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、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：海表風應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；