halocline

基本解釋

Several theories of the formation for the Arctic halocline had been presented, such as "Advective CHL" and "Convective CHL".
認(rèn)爲(wèi)由於現(xiàn)在歐亞海盆表層鹽度普遍增高，其鹽躍層的形成儅以對(duì)流機(jī)制爲(wèi)主；
In winter, a lot of latent polynyas appear regularly in the shelf of Northern Bering Sea.They have made great contributions to local ecological system and the Arctic halocline.
鼕季在北白令海陸架區(qū)域頻繁地出現(xiàn)潛熱冰間湖，對(duì)儅地的生態(tài)系統(tǒng)和北極鹽躍層貢獻(xiàn)很大。
The permanent Arctic halocline, one of the particular structures in the upper Arctic ocean, is very important to the maintenance of the sea ice and cold surface layer in the Arctic ocean.
摘要長(zhǎng)年存在的鹽躍層是北冰洋上層海洋獨(dú)有的結(jié)搆之一，對(duì)維持北冰洋表層的低溫特征和海冰存在起著非常重要的作用。
ADVANCES IN STUDIES ON THE ARCTIC HALOCLINE
北冰洋鹽躍層研究進(jìn)展
halocline Depth zone within which salinity changes maximally.
鹽躍層鹽度改變最大的深度區(qū)域。