Hydrodynamical model during east season at Gosong Coastal West Borneo as candidate location of nuclear power plant in Indonesia

Indonesia planned to build the first nuclear power plant in Gosong Coast, Bengkayang Regency, West Kalimantan. This research examined the hydrodynamical conditions in the ocean of Gosong Coast during the eastern season. This hydrodynamic model can be considered in estimating the distribution of various radionuclide wastes that release to the ocean. It was simulated using the Delft3D flow module application for 15 days which included the neap and spring tide conditions. Base on the result of the hydrodynamical model, Gosong Coast had a mixed semidiurnal type of tide with low amplitude. The wind parameters involved higher impacts to the hydrodynamical conditions. The model result did not find significant differences between neap and spring tide periods. There was a flow collision between 2 opposite water currents which was occurred at Burung Archipelagic during flood tide and at the Coastal area of Singkawang City during ebb tide. Therefore, the ocean currents at Gosong Coast flowed directly offshore through Burung Archipelagic during ebb tide. Meanwhile during flood tide, these ocean currents moved to Singkawang and Sambas Coastal area before they deflected toward offshore.

Hydrodynamical Model for Charge Transport in Graphene Nanoribbons

We present a hydrodynamical model for graphene nanoribbons that takes into account the electron collisions with the lattice and with the edge of the ribbon. Moreover the bandgap due to the low dimension of the ribbon is considered. The simulation shows that the model describes qualitatively the macroscopic behavior of the charges and the results are comparable with that ones obtained by solving numerically the Boltzmann equation but with a remarkable reduction of the computational time.

Wave-currents interaction in the Black Sea: new modelling approach for next generation of operational forecasting system.

<p>This study analyzes wave-currents interactions in the Black Sea basin focusing on deep water processes by using a coupled two-ways off-line numerical system, based on the ocean circulation model NEMO v4.0 and the third-generation wave model WaveWatchIII v5.16. The coupling between wave and hydrodynamical models is carried out at hourly frequency. The physical processes taken in consideration are: Stokes-Coriolis force, sea-state dependent momentum flux, wave induced vertical mixing, Doppler shift, and the stability parameter for the computation of effective wind speed. </p><p>The hydrodynamical model is implemented over the Black Sea at the horizontal resolution of about 3km and 31 vertical levels, with closed boundary at the Bosporus Strait. The impact of the Bosporus Strait on the Black Sea dynamics is modeled using a surface boundary condition, taking into account the barotropic transport, which balances the freshwater fluxes on monthly basis (Stanev and Beckers, 1999; Peneva et al., 2001; Ciliberti et al., 2021). Additionally, Mediterranean waters inflow is represented by applying a local damping to high resolution temperature and salinity profiles (Aydogdu et al., 2018) at the Bosporus exit.</p><p>The wave model adopts the WW3 implementation of the WAM Cycle4 model physics, with Ultimate Quickest propagation scheme and GSE alleviation, over the same spatial grid as the hydrodynamical model Wind input and dissipation are based on Ardhuin et al. (2010), wave-wave interactions are based on Discrete Interaction Approximation. The wave spectrum is discretized using 24 directional sectors, and 30 frequencies, with 10% increment starting from 0.055Hz. Validation and statistical analysis of the results have been carried out to compare coupled and uncoupled runs, aiming to identify the model set-up to upgrade in the future the near real time operational system.</p><p>The evaluation of the coupling impact on significant wave height and temperature shows BIAS reduction, and even slight improvement of RMSE.</p>

Is the gap in the DS Tau disc hiding a planet?

ABSTRACT Recent millimetre-wavelength surveys performed with the Atacama Large Millimeter Array (ALMA) have revealed protoplanetary discs characterized by rings and gaps. A possible explanation for the origin of such rings is the tidal interaction with an unseen planetary companion. The protoplanetary disc around DS Tau shows a wide gap in the ALMA observation at 1.3 mm. We construct a hydrodynamical model for the dust continuum observed by ALMA assuming the observed gap is carved by a planet between one and five Jupiter masses. We fit the shape of the radial intensity profile along the disc major axis varying the planet mass, the dust disc mass, and the evolution time of the system. The best-fitting model is obtained for a planet with $M_{\rm p}=3.5\, \mathrm{ M}_{\rm Jup}$ and a disc with $M_{\rm dust}= 9.6\,\times \,10^{-5}\, \mathrm{ M}_{\odot }$. Starting from this result, we also compute the expected signature of the planet in the gas kinematics, as traced by CO emission. We find that such a signature (in the form of a ‘kink’ in the channel maps) could be observed by ALMA with a velocity resolution between $0.2-0.5\, \rm {kms}^{-1}$ and a beam size between 30 and 50 mas.

The significance of wave–current interaction on modelled wave fields in the Baltic Sea

<p>Currents in the Baltic Sea are relatively weak and are thus often expected to have a negligible effect on sea surface waves. To evaluate the magnitude of wave–current interactions in the Baltic Sea, we ran the third generation wave model WAM with and without surface currents from the 3D hydrodynamical model Nemo4. The results showed that the currents have a notable effect on wave field only on rare occasions and that the effects are largest in coastal areas of the Baltic Proper, most notably in the western Gotland Basin, and the Gulf of Finland. The simulations showed that the currents in the Baltic Sea can cause differences of significant wave height up to tens of centimeters. More notable effect was the change in the peak of the wave spectrum from swell to wind driven waves and vice versa in some occasions. In our study w<span>e mostly focus on the events of strong wave–current interactions in the northern Baltic Proper and Gulf of Finland as we have measured wave spectra available from these locations. From the comparison with wave buoy measurements we see that implementing surface currents</span> <span>slightly improves the </span><span>m</span><span>odelled peak period in the Gulf of Finland.</span> <span>The Gulf of Finland is of special interest also because a group of ADCP’s were installed close to the wave buoy. The current measurements from these devices can therefore be used to evaluate the accuracy of the currents in the hydrodynamical model. </span></p>

Testing a Best-Fit Hydrodynamical Model Using PCA

Recently, a comprehensive Bayesian analysis was performed to simultaneously extract the values of a number of hydrodynamic parameters necessary for compatibility with a limited set of experimental data from the LHC. In this work, this best-fit model is tested against newly measured experimental flow results not included in the original work, namely the principal components of the two-particle correlation matrix in transverse momentum. The results from simulations show a good numerical agreement with data obtained by the CMS Collaboration.