선택한 단어 수는 입니다.
최소 단어 이상 선택하여야 합니다.
최소 단어 이상 선택하여야 합니다.
선택한 단어 수는 30입니다.
최대 10 단어까지만 선택 가능합니다.
최대 10 단어까지만 선택 가능합니다.
제안 방법
- In this study, the influences of surface wind waves are not considered which not only effect the typhoon circulation through the surface roughness and heat flux but also have effects on the surface currents in terms of wave breaking (whitecapping in deep water and depth-induced wave breaking in shallow water) and turbulence production in surface boundary layer.
- The objectives of this study is to investigate the dynamic ocean response to typhoon as well as that of typhoon in terms of ocean mixed layer, mixed-layer currents and temperature profiles in the wake of typhoon in addition to SST changes by means of a three-dimensional non-hydrostatic atmosphere and ocean coupled model.
- In the coupling simulation, MITgcm obtained the surface heat flux, momentum flux by wind and sea surface pressure from MM5 integration while MM5 got the variable SST values from MITgcm integration for multiple c쟎mmoii time steps. The simulations were performed for 90 h from 0000 UTC 5 August to 1800 UTC 8 August in 2003 until the typhoon made landfall.
- This model is based on non-hydrostatic, compressible form of governing equations in spherical and sigma coordinates with physical processes such as precipitation physics, Planetary Boundary Layer (PBL) processes and atmospheric radiation processes incorporated by a number of physics parameterizations. Further details of MM5 are referred to Grell et al.
이론/모형
- In this study, the local air-sea interaction under Typhoon ETAU was investigated using the non-hydrostatic atmosphere-ocean coupled model. The local ocean response shows general accordance with satellite observations in SST.
- Most recently, a project on the impacts of reduced discharge of freshwater and sediment from Yangtze River basin on the adjacent East Asian Seas has been initiated using the RES as a significant tool for the environment assessment and multidisciplinary environmental science. In this study, the local air-sea interaction under typhoon with regards to typhoon and ocean responses to each other has been investigated using the non-hydrostatic atmosphere-ocean coupled model which is the core circulation part of the RES.
- The atmospheric circulation in a coupled simulation model and in RES is described by mesoscale model, MM5, developed at Pennsylvania State University (PSU)-Natinal Center for Atmospheric Research (NCAR). This model is based on non-hydrostatic, compressible form of governing equations in spherical and sigma coordinates with physical processes such as precipitation physics, Planetary Boundary Layer (PBL) processes and atmospheric radiation processes incorporated by a number of physics parameterizations.
- 1997a, b), developed from Massachusetts Institute of Technology. This model is a non-hydrostatic three-dimensional model based on the incompressible Navier-Stokes equations with Boussinesq approximation formulated in finite volume method.
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