Quantcast
Last updated on April 19, 2014 at 17:21 EDT
Numerical Simulation of Channel Flows Image 2
2002 of 3476

Numerical Simulation of Channel Flows (Image 2)

July 1, 2010
Numerical Simulation of Channel Flows (Image 2) Tidal currents filling up the Elkhorn Slough, on the coast of Monterey Bay, Calif. (time in seconds from low-low water). The water surface elevation inside Elkhorn Slough is determined by the tide. At low tides, the water surface elevation is low, so the mudflats on both sides of the channel are dry (see top-left pane). When high tide comes, water surface starts to rise, and sea-water flows into the slough, filling up the channel and spilling over onto the mudflats (see top-right to bottom-left panes). At high tide, the water surface elevation is high, and the mudflats are inundated (see bottom-right pane). In reality, the elevation of the mudflat bottom is not constant, and there are bumps and dips. But in this test run, the researchers used a constant elevation for the mudflat to simplify the problem. [Note: This figure was from a test run and a flat floodplain was used; the results are not accurate.] [Image 2 of 4 related images. See Image 3.] More about this Image Researchers Gang Zhao, Peter Ioannidis and Robert Street from the Environmental Fluid Mechanics Laboratory in the Civil and Environmental Engineering Department at Stanford University, used a three-dimensional numerical model--which simply speaking, is a computer program--to study the hydrodynamics of complex channel flows. Understanding how water flows in channels is important for engineering projects, such as flood control, channel bank erosion control, and habitats restoration. The purpose of this study was to develop a numerical model and apply it to simulate complex channel flows. To learn more about the model, visit the SUNTAN (Stanford Unstructured Nonhydrostatic Terrain-following Adaptive Navier-Stokes Simulator) Web site. The research team simulated the tidal currents in Elkhorn Slough, which is about 10 kilometers long and consists of a meandering main channel and a large area of mudflat and marsh. Elkhorn Slough has the second largest tidal salt marsh in California, which provides habitat for many plants and animals. However, the size of the salt marsh at Elkhorn Slough is decreasing due in part to tidal erosion. This simulation provides high-resolution velocity distribution inside the slough, which is a key step in understanding the hydrodynamics of the slough, and is important for future habitat conservation and restoration projects. [This research was supported in part by National Science Foundation (NSF) grant 00-87842. Computations were performed at Stanford University's Center for Computational Earth and Environmental Science. SUNTAN is sponsored in part by NSF grant 0113111.] (Date of Image: 2005)