Ther mohaline finestructure and its relation with the water masses and currents system in the Northern East China Sea

Bao Xian-wen; Fang Xin-hua; Liu Xue-gang

doi:10.1007/BF02850369

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Ther mohaline finestructure and its relation with the water masses and currents system in the Northern East China Sea

Updated：2023-05-16

- Ther mohaline finestructure and its relation with the water masses and currents system in the Northern East China Sea
- Journal of Oceanology and Limnology Vol. 14, Issue 2, Pages: 128-134(1996)
- Affiliations：
  
  1. Physical Oceanography Institute
  2. North China Sea Administration
- Author bio：
- Funds：
- DOI：10.1007/BF02850369
  CLC：
- Online First：31 January 2013，
  
  Published：1996
- Accepted：
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Xian-wen, B., Xin-hua, F. & Xue-gang, L. Ther mohaline finestructure and its relation with the water masses and currents system in the Northern East China Sea., Chin. J. Ocean. Limnol. 14, 128–134 (1996). https://doi.org/10.1007/BF02850369
DOI：

Xian-wen, B., Xin-hua, F. & Xue-gang, L. Ther mohaline finestructure and its relation with the water masses and currents system in the Northern East China Sea., Chin. J. Ocean. Limnol. 14, 128–134 (1996). https://doi.org/10.1007/BF02850369 DOI：

摘要

Abstract

Eighty-one CTD profiles gathered in springtime were used for northern East China Sea thermohaline finestructure studies indicating that the finestructure properties varied with region and depth

as shown in finestructure spectra

distribution of Cox numbers

etc.

Some results closely related to distribution of water masses and currents. Analysis of two typical profiles revealed differences in autospectra of temperature

salinity and potential density gradients

probability distribution of temperature finestructure gradient

Cox numbers

etc. The probability density function of vertical temperature gradients

which varied with sample interval

is given. The variances of temperature finestructure gradient are used to estimate the lateral diffusivity {ie128-1} and lateral temperature flux

which were 10.3 (m2/s) and 5.5×10−4 (°C m/s). respectively.

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Keywords

references

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