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Table 1 Characterization of the water masses in the southern Ryukyu Island Arc. *Only one data available

From: Characterization of water masses around the southern Ryukyu Islands based on isotopic compositions

 

Depth

T (°C)

Salinity

σθ (kg m−3)

δD (‰, average)

δ18O (‰, average)

εNd

Okinawa Trough side

Kuroshio Surface Water

< 100

23.4–28.2

34.47–34.78

< 23.0

4.5*

0.5*

− 2.2

Kuroshio Tropical Water

100–200

18.6–24.1

34.81–34.88

23.5–24.6

3.6

0.4

− 5.3 to − 5.2

Western North Pacific Central Water

250–500

10.0–18.6

34.32–34.82

25.0–26.4

3.1

0.4

− 6.2 to − 2.8

Kuroshio Intermediate Water

500–755

5.8–9.0

34.29–34.36

26.5–27.0

1.0

0.2

− 5.1 to − 4.8

Deeper Kuroshio Intermediate Water

755–1900

3.6–5.7

34.36–34.48

27.0–27.5

0.4

0.0

− 8.2 to − 4.9

Deep water

1900–1938

2.0

34.63

> 27.5

–

–

–

Pacific side

Surface water

< 83

24.5–28.6

34.31–34.74

< 23.0

3.3

0.4

− 1.7 to − 1.2

North Pacific Tropical Water

99–216

19.3–24.6

34.67–34.90

23.5–24.7

3.4

0.4

− 4.1 to − 1.1

Western North Pacific Central Water

222–476

11.2–18.9

34.37–34.82

24.9–26.0

3.1

0.4

− 5.2 to − 3.4

North Pacific Intermediate Water

478–863

4.9–11.4

34.18–34.39

26.3–27.2

1.3

0.1

− 7.0 to − 3.8

Deeper North Pacific Intermediate Water

864–1851

2.2–4.9

34.40–34.61

27.2–27.6

0.5

0.1

− 4.0

Pacific Deep Water

1907–2620

1.7–2.1

34.59–34.64

> 27.7

0.7

0.0

− 5.3