Tidal and residual currents across the northern Ryukyu Island chain observed by ferryboat ADCP

2017 ◽  
Vol 122 (9) ◽  
pp. 7198-7217 ◽  
Author(s):  
Zhao-Jun Liu ◽  
Hirohiko Nakamura ◽  
Xiao-Hua Zhu ◽  
Ayako Nishina ◽  
Menghong Dong
Keyword(s):  
Ryukyu Island ◽  
Residual Currents ◽  
Tidal And Residual Currents

The observed tidal and residual currents in the Andaman Sea during the second half of 2016

2018 ◽  
Vol 37 (9) ◽  
pp. 13-21 ◽  
Author(s):  
Yanliang Liu ◽  
Jingsong Guo ◽  
Huiwu Wang ◽  
Yuhuan Xue ◽  
Somkiat Khokiattiwong ◽  
...  
Keyword(s):  
Andaman Sea ◽  
Residual Currents ◽  
Tidal And Residual Currents

Measurement of tidal and residual currents in the Strait of Hormuz

2016 ◽  
Vol 178 ◽  
pp. 101-109 ◽  
Author(s):  
Jafar Azizpour ◽  
Seyed Mostafa Siadatmousavi ◽  
Vahid Chegini
Keyword(s):  
Residual Currents ◽  
Strait Of Hormuz ◽  
Tidal And Residual Currents

Tidal and residual currents over abrupt deep-sea topography based on shipboard ADCP data and tidal model solutions for three popular bathymetry grids

2013 ◽  
Vol 63 (2-3) ◽  
pp. 195-208 ◽  
Author(s):  
Christian Mohn ◽  
Svetlana Erofeeva ◽  
Robert Turnewitsch ◽  
Bernd Christiansen ◽  
Martin White
Keyword(s):  
Deep Sea ◽  
Tidal Model ◽  
Residual Currents ◽  
Model Solutions ◽  
Tidal And Residual Currents ◽  
Adcp Data

Tidal and residual currents in the Bransfield Strait, Antarctica

1994 ◽  
Vol 12 (9) ◽  
pp. 887-902 ◽  
Author(s):  
O. López ◽  
M. A. García ◽  
A. S.-Arcilla
Keyword(s):  
Time Series ◽  
Tidal Flow ◽  
Relative Importance ◽  
Tide Gauges ◽  
Recording Equipment ◽  
Residual Currents ◽  
Bransfield Strait ◽  
Operation Period ◽  
Dense Grid ◽  
Tidal And Residual Currents

Abstract. During the 1992-1993 oceanographic cruise of the Spanish R/V Hespérides, recording equipment was deployed in the Bransfield Strait. Six Aanderaa RCM7 current meters and three Aanderaa WLR7 tide gauges were successfully recovered after an operation period of 2.5 months. Relevant features of the time series obtained are presented and discussed in this paper. The emphasis is placed on the tidal character of the currents and the relative importance of tidal flow in the general hydrodynamics of the strait. For these purposes a dense grid of hydrographic stations, completed during the BIOANTAR 93 cruise, is used. Preliminary geostrophic calculations relative to a 400 m depth, yield current velocities of around 0.20 m s-1 in the study area, whereas the magnitude of tidal currents is seen to be 0.30-0.40 m s-1.

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