Intrusion of Kuroshio-Derived bottom cold water into Osaka Bay and its possible cause

Koichi Sugimatsu, Atsuhiko Isobe

Research output: Contribution to journalArticle

8 Citations (Scopus)

Abstract

The bottom layer in Osaka Bay was occupied in August from 1980 to 1995 by a water mass of relatively low temperature and rich in nutrients in comparison to previous and following decades. The relationship between Osaka Bay bottom temperature and Kuroshio axis location south of Kii Peninsula has been investigated using the dataset archived by Osaka Research Institute of Environment of Agriculture and Fisheries and axis-location data provided by Marine Information Research Center. The correlation between bottom temperature in the bay and Kuroshio-axis distance from Cape Shionomisaki indicates that the bottom temperature in the bay decreases when the Kuroshio axis is a long distance from the cape, and vice versa. To investigate why the temperature distribution depends on the axis location, composite temperature maps are depicted using summer temperature data from 1970 to 2005 archived in the Japan Oceanographic Data Center (JODC) after dividing all data into two groups with different axis locations. These temperature maps and temperature-salinity plots using the same JODC data suggest a scenario: cold water in the Kuroshio intermediate layer is first upwelled on the eastern side of the Kii Peninsula and thereafter moves westward as a coastal boundary current in the Kelvin wave sense of the Northern Hemisphere when the Kuroshio axis is located around 74-km distance from Cape Shionomisaki. This scenario is validated using internal Froude number maps depicted using the JODC-archived hydrographic data and geostrophic current fields. In addition, the reanalysis daily data provided by Japan Coastal Ocean Predictability Experiment are used for the validation.

Original languageEnglish
Pages (from-to)191-199
Number of pages9
JournalJournal of Oceanography
Volume66
Issue number2
DOIs
Publication statusPublished - Apr 1 2010
Externally publishedYes

Fingerprint

cold water
bottom water
temperature
boundary current
coastal current
Kelvin wave
Froude number
water mass
Northern Hemisphere
fishery
agriculture
salinity
nutrient
ocean
summer
data centre

All Science Journal Classification (ASJC) codes

  • Oceanography

Cite this

Intrusion of Kuroshio-Derived bottom cold water into Osaka Bay and its possible cause. / Sugimatsu, Koichi; Isobe, Atsuhiko.

In: Journal of Oceanography, Vol. 66, No. 2, 01.04.2010, p. 191-199.

Research output: Contribution to journalArticle

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