琉球海流是琉球群岛以东一支东北向的西边界流。
The Ryukyu current is a northeastward and western boundary current east of Ryukyu Islands.
冷涌爆发后，斧形干区南压过程中演变为倒T形干区，之后倒T形干区转变为西南东北向的带状干区进入南海海面。
After outbreak, the axe-shape arid region is turning into the inverted T shape as moving to south, followed by turning to southwest-northeast zonal arid region and moving to South China Sea.
冷涌爆发后，斧形干区南压过程中演变为倒T形干区，之后倒T形干区转变为西南东北向的带状干区进入南海海面。
After outbreak, the axe-shape arid region is turning into the inverted T shape as moving to south, followed by turning to southwest-northeast zonal arid region and moving to South China Sea.
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