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https://doi.org/10.5194/os-2019-62
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/os-2019-62
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.

Submitted as: research article 07 Aug 2019

Submitted as: research article | 07 Aug 2019

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A revised version of this preprint was accepted for the journal OS and is expected to appear here in due course.

Hydrographic survey over the Carlsberg Ridge in May 2012

Hailun He1, Yuan Wang2, Xiqiu Han2, Yanzhou Wei1, Pengfei Lin3, Zhongyan Qiu2, and Yejian Wang2 Hailun He et al.
  • 1State Key Laboratory of Satellite Ocean Environment Dynamics, Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou 310012, China
  • 2Key Laboratory of Submarine Geosciences, Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou 310012, China
  • 3State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China

Abstract. In May 2012, we conducted a hydrographic survey over the Carlsberg Ridge in the northwest Indian Ocean. In this paper, we use these station data, in combination with some free-floating Argo profiles, to obtain the sectional temperature and salinity fields, and subsequently, the hydrographic characteristics are comprehensively analyzed. Through the basic T-S diagram, three salty water masses, Arabian Sea High-Salinity Water, Persian Gulf Water, and Red Sea Water, are identified. The sectional data show a clear ventilation structure associated with Arabian Sea High-Salinity Water. The 35.8 psu salty water sinks at 6.9° N and extends southward to 4.4° N at depths around the thermocline, where the thermocline depth is in the range of 100 to 150 m. This salty thermocline extends much further south than the climatology indicates. Furthermore, the temperature and salinity data are used to compute the absolute geostrophic current over the specific section, and the results show meso-scale eddy vertical structure different from some widely used oceanic reanalysis data. We also find a west-propagating disturbance at 6° N, and the related features are described in terms of phase speed, horizontal and vertical structures.

Hailun He et al.

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Hailun He et al.

Hailun He et al.

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Latest update: 09 Jul 2020
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Short summary
Ocean profiling observation in Indian Ocean is not sufficient. We conducted a hydrographic survey on the Carlsberg Ridge, which is a mid-ocean ridge in northwest Indian Ocean, to obtain the snapshots of sectional temperature, salinity and density fields by combining the ARGO data. The results show a meso-scale eddy located along specific ridge and the existence of west-propagating disturbance. The results shed light on the regional ocean circulation.
Ocean profiling observation in Indian Ocean is not sufficient. We conducted a hydrographic...
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