Oceanic Internal Waves and Internal Tides in the East Asian Marginal Seas

Oceanic internal waves (IWs) at frequencies from local inertial (e.g., near-inertial internal waves) to buoyancy frequencies (nonlinear internal waves or internal solitary waves), sometimes including diurnal and semidiurnal tidal frequencies, play an important role in redistributing heat, momentum,...

Full description

Saved in:
Bibliographic Details
HerausgeberIn:
Sonstige:
Year of Publication:2022
Language:English
Physical Description:1 electronic resource (126 p.)
Tags: Add Tag
No Tags, Be the first to tag this record!
LEADER 03542nam-a2200781z--4500
001 993544461804498
005 20231214132828.0
006 m o d
007 cr|mn|---annan
008 202206s2022 xx |||||o ||| 0|eng d
035 |a (CKB)5720000000008435 
035 |a (oapen)https://directory.doabooks.org/handle/20.500.12854/84601 
035 |a (EXLCZ)995720000000008435 
041 0 |a eng 
100 1 |a Nam, SungHyun  |4 edt 
245 1 0 |a Oceanic Internal Waves and Internal Tides in the East Asian Marginal Seas 
260 |b MDPI - Multidisciplinary Digital Publishing Institute  |c 2022 
300 |a 1 electronic resource (126 p.) 
336 |a text  |b txt  |2 rdacontent 
337 |a computer  |b c  |2 rdamedia 
338 |a online resource  |b cr  |2 rdacarrier 
520 |a Oceanic internal waves (IWs) at frequencies from local inertial (e.g., near-inertial internal waves) to buoyancy frequencies (nonlinear internal waves or internal solitary waves), sometimes including diurnal and semidiurnal tidal frequencies, play an important role in redistributing heat, momentum, materials, and energy via turbulent mixing. IWs are found ubiquitously in many seas, including East Asian marginal seas (Indonesian Seas, South China Sea, East China Sea, Yellow Sea, and East Sea or Japan Sea), significantly affecting underwater acoustics, coastal and offshore engineering, submarine navigation, biological productivity, and the local and global climate. Despite decades of study on the IWs in some regions, our understanding of the IWs in the East Asian marginal seas is still in a primitive state and the mechanisms underlying every stage (generation, propagation, evolution, and dissipation) of IWs are not always clear. This Special Issue includes papers related to all fields of both low- and high-frequency IW studies in the specified region, including remote sensing, in situ observations, theories, and numerical models. 
546 |a English 
650 7 |a Technology: general issues  |2 bicssc 
650 7 |a History of engineering & technology  |2 bicssc 
653 |a near-inertial waves 
653 |a typhoon Megi 
653 |a South China Sea 
653 |a hybrid coordinate ocean model reanalysis results 
653 |a Luzon Strait 
653 |a baroclinic tides 
653 |a stratification variability 
653 |a MITgcm 
653 |a nonlinear internal wave 
653 |a propagating speed 
653 |a propagating direction 
653 |a underway observation 
653 |a moored observation 
653 |a East China Sea 
653 |a internal solitary wave 
653 |a shipboard observation 
653 |a extreme current velocity 
653 |a wave breaking 
653 |a trapped core 
653 |a near-inertial internal waves 
653 |a nonseasonal variability 
653 |a mesoscale flow field 
653 |a relative vorticity 
653 |a Okubo-Weiss parameter 
653 |a subsurface mooring 
653 |a southwestern East Sea 
653 |a Japan Sea 
653 |a internal waves 
653 |a Hainan Island 
653 |a KRI nanggala-402 submarine wreck 
653 |a Lombok Strait 
653 |a Bali Sea 
653 |a internal solitary waves 
653 |a remote sensing images 
653 |a underwater noise 
653 |a flow noise 
653 |a vortex-induced vibration 
653 |a the South China Sea 
776 |z 3-0365-4213-2 
776 |z 3-0365-4214-0 
700 1 |a Chen, Xueen  |4 edt 
700 1 |a Nam, SungHyun  |4 oth 
700 1 |a Chen, Xueen  |4 oth 
906 |a BOOK 
ADM |b 2023-12-15 05:32:29 Europe/Vienna  |f system  |c marc21  |a 2022-07-02 22:45:44 Europe/Vienna  |g false 
AVE |i DOAB Directory of Open Access Books  |P DOAB Directory of Open Access Books  |x https://eu02.alma.exlibrisgroup.com/view/uresolver/43ACC_OEAW/openurl?u.ignore_date_coverage=true&portfolio_pid=5337631100004498&Force_direct=true  |Z 5337631100004498  |b Available  |8 5337631100004498