01257nam--2200385---450-99000272966020331620060405150956.0000272966USA01000272966(ALEPH)000272966USA0100027296620060405d1980----km-y0itay0103----baengUS||||||||001yy<<An>> assessment of energy requirements in proven and new copper processesfinal report[Charles H. Pitt and Milton E. Wadsworth]Salt Lake City, UtahUniversity of Utah1980xiv, 362 p.ill.28 cm20012001001-------2001Industria metallurgica669.1PITT,Charles H.592972WADSWORTH,Milton E.95191University of Utah: Department of Metallurgy and Metallurgical EngineeringITsalbcISBD990002729660203316P13 203DISTRABKDISTRADISTRA21020060405USA011508DISTRA21020060405USA011509Assessment of energy requirements in proven and new copper processes1000803UNISA03801nam 2200853z- 450 991057687400332120220621(CKB)5720000000008435(oapen)https://directory.doabooks.org/handle/20.500.12854/84601(oapen)doab84601(EXLCZ)99572000000000843520202206d2022 |y 0engurmn|---annantxtrdacontentcrdamediacrrdacarrierOceanic Internal Waves and Internal Tides in the East Asian Marginal SeasMDPI - Multidisciplinary Digital Publishing Institute20221 online resource (126 p.)3-0365-4213-2 3-0365-4214-0 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.History of engineering and technologybicsscTechnology: general issuesbicsscBali Seabaroclinic tidesEast China Seaextreme current velocityflow noiseHainan Islandhybrid coordinate ocean model reanalysis resultsinternal solitary waveinternal solitary wavesinternal wavesJapan SeaKRI nanggala-402 submarine wreckLombok StraitLuzon Straitmesoscale flow fieldMITgcmmoored observationn/anear-inertial internal wavesnear-inertial wavesnonlinear internal wavenonseasonal variabilityOkubo-Weiss parameterpropagating directionpropagating speedrelative vorticityremote sensing imagesshipboard observationSouth China Seasouthwestern East Seastratification variabilitysubsurface mooringthe South China Seatrapped coretyphoon Megiunderwater noiseunderway observationvortex-induced vibrationwave breakingHistory of engineering and technologyTechnology: general issuesNam SungHyunedt1296670Chen XueenedtNam SungHyunothChen XueenothBOOK9910576874003321Oceanic Internal Waves and Internal Tides in the East Asian Marginal Seas3024202UNINA