Research Article
Research on Cold Core Eddy Change and Phytoplankton Bloom Induced by Typhoons: Case Studies in the South China Sea
Table 1
Typhoon information and the spatial average chl-a concentration before and after typhoon overlaid on CCE.
| Typhoon’s name | Transit speed (m/s) | Average wind speed (m/s) | Minimum sea level pressure (mb) | Prestorm chl-a (mg/m3) | Poststorm chl-a (mg/m3) |
| Leo | 2.8864 | 49.901 | — | 0.1089 | 0.7174 | Lingling | 3.6846 | 55.487 | 927 | 0.1218 | 0.4750 | Nanmadol | 6.4741 | 40.127 | 967 | 0.1483 | 0.4323 | Kai-tak | 2.1016 | 29.581 | 963 | 0.1661 | 0.8212 | Chanchu | 2.7270 | 59.676 | 927 | 0.0847 | 0.3335 | Durian | 3.7176 | 44.156 | 954 | 0.1141 | 0.2664 | Utor | 4.8184 | 41.156 | 954 | 0.1141 | 0.2454 | Hagibis | 1.9072 | 31.438 | 982 | 0.1145 | 1.4338 |
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