This study evaluates a data-assimilated model simulation of near-surface circulation in DeSoto Canyon (DSC), Gulf of Mexico, with emphasis on analyzing moored current-meter observations and comparing them with satellite data and model results. The study period is for two years from April 1997 to April 1999. The model results are from a high-resolution Gulf of Mexico model forced by analyzed win...

Underwater fiber optic cables commonly traverse a variety of seafloor conditions, which leads to an uneven mechanical coupling between the cable and ocean bottom. On rough bathymetry, some portions might be suspended thus susceptible vortex-induced vibrations (VIV) driven by deep currents. Here, we examine potential distributed acoustic sensing (DAS) monitor deep-sea currents along sections und...

Abstract Currents in the Baltic Sea are generally weak, but during strong winds they can grow high enough to affect surface wave propagation and evolution. To evaluate significance of wave-current interactions Sea, we conducted a study using model WAM, comparing run without currents one with current forcing from NEMO hydrodynamical simulation. The overall changes field caused by were quite smal...

The aim of this paper is to simulate the impact a potential offshore LNG terminal on sea temperature (in autumn and spring/ summer) currents autumn/winter) at three different depths (at surface, 25 m depth seabed) in northern Adriatic Sea from 14 November 2015 06 August 2016 using Regional Ocean Modelling System (ROMS) model. location Istria Sea) was selected visual PROMETHEE method. uses seawa...

this paper proposes an extension of markov chain model to characterize of geological formations and to make conditioning on any number of well data possible. in this study, lithofacies cycles of the amiran formation at type and pirshamsedin sections are examined by markov method and entropy analysis as well as field observations, and depositional environment has interpreted by proposed ideal se...

Current observations of ocean currents are mainly based on altimetric measurements Sea Surface Heights (SSH), however the characteristics present-day constellation altimeters only capable to retrieve surface at scales larger than 50–70 km. By contrast, infrared and visible radiometers reach spatial resolutions thirty times higher under cloud-free conditions. During last years, it has been shown...