Bathymetry and Hydrodynamics in Pare Bay Waters During Transitional Seasons (SeptemberOctober)

Ulung Jantama Wisha (Researcher in Research Institute for Coastal Resources and Vulnerability, Ministry of Marine Affairs and Fisheries, JL. Raya Padang-Painan KM. 16, Teluk Bungus Padang 25245 Indonesia)
Aida Heriati (Researcher in Agency for Research and Development of Marine and Coastal Resources, Ministry of Marine Affairs and Fisheries , Komplek Bina Samudera JL. Pasir Putih II Lantai 4, Ancol Timur, Jakarta Utara 14430 Indonesia)

Omni-Akuatika
Vol 12, No 2 (2016): Omni-Akuatika November

Sedimentation on Pare bay and Karajae estuary originated from the run off of Karajae River. Highsedimentation process leads to the adverse effect of abiotic environmental changes. The aim of thisresearch is to analyse bathymetry condition and hydrodynamic characteristics of the area inunderstanding sediment distribution on Pare Bay. Corrected bathymetric data by tide data isprocessed using Surfer software 9.0 versions to analyse Pare Bay contour in 2D and 3D, the resultshow depth ranges from 0 to 20 meters. Flow model module by MIKE 21 software was used inhydrodynamic simulation (MRSE 11.44%) and shows that current condition in Pare Bay wasdominated by tidal (within its speed up to 0.43 ms-1), surface currents speed is higher and morerandom than the speed in water column and near bottom. Due to its location, Pare Bay is directlyinfluenced by Indonesian Through flow which has strong currents flow and cause mixing andturbulence along its way, this condition influences Pare Bay condition, especially in the process ofsedimentation and turbulence.  Keywords: bathymetry, currents, hydrodynamics, sedimentation, pare bay