晴天小希希
(One) storm is damp main characteristic Storm is damp point to intense atmosphere of reason perturbation motion, elevate phenomenon if the sea surface that tropics cyclone (stage manner , furacan) , temperate zone cyclone (cold wave) etc. arouses is abnormal. Examine sea surface recorded by tide station or river mouth gaging station along the coast going up and down, tide, (earthquake) seaquake and their his long wave vibrates generally for astronomy tide , storm arousing the synthetical characteristic that sea surface changes. Examine the tide device in general already filtering the sea surface that the minor-cycle sea wave having decreased by several seconds of level arouses undulating. Climax folds up each other (especially and the climax during astronomy spring tide looks at and appraises a pack) fitly with astronomy if storm is damp, storm of adding sometimes lined fierce storm of tide but extremely, go against rivers flood but upper
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