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Drag increment due to internal waves generated by Rankine ovoid
引用本文:XU Zhaoting,ZHOU Xiwu,CHEN Xu. Drag increment due to internal waves generated by Rankine ovoid[J]. 自然科学进展(英文版), 2002, 12(11): 849-853
作者姓名:XU Zhaoting  ZHOU Xiwu  CHEN Xu
作者单位:Institute of Physical Oceanography and Physical Oceanography Laboratory, Ocean University of Qingdao, Qingdao 266003, China;Key Laboratory of Marine Science and Numerical Modeling of State Oceanic Administration, Qingdao 266061, China,Institute of Physical Oceanography and Physical Oceanography Laboratory, Ocean University of Qingdao, Qingdao 266003, China,Institute of Physical Oceanography and Physical Oceanography Laboratory, Ocean University of Qingdao, Qingdao 266003, China
基金项目:Supported by the National Natural Science Foundation of China (Grant No.49776284), The Research Fund for the Doctoral Program of Higher Education (No.2000042309) and 99JS21.6.1.JW1002
摘    要:The experimental results on drag increment caused by internal waves, which are generated by a Rankine ovoid towed horizontally at constant velocities in a two-layer stratified water (a strong pycnocline) initially at rest, are presented. The drag increment due to stratification is obtained experimentally as a function of internal Froude number Frd and Reynolds number Re. From the results, it is shown that as a function of Frd or Re, an increment in mean drag coefficient due to stratification ΔCd has both increasing and decreasing region attributable respectively to internal wave and to collapse of mixing fluids in the wakes. A most significant result shows that when Frd=0.838 there exists a maximum of ΔCd, which is equal to 0.05 in the exciting region of the strong internal wave generation.

关 键 词:internal wave   wake   stratified flow   drag increment

Drag increment due to internal waves generated by Rankine ovoid
Xu Zhaoting,ZHOU Xiwu,CHEN Xu. Drag increment due to internal waves generated by Rankine ovoid[J]. Progress in Natural Science, 2002, 12(11): 849-853
Authors:Xu Zhaoting  ZHOU Xiwu  CHEN Xu
Affiliation:1. Institute of Physical Oceanography and Physical Oceanography Laboratory, Ocean University of Qingdao, Qingdao 266003, China;Key Laboratory of Marine Science and Numerical Modeling of State Oceanic Administration, Qingdao 266061, China
2. Institute of Physical Oceanography and Physical Oceanography Laboratory, Ocean University of Qingdao, Qingdao 266003, China
Abstract:The experimental results on drag increment caused by internal waves, which are generated by a Rankine ovoid towed horizontally at constant velocities in a two-layer stratified water (a strong pycnocline) initially at rest, are presented. The drag increment due to stratification is obtained experimentally as a function of internal Froude number Frd and Reynolds number Re. From the results, it is shown that as a function of Frd or Re, an increment in mean drag coefficient due to stratification ΔCd has both increasing and decreasing region attributable respectively to internal wave and to collapse of mixing fluids in the wakes. A most significant result shows that when Frd=0.838 there exists a maximum of ΔCd, which is equal to 0.05 in the exciting region of the strong internal wave generation.
Keywords:internal wave   wake   stratified flow   drag increment
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