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3-D water current, vertically averaged 2-D water current, 3-D salinity and DIN, 2-D water level collected from Numerical model (i.e., FVCOM) simulated current, salinity, and DIN time series in Barataria Bay and adjacent Louisiana-Texas continental shelf from 20210101 to 20210825 (NCEI Accession 0301508)

Published by NOAA National Centers for Environmental Information | National Oceanic and Atmospheric Administration, Department of Commerce | Metadata Last Checked: January 26, 2026 | Last Modified: 2025-02-06T00:00:00.000+00:00
The Finite Volume Coastal Ocean Model (FVCOM) was applied over the northern Gulf of Mexico continental shelf that includes Barataria Basin and the Gulf Intracoastal Waterway (GIWW) to simulate three-dimensional circulation and dissolved inorganic nitrogen (DIN) dispersive patterns driven by larger rivers and river diversion, tides, and winds. The numerical model mesh covers a much larger computational domain which extends longitudinally from Mobile Bay, Alabama to west of Galveston Bay, Texas and offshore to ~ 300 m - 1000 m isobaths over the Alabama-Mississippi-Louisiana-Texas continental shelf and slope. Simulated hydrodynamic variables include sea level elevation, u- and v-velocity component, salinity, and turbulence parameters. DIN is simulated as a passive tracer (i.e., without considering the relevant biogeochemical processes) with three major input sources: the Mississippi River through the various passes in the birdfoot delta, the Davis Pond Freshwater Diversion inside Barataria Basin, and GIWW at Larose inlet. The FVCOM simulation period is from 1 January 2021 to 25 August 2021. Output file is in NetCDF (Network Common Data Form) format, which is a set of software libraries and self-describing, machine-independent data formats that support the creation, access, and sharing of array-oriented scientific data. Output time interval is daily (at 00:00 GMT everyday). DIN variable is saved in the NetCDF files as variable temperature since we modified FVCOM source code and used the temperature subroutines for advection and diffusion process to calculate DIN advection and diffusion process.

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0301508 BATHYMETRY CURRENT SPEED - EAST/WEST COMPONENT (U) CURRENT SPEED - NORTH/SOUTH COMPONENT (V) CURRENT SPEED - UP/DOWN COMPONENT (W) LATITUDE LONGITUDE SALINITY SEA SURFACE TOPOGRAPHY turbulence WATER DENSITY water depth WATER TEMPERATURE model output Louisiana State University Louisiana State University Coastal Waters of Gulf of Mexico Coastal Waters of Louisiana Coastal Waters of Texas Gulf of Mexico oceanography QUANTIFYING MARSH EDGE ERODIBILITY AS A FUNCTION OF SALINITY AND WATER CHEMISTRY, AND ASSESSING POSSIBLE EFFECTS OF THE GULF INTRACOASTAL WATERWAY IN BARATARIA BAY EARTH SCIENCE > OCEANS > BATHYMETRY/SEAFLOOR TOPOGRAPHY > BATHYMETRY EARTH SCIENCE > OCEANS > BATHYMETRY/SEAFLOOR TOPOGRAPHY > WATER DEPTH EARTH SCIENCE > OCEANS > OCEAN CIRCULATION > OCEAN CURRENTS EARTH SCIENCE > OCEANS > OCEAN CIRCULATION > TURBULENCE EARTH SCIENCE > OCEANS > OCEAN TEMPERATURE > WATER TEMPERATURE EARTH SCIENCE > OCEANS > SALINITY/DENSITY > DENSITY EARTH SCIENCE > OCEANS > SALINITY/DENSITY > SALINITY EARTH SCIENCE > OCEANS > SEA SURFACE TOPOGRAPHY 3-D water current, vertically averaged 2-D water current, 3-D salinity and DIN, 2-D water level Dissolved inorganic nitrogen (DIN) Eastward Water Velocity Initial Density Northward Water Velocity Shifted Sigma Layers Sigma Layers Sigma Levels Vertically Averaged x-velocity Vertically Averaged y-velocity Water Surface Elevation Wet Cells Wet nodes a1u a2u aw0 awx awy internal mode iteration number nodal x-coordinate nodal y-coordinate nodes surrounding element number of processors partition zonal x-coordinate zonal y-coordinate calculated from Finite-volume Coastal Ocean Model (FVCOM) Numerical model (i.e., FVCOM) simulated current, salinity, and DIN time series OCEAN > ATLANTIC OCEAN > NORTH ATLANTIC OCEAN > GULF OF AMERICA OCEAN > ATLANTIC OCEAN > NORTH ATLANTIC OCEAN > GULF OF MEXICO Barataria Bay and adjacent Louisiana-Texas continental shelf 1HULA2

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