02.035 主温跃层(main thermocline) 永久存在的温跃层,亦称永久性温跃层。 02.036 永久性温跃层(permanent thermocline) 永久存在的温跃层。
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航海航天行业专业英语第420页 ... magnetic tape recording current-meter 磁带记录式海流计 main thermocline 主(温)跃层 major constituents of sea water 海水主要成分 ...
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sea main thermocline [海洋] 海洋主温跃层
In summer, the temperature of the south part of the area is higher than the north part. Both the main thermocline and the main halocline are thin and their depths range from 50 to 120m.
第四章对历年温盐和表层流资料的进行了统计分析,给出了开辟区的温盐和表层流的分布特征和年变化特征:(1)表层水温在夏季呈南高北低的特点,温盐跃层较薄,中心位置在50~120米之间变化;
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.
主要结果如下:海表风应力是影响温跃层的动力因子,对季节性温跃层的深度和强度均有重大影响,但对大洋温跃层的影响不大;
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