seasonal thermocline

基本解釋

Besides the seasonal variation, the instantaneous wave of thermocline may occur under the effects of tide, wind mixing and rainfall, etc.
躍層除有季節(jié)性的變化外，還時刻受到潮汐、風(fēng)、降水等諸多因素擾動而引起波動與起伏。
Thermocline was mainly due to warming sea surface caused by the seasonal thermocline and wind mixing (also called "first duplex"), sometimes a "thermocline" phenomenon.
溫躍層主要是由于海面增溫和風(fēng)混合造成的季節(jié)性躍層（也稱“第一類躍層”），有時也出現(xiàn)“雙躍層”現(xiàn)象。
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The main conclusions are as follow: 1. The wind stress of sea surface is one dynamical factor of thermocline, which has important effect on intensity and depth of the seasonal thermocline.
主要結(jié)果如下：海表風(fēng)應(yīng)力是影響溫躍層的動力因子，對季節(jié)性溫躍層的深度和強度均有重大影響，但對大洋溫躍層的影響不大；