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.
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.
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