Seasonal variation of the barrier layer in the PN section

Yuan Zhang; Dexing Wu; Xiaopei Lin; Feng Shan

doi:10.1007/s00343-009-9261-5

Your Location：

Home >

Browse articles >

Seasonal variation of the barrier layer in the PN section

OriginalPaper | Updated：2023-05-16

- Seasonal variation of the barrier layer in the PN section
- Seasonal variation of the barrier layer in the PN section
- 海洋湖沼学报（英文） 2009年27卷第2期页码：192-201
- Affiliations：
  
  1. Physical Oceanography Laboratory Ocean University of China
  2. First Institute of Oceanography SOA
- Author bio：
- Funds：
  
  Supported by National Basic Research Program of China (973 Program, No. 2005CB422303 and 2007CB411804), the Key Project of the International Science and Technology Cooperation Program of China (No. 2006DFB21250), the “111 Project” of the Ministry of Education (No. B07036), the Program for New Century Excellent Talents in University, China (No. NECT-07-0781)
- DOI：10.1007/s00343-009-9261-5
  中图分类号：
- 网络首发：2009-07-12，
  
  纸质出版：2009
- Accepted：
Scan QR Code
Seasonal variation of the barrier layer in the PN section[J]. 海洋湖沼学报（英文）, 2009,27(2):192-201.

Zhang, Y., Wu, D., Lin, X. et al. Seasonal variation of the barrier layer in the PN section., Chin. J. Ocean. Limnol. 27, 192–201 (2009). https://doi.org/10.1007/s00343-009-9261-5
Seasonal variation of the barrier layer in the PN section[J]. 海洋湖沼学报（英文）, 2009,27(2):192-201. DOI： 10.1007/s00343-009-9261-5.

Zhang, Y., Wu, D., Lin, X. et al. Seasonal variation of the barrier layer in the PN section., Chin. J. Ocean. Limnol. 27, 192–201 (2009). https://doi.org/10.1007/s00343-009-9261-5 DOI：

摘要

Abstract

In this paper

we use the conductivity-temperature-depth (CTD) observation data and a three-dimensional ocean model in a seasonally-varying forcing field to study the barrier layer (BL) in the PN section in the East China Sea (ECS). The BL can be found along the PN section with obviously seasonal variability. In winter

spring and autumn

the BL occurs around the slope where the cold shelf water meets with the warm Kuroshio water. In summer

the BL can also be found in the shelf area near salinity front of the Changjiang (Yangtze) River Dilution Water (YRDW). Seasonal variations of BL in the PN section are caused by local hydrological characteristics and seasonal variations of atmospheric forcing. Strong vertical convection caused by sea surface cooling thickens the BL in winter and spring in the slope area. Due to the large discharge of Changjiang River in summer

the BL occurs extensively in the shelf region where the fresh YRDW and the salty bottom water meet and form a strong halocline above the seasonal thermocline. The formation mechanism of BL in the PN section can be explained by the vertical shear of different water masses

which is called the advection mechanism. The interannual variation of BL in summer is greatly affected by the YRDW. In the larger YRDW year (such as 1998)

a shallow but much thicker BL existed on the shelf area.

关键词

Keywords

references

Bai, X. Z. and F. Wang, 2003. Numerical study on the mechanism of the expansion of the Changjiang River diluted water in summer. Oceanologia et Limnologia Sinica 34(6): 593–603. (in Chinese with English abstract)

Bao, X. W., X. P. Lin, D. X. Wu et al., 2005. Simulation and analysis of shelf circulation and its seasonal variability in the East China Sea. Journal of Ocean University of China 35(3): 349–356. (in Chinese with English abstract)

Breugem, W. P., P. Chang, C. J. Jang et al., 2007. Barrier layer and tropical Atlantic SST biases in coupled GCMs. Tellus A 60(5): 885–897.

Defant, A., 1961. Physical Oceanography. Pergamon, New York. p. 729.

Du, Y., D. X. Wang, P. Shi et al., 2004. Seasonal variation of the barrier layer in the South China Sea and its relationship to the sea surface flux. Chinese Journal of Atmospheric Sciences 28(1): 101–111. (in Chinese with English abstract)

Editorial Committee of the Ocean Atlas, 1993. Ocean Atlas of the Bohai Sea, Yellow Sea and East China Sea (Hydrology), Beijing, China. 524p. (in Chinese)

Fang, X. H., Y. L. Zhang and J. M. Wang, 1992. Quality Control of the CTD Data, Publishing Company of Ocean University of China, Qingdao, China. p. 1–200. (in Chinese)

Guo, X. Y., Y. Miyazawa and T. Yamagata, 2006. The Kuroshio onshore intrusion along the shelf break of the East China Sea: The origin of the Tsushima warm current. J. Phys.Oceanogr. 36: 2 205–2 231.

Ichikawa, H. and R. C. Beardsley, 2002. The current system in the Yellow Sea and East China Sea. Journal of Oceanography 58: 77–92.

Jia, X. J., Q. Y. Liu et al., 2001. A comparison between two different definitions of the mixlayer and the thermocline in the South China Sea. Transactions of Oceanology and Limnology 1: 1–7.

Li, F. Q., Y. Li and J. Xie, 2003. Fitting Method and Application of Membership Function of Water Masses at Subsurface and Intermediate Layer in the Oceans. Journal of Ocean University of China 33(6): 833–840. (in Chinese with English abstract)

Li, F. Q., J. Xie and T. T. Zu, 2004. Fitting method of membership function of the oceanic subsurface intermediate mixing water mass and analysis of water masses in the South China Sea. Periodial of Ocean University of China 34(5): 861–86.

Lindstrom, E., R. Lukas and R. Fine, 1987. The western equatorial Pacific Ocean circulation study. Nature 330: 533–537.

Maes, C. and J. Picaut 2005. Importance of the salinity barrier layer for the buildup of El Niño. J. Climate 18: 104–118.

Masson, S., J. J. Luo, G. Madec et al., 2005. Impact of barrier layer on winter-spring variability of the southeastern Arabian Sea. Geopys. Res. Lett. 32: 1–4.

Meghan, F. C. and J. M. Michael, 2002. Barrier layer formation during westerly wind bursts. J. Geophys. Res. 107(C12), 8020, doi:10.1029/2001JC001171.

Pan, A. J., X. F. Wan, J. D. Xu et al., 2006. Characteristics and forming mechanism of the barrier layer in the northeastern of the South China Sea. Chinese Science Bulletin 51: 951–957. (in Chinese with English abstract)

Pan, A. J., X. F. Wan, H. Y. Chen et al., 2009. Diurnal evolution of the barrier layer and its local feedback. Chinese Science (in press).

Peter, C., Q. Y. Liu, Y. L. Jia et al., 2002. Evidence of a barrier layer in the Sulu and Celebes Seas. J. Phys. Oceanogr. 32: 3 299–3 309.

Qiao, F. L., J. Ma, C. S. Xia et al., 2004. Influence of the wave and tide-induced mixing for the vertial temperature structure in summer. Progress in Natural Science 14(12): 1 434–1 441.

Qiao, F. L., Y. L. Yuan, Y. Z. Yang et al., 2004. Wave induced mixing in the upper ocean: Distributionand application to a global ocean circulation model. Geophys Res. Lett. 31: L11303.

Qu, T. D. and M. Gary, 2005. Seasonal variation of barrier layer in the southeastern tropical Indian Ocean. J. Geophys. Res. 110: 1 029–1 039.

Smyth, W. D., P. O. Zavialov and J. N. Moum, 1997. Decay of turbulence in the upper ocean following sudden isolation from surface forcing. J. Phys. Oceanogr. 27: 810–822.

Soloviev, A. and R. Lukas, 1996. Observation of spatial variability of diurnal thermocline and rain-formed halocline in the western Pacific warm pool. J. Phys. Oceanogr. 26: 2 529–2 538.

Sprintall, J. and M. Tomczak, 1992. Evidence of the barrier layer in the surface layer of the tropics. J. Geophys. Res. 97: 7 305–7 316. (in Chinese with English abstract)

Su, J., 2001. A review of circulation dynamics of the coastal oceans near China. Acta Oceanologica Sinica. 23(supp.4): 1–16.

Vialard, J. and P. Delecluse, 1998a. An OGCM study for the TOGA decade, Part I, Role of salinity in the physics of the western Pacific fresh pool. J. Phys. Oceanogr. 28: 1 071–1 088.

Vialard, J. and P. Delecluse, 1998b. An OGCM study for the TOGA decade, part II, Barrier layer formation and variability. J. Phys. Oceanogr. 28: 1 089–1 106.

Wijesekera, H. W. and M. C. Gregg, 1996. Surface layer response to weak winds, westerly bursts, and rain squalls in the western Pacific warm pool. J. Geophys. Res. 101: 977–997.

Wijesekera, H. W., C. A. Paulson and A. Huyer, 1999. The effect of rainfall on the surface layer during a westerly wind burst in the western equatorial Pacific. J. Phys. Oceanogr. 29: 612–632.

Wu, W. and M. Tomxzak, 2001. The barrier layer in the southern area of the South China Sea. Chinese Science Bulletin 46(7): 590–594. (in Chinese with English abstract)

Wu, W., X. H. Fang and D. X. Wu, 2001. On the methods of determining the depths of thermocline, halocline and pycnocline. Transaction of Oceanology and Limnology 2: 1–7.

You, Y. Z., 1995. Salinity variability and its role in the barrier layer formation during TOGA-COARE. J. Phys. Oceanogr. 25: 2 778–2 807.

You, Y. Z., 1998. Rain-formed barrier layer of the western equatorial Pacific Warm Pool: A case study. J. Phys. Oceanogr. 103: 5 361–5 378.

Zhang, X. D., G. Y. Zhang, K. Tong et al., 2004. Water mass analysis of the source area of Kuroshio. Marine Science Bulletin 23(1): 15–21. (in Chinese with English abstract)

Zhang, Y., D. X. Wu and X. P. Lin, 2006. The Study of thermocline and pycnocline calculation in the East China Sea in summer. Journal of Ocean University of China 36(3): 1–7. (in Chinese with English abstract)

Zhu, J. R., C. Y. Xiao and H. T. Shen, 1998. Numerical model simulation of expansion of Changjiang diluted water in summer. Acta Oceanologica Sinca 20(5): 13–22. (in Chinese with English abstract)

Zou, E. M., B. H. Guo and Y. X. Tang, 2001. An analysis of summer hydrographic features and circulation in the southern Yellow Sea and the northern East China Sea. Oceanologia et Limnologia Sinica 32(3): 340–348. (in Chinese with English abstract)

浏览量

Downloads

CSCD

文章被引用时，请邮件提醒。

Submit

工具集

关联资源

Intraseasonal variability of the Kuroshio observed via mooring at 18°N

Effects of multiple dynamic processes on chlorophyll variation in the Luzon Strait in summer 2019 based on glider observation

Effects of dissolved oxygen and nutrients from the Kuroshio on hypoxia off the Changjiang River estuary

Numerical study on interaction between eddies and the Kuroshio Current east of Taiwan, China

Statistical analysis of intensity variations in tropical cyclones in the East China Sea passing over the Kuroshio