盐跃层

盐跃层（Halocline）是指有明显盐度梯度的海水层[1]，它位於海洋表层水之下。一般位於50-200公尺之間。其盐度随深度而迅速增加。研究海水盐度及其梯度可提供水团起源和运动的重要线索[2].

参考文献
  1. White, William B; Culver, David C (2012). Encyclopedia of Caves. Academic Press. p. 157. ISBN 978-0-12-383832-2.
  2. Garrison, Tom (2006). Enhanced Essentials of Oceanography. Cengage Learning. p. 115. ISBN 0-495-11372-7.
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