LEADER 03760nam 2200829z- 450 001 9910576874003321 005 20231214132828.0 035 $a(CKB)5720000000008435 035 $a(oapen)https://directory.doabooks.org/handle/20.500.12854/84601 035 $a(EXLCZ)995720000000008435 100 $a20202206d2022 |y 0 101 0 $aeng 135 $aurmn|---annan 181 $ctxt$2rdacontent 182 $cc$2rdamedia 183 $acr$2rdacarrier 200 10$aOceanic Internal Waves and Internal Tides in the East Asian Marginal Seas 210 $cMDPI - Multidisciplinary Digital Publishing Institute$d2022 215 $a1 electronic resource (126 p.) 311 $a3-0365-4213-2 311 $a3-0365-4214-0 330 $aOceanic 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. 606 $aTechnology: general issues$2bicssc 606 $aHistory of engineering & technology$2bicssc 610 $anear-inertial waves 610 $atyphoon Megi 610 $aSouth China Sea 610 $ahybrid coordinate ocean model reanalysis results 610 $aLuzon Strait 610 $abaroclinic tides 610 $astratification variability 610 $aMITgcm 610 $anonlinear internal wave 610 $apropagating speed 610 $apropagating direction 610 $aunderway observation 610 $amoored observation 610 $aEast China Sea 610 $ainternal solitary wave 610 $ashipboard observation 610 $aextreme current velocity 610 $awave breaking 610 $atrapped core 610 $anear-inertial internal waves 610 $anonseasonal variability 610 $amesoscale flow field 610 $arelative vorticity 610 $aOkubo-Weiss parameter 610 $asubsurface mooring 610 $asouthwestern East Sea 610 $aJapan Sea 610 $ainternal waves 610 $aHainan Island 610 $aKRI nanggala-402 submarine wreck 610 $aLombok Strait 610 $aBali Sea 610 $ainternal solitary waves 610 $aremote sensing images 610 $aunderwater noise 610 $aflow noise 610 $avortex-induced vibration 610 $athe South China Sea 615 7$aTechnology: general issues 615 7$aHistory of engineering & technology 700 $aNam$b SungHyun$4edt$01296670 702 $aChen$b Xueen$4edt 702 $aNam$b SungHyun$4oth 702 $aChen$b Xueen$4oth 906 $aBOOK 912 $a9910576874003321 996 $aOceanic Internal Waves and Internal Tides in the East Asian Marginal Seas$93024202 997 $aUNINA