scholarly journals Meridional transport of North Pacific Intermediate Water across 37°N based on an objective analysis of lowered acoustic Doppler current profiler data

2004 ◽  
Vol 109 (C2) ◽  
Author(s):  
Hiroshi Yoshinari
2016 ◽  
Vol 1 (2) ◽  
pp. 17
Author(s):  
Dewi Surinati ◽  
Edi Kusmanto

<strong>Stratification of Water Mass in Lasolo Bay, Southeast Sulawesi.</strong> As a nature conservation area, Lasolo Bay should be supported by data and information of waters oceanographic. Research for stratification of water masses in Lasolo Bay was conducted. from 10 to 19 July 2011. Temperature and salinity data were obtained using CTD SBE 911 Plus preinstalled on Research Vessel Baruna Jaya VIII at intervals of 24 data per second. Current data were obtained using Vessel Mounted Acoustic Doppler Current Profiler (VMADCP) with an interval of two seconds. The results show that there are differences in the speed and direction of currents in the water column that lead to stratification of water masses. Currents that drove the water mass of Banda Sea into Lasolo Bay was caused by southeasterly winds with an average speed of 4.1 m/s. At depths of 0–50 m and 100–200 m the current dominance occurs to the northwest, while at depths of 50–100 m and 200–350 m it occurs to the south. The water mass with a salinity of 32.1–34.0 PSU and temperature 26–28°C occupied the surface layer (0–50 m). The water mass with a salinity of 34.4–34.5 PSU identified as the water mass of North Pacific Intermediate Water (NPIW) occupied two depths, i.e. 50–100 m and 200–350 m with different range of temperatures. The water mass with maximum salinity (34.5–34.6 PSU), identified as the water mass of North Pacific Subtropical Water (NPSW) also occupied two depths i.e. 100–200 m and 350 m until near the bottom with different range of temperatures<br /><br />


2021 ◽  
Vol 6 (2) ◽  
pp. 97
Author(s):  
Adi Purwandana ◽  
Mochamad Riza Iskandar ◽  
Edi Kusmanto ◽  
Muhammad Fadli ◽  
Priyadi Dwi Santoso ◽  
...  

<strong>Vertical mixing in the northern Maluku Sea and Talaud Waters in February 2021. </strong>The spatial variability of water mass mixing in the northern Maluku Sea and Talaud waters are presented based on the results of Eastern Indonesia Expedition (EIT) 2021 using RV Baruna Jaya VIII-LIPI. The turbulent kinetic energy dissipation rate was obtained using the Kunze-Williams-Briscoe (KWB) Method calculated from CTD (Conductivity, Temperature, Depth) and LADCP (Lowered Acoustic Doppler Current Profiler) datasets. We found the dissipation rate in the core layer of North Pacific Subtropical Water (NPSW) and North Pacific Intermediate Water (NPIW) are in the order of 10<sup>-6</sup> W/kg and 10<sup>-8</sup> W/kg, respectively. The KWB Method used in this study is also proven comparable with the Thorpe Method.


2001 ◽  
Vol 28 (18) ◽  
pp. 3445-3448 ◽  
Author(s):  
Hiroshi Yoshinari ◽  
Ichiro Yasuda ◽  
Shin-ichi Ito ◽  
Eric Firing ◽  
Yutaka Matsuo ◽  
...  

2008 ◽  
Author(s):  
Annett B. Sullivan ◽  
Michael L. Deas ◽  
Jessica Asbill ◽  
Julie D. Kirshtein ◽  
Kenna D. Butler ◽  
...  

2007 ◽  
Vol 34 (2) ◽  
Author(s):  
Shinya Kouketsu ◽  
Ikuo Kaneko ◽  
Takeshi Kawano ◽  
Hiroshi Uchida ◽  
Toshimasa Doi ◽  
...  

1996 ◽  
Vol 52 (4) ◽  
pp. 475-490 ◽  
Author(s):  
Takayuki Tokieda ◽  
Shuichi Watanabe ◽  
Shizuo Tsunogai

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