Research Article
[Retracted] Prediction of Long-term Variation of Ocean Circulation Based on Grey Correlation Clustering
Table 5
Properties of water masses in the South China Sea.
| Name | Symbol | Source | Depth range/m | Temperature range/°C (early winter and late summer) | Salinity range (early winter and late summer) |
| Coastal freshwater mass | F | Continental runoff | <20 | | | Nearshore mixed water mass | M | The coastal fresh water is mixed with the external seawater to form | <75 | | | South China sea surface water mass | S | Western Pacific surface water | 0–100 | | | 0–120 | | | Continental shelf water in the southern South China Sea (only in summer) | TS | Java Sea water and Gulf of Thailand water mixed to form | 0–120 | | | Kuroshio surface water mass | KS | Kuroshio surface water | 0–100 | | | Kuroshio subsurface water mass | KU | Kuroshio subsurface water | 100–250 | | | South China Sea subsurface water mass | U | Western Pacific subsurface water | 100–200 | 15.0–21.5 | 34.00–34.70 | 120–200 | 6.0–22.0 | 34.00–34.65 | South China Sea sub-middle water mass | UI | Western Pacific subtropical thermocline water | 200–350 | 9.8–15.0 | 34.40–34.70 | 200–350 | 11.0–16.0 | 34.35–34.65 | Middle water mass in the South China Sea | I | Western Pacific middle water | 350–900 | 4.5–10.0 | 34.40–34.50 | 350–800 | 5.5–11.0 | 34.39–34.55 | Deep water mass in the South China Sea | D | Western Pacific deep water | >900 | <5.0 | 34.35–34.62 | >800 | <5.5 | 34.30–34.70 |
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