hajime Katayama, Mutsumi Iizuka, Yoshiaki SUZUKI
article en
1 citations

Abstract

CTD (Conductivity-Temperature-Depth profiler) observations and bottom water sampling were conducted at 192 sites in the waters surrounding the Tsushima Island during cruise GB23 from October to November in 2023.The survey area is located around the Tsushima Strait, through which the Tsushima Warm Current flows into the Sea of Japan.The observed sea surface water temperature ranged from 18.9 to 23.9 and salinity ranged from 33.7 to 34.6, suggesting the influence of both the Kyushu Coastal Current and the Tsushima Warm Current.The bottom water temperature generally decreased with increasing depth.In the deeper layers south of the Goto Islands, we observed a water mass thought to be North Pacific Subtropical Mode Water, which flowed to this region from the Goto Canyon.A high-turbidity layer was detected in the coastal waters off Kyushu and north of Tsushima Island, likely influenced by the local topography and ocean currents.

BULLETIN OF THE GEOLOGICAL SURVEY OF JAPANVol. 76(4-5)
Geological Survey of Japan (JP)
Openalex Percentile: Top 10%
Earthquake and Disaster Impact Studies
2.18
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Oceanographic environment of the Tsushima Island — Naoki Saito, Takuya Itaki, et al. · BULLETIN OF THE GEOLOGICAL SURVEY OF JAPAN (2025) | TGRS Research Map | TGRS