

FOLLOWUS
1.Key Laboratory of Ocean Circulation and Waves, Institute of Oceanology, Center for Ocean Mega-Science, Chinese Academy of Sciences, Qingdao 266071, China
2.Laboratory for Ocean and Climate Dynamics, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266000, China
3.Institute of Acoustics, Chinese Academy of Sciences, Beijing 100190, China
4.University of Chinese Academy of Sciences, Beijing 100049, China
WANG Fan, fwang@qdio.ac.cn
收稿:2020-04-02,
录用:2020-4-26,
网络首发:2020-03-03,
纸质出版:2020-07
Scan QR Code
The development of a new real-time subsurface mooring[J]. 海洋湖沼学报(英文), 2020,38(4):1080-1091.
Fan WANG, Jianing WANG, Lijun XU, et al. The development of a new real-time subsurface mooring[J]. Journal of Oceanology and Limnology, 2020, 38(4): 1080-1091.
The development of a new real-time subsurface mooring[J]. 海洋湖沼学报(英文), 2020,38(4):1080-1091. DOI: 10.1007/s00343-020-0144-0.
Fan WANG, Jianing WANG, Lijun XU, et al. The development of a new real-time subsurface mooring[J]. Journal of Oceanology and Limnology, 2020, 38(4): 1080-1091. DOI: 10.1007/s00343-020-0144-0.
Subsurface mooring allows researchers to measure the ocean properties such as water temperature
salinity
and velocity at several depths of the water column for a long period. Traditional subsurface mooring can release data only after recovered
which constrains the usage of the subsurface and deep layer data in the ocean and climate predictions. Recently
we developed a new real-time subsurface mooring (RTSM). Velocity profiles over upper 1 000 m depth and layered data from sensors up to 5 000 m depth can be realtime transmitted to the small surface buoy through underwater acoustic communication and then to the office through Beidou or Iridium satellite. To verify and refine their design and data transmission process
we deployed more than 30 sets of RTSMs in the western Pacific to do a 1-year continuous run during 2016-2018. The continuous running period of RTSM in a 1-year cycle can reach more than 260 days on average
and more than 95% of observed data can be successfully transmitted back to the office. Compared to the widely-used inductive coupling communication
wireless acoustic communication has been shown more applicable to the underwater sensor network with large depth intervals and long transmission distance to the surface.
K Ando , Y Kuroda , Y Fujii , T Fukuda , T Hasegawa , T Horii , Y Ishihara , Y Kashino , Y Masumoto , K Mizuno , M Nagura , I Ueki . Fifteen years progress of the TRITON array in the Western Pacific and Eastern Indian Oceans . Journal of Oceanography , 2017 . 73 ( 4 ): 403 - 426 . DOI: 10.1007/s10872-017-0414-4 http://doi.org/10.1007/s10872-017-0414-4 .
A Baggeroer . Acoustic telemetry-an overview . IEEE Journal of Oceanic Engineering , 1984 . 9 ( 4 ): 229 - 235 . DOI: 10.1109/JOE.1984.1145629 http://doi.org/10.1109/JOE.1984.1145629 .
A G Barnston , M K Tippett , M L L'Heureux , S H Li , D G DeWitt . Skill of real-time seasonal ENSO model predictions during 2002-11: is our capability increasing? . Bulletin of the American Meteorological Society , 2012 . 93 ( 5 ): 631 - 651 . DOI: 10.1175/BAMS-D-11-00111.1 http://doi.org/10.1175/BAMS-D-11-00111.1 .
F Bonjean , G S E Lagerloef . Diagnostic model and analysis of the surface currents in the tropical Pacific Ocean . Journal of Physical Oceanography , 2002 . 32 ( 10 ): 2 938 - 2 954 . DOI: 10.1175/1520-0485(2002)032<2938:DMAAOT>2.0.CO;2 http://doi.org/10.1175/1520-0485(2002)032<2938:DMAAOT>2.0.CO;2 .
A J Clarke . El Niño physics and El Niño predictability . Annual Review of Marine Science , 2014 . 6 79 - 99 . DOI: 10.1146/annurev-marine-010213-135026 http://doi.org/10.1146/annurev-marine-010213-135026 .
J Gao , J N Wang , F Wang . Response of near-inertial shear to wind stress curl and sea level . Scientific Reports , 2019 . 9 ( 1 ): 20417 DOI: 10.1038/s41598-019-56822-z http://doi.org/10.1038/s41598-019-56822-z .
I Hoteit , B Cornuelle , P Heimbach . An eddy-permitting, dynamically consistent adjoint-based assimilation system for the tropical Pacific: hindcast experiments in 2000 . Journal of Geophysical Research: Oceans , 2010 . 115 ( C3 ): C03001 DOI: 10.1029/2009JC005437 http://doi.org/10.1029/2009JC005437 .
J Y Hu , W S Duan . Relationship between optimal precursory disturbances and optimally growing initial errors associated with ENSO events: implications to target observations for ENSO prediction . Journal of Geophysical Research: Ocean , 2016 . 121 ( 5 ): 2 901 - 2 917 . DOI: 10.1002/2015JC011386 http://doi.org/10.1002/2015JC011386 .
J Y Hu , W S Duan , Q Zhou . Season-dependent predictability and error growth dynamics for La Niña predictions . Climate Dynamics , 2019 . 53 ( 1-2 ): 1 063 - 1 076 . DOI: 10.1007/s00382-019-04631-5 http://doi.org/10.1007/s00382-019-04631-5 .
A Köhl . Influence of assimilating transports and in situ data from the Rapid-MOCHA array into the GECCO 2 ocean synthesis . Dynamics of Atmospheres and Oceans , 2015 . 72 38 - 51 . DOI: 10.1016/j.dynatmoce.2015.09.001 http://doi.org/10.1016/j.dynatmoce.2015.09.001 .
Q Ma , F Wang , J N Wang , Y Lyu . Intensified deep ocean variability induced by topographic Rossby waves at the Pacific Yap‐Mariana Junction . Journal of Geophysical Research: Oceans , 2019 . 124 ( 1 ): 8 360 - 8 374 . DOI: 10.1029/2019JC015490 http://doi.org/10.1029/2019JC015490 .
Morrison A T, Billings J D, Doherty K W. 2000. The McLane moored profiler: an autonomous platform for oceanographic measurements. In: Proceedings of OCEANS 2000 MTS/IEEE Conference and Exhibition.IEEE, Providence, RI, USA. p.353-358, https://doi.org/10.1109/oceans.2000.881284 https://doi.org/10.1109/oceans.2000.881284 . 10.1109/oceans.2000.881284
U Send , G Fowler , G Siddall , B Beanlands , M Pittman , C Waldmann , J Karstensen , R Lampitt . SeaCycler: a moored open-ocean profiling system for the upper ocean in extended self-contained deployments . Journal of Atmospheric and Oceanic Technology , 2013 . 30 ( 7 ): 1 555 - 1 565 . DOI: 10.1175/JTECH-D-11-00168.1 http://doi.org/10.1175/JTECH-D-11-00168.1 .
L N Song , Y L Li , J N Wang , F Wang , S J Hu , C Y Liu , X Y Diao , C Guan . Tropical meridional overturning circulation observed by subsurface moorings in the Western Pacific . Scientific Reports , 2018 . 8 ( 1 ): 7 632 DOI: 10.1038/s41598-018-26047-7 http://doi.org/10.1038/s41598-018-26047-7 .
C Tian , Z D Deng , X Y Xu , Q X Yang , W Zhao . Timed communication buoy system: a subsurface mooring system for efficient sensor data recovery . Marine Technology Society Journal , 2015 . 49 ( 3 ): 117 - 126 . DOI: 10.4031/MTSJ.49.3.7 http://doi.org/10.4031/MTSJ.49.3.7 .
F Wang , J N Wang , C Guan , Q Ma , D X Zhang . Mooring observations of equatorial currents in the upper 1000 m of the western Pacific Ocean during 2014 . Journal of Geophysical Research: Oceans , 2016 . 121 ( 6 ): 3 730 - 3 740 . DOI: 10.1002/2015JC011510 http://doi.org/10.1002/2015JC011510 .
J N Wang , Y Y Lu , F Wang , R H Zhang . Surface current in "hotspot" serves as a new and effective precursor for El Niño prediction . Scientific Reports , 2017 . 7 ( 1 ): 166 DOI: 10.1038/s41598-017-00244-2 http://doi.org/10.1038/s41598-017-00244-2 .
J Y Xi , S F Yan , L J Xu . Direct-adaptation based bidirectional turbo equalization for underwater acoustic communications: algorithm and undersea experimental results . The Journal of the Acoustical Society of America , 2018 . 143 ( 5 ): 2 715 - 2 728 . DOI: 10.1121/1.5036730 http://doi.org/10.1121/1.5036730 .
Z X Zhang , L J Pratt , F Wang , J N Wang , S W Tan . Intermediate intraseasonal variability in the western tropical Pacific Ocean: meridional distribution of equatorial Rossby waves influenced by a tilted boundary . Journal of Physical Oceanography , 2020 . 50 ( 4 ): 921 - 933 . DOI: 10.1175/JPO-D-19-0184.1 http://doi.org/10.1175/JPO-D-19-0184.1 .
0
浏览量
0
Downloads
2
CSCD
关联资源
相关文章
相关作者
相关机构

京公网安备11010802024621