对于受潮严重的表可适当延长吸潮时间。
For damp serious form can be extended to absorb moisture time.
利用验潮站海表高度差反演吐噶喇海峡黑潮的流量，分析了黑潮流量的年内和年际变化。
This paper USES TKC to reflect the volume transport of Kuroshio through the Tokara strait, analyzes the intra-annual and annual period of the volume of Kuroshio.
利用验潮站海表高度差反演吐噶喇海峡黑潮的流量，分析了黑潮流量的年内和年际变化。
This paper USES TKC to reflect the volume transport of Kuroshio through the Tokara strait, analyzes the intra-annual and annual period of the volume of Kuroshio.
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