当东北部海啸所形成的潮水到达苏兹贝格冰架时仅剩一英尺高了（30厘米），但是海浪的惯性施加的压力仍足以引起裂冰作用。

The swell from the Tohoku tsunami was likely only a foot high (30 cm) when it reached the Sulzberger Ice Shelf, but the consistency of the waves created enough stress to cause the calving.

youdao

当东北部海啸所形成的潮水到达苏兹贝格冰架时仅剩一英尺高了（30厘米），但是海浪的惯性施加的压力仍足以引起裂冰作用。

The swell from the Tohoku tsunami was likely only a foot high (30 cm) when it reached the Sulzberger Ice Shelf, but the consistency of the waves created enough stress to cause the calving.

youdao