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CIRCULATION and TRANSPORT MODELS in the coastal area of AGIA PELAGIA - MILATOS Evangelos Pafilis
2D Wind Coastal Circulation Model 2D Advective Pollutant Transport Model This report describes the practice that took place in July 99 at I.M.B.C. The main objective was to study and to predict the behavior of the coastal area near Heraklion, from Agia Pelagia to Milatos. This was achieved with the development of two computer programs. At first these computer programs calculate the sea circulation, based on the bathymetry of the area and the wind stress, and after they compute the transport of a certain pollutant in the same region. The final results were saved on files easily accessed and animated providing infos in a simple and understandable manner. Numerical Models are predictive scientific tools that use data taken right away from the observation field. In order to make the prediction a great number of parameters is taken under consideration. These parameters are expressed through, usually complex, mathematical equations. Nowadays by the use of computers a greater size of calculations is possible, providing this way even more accurate results and setting aside the traditional methods such as laboratory models. 2D Wind Coastal Circulation Model Coastal Domain is defined as the area that extends from the coastline to the continental slope. So it comprises of marine regions where human interference is extensive. Coastal circulation is defined as the development of generally non-steady velocity and surface elevation fields in a coastal zone. This means that for each point of the area being studied, a vector for the velocity and a number for the elevation of the surface are computed. This number can either be positive or negative depending on whether the surface rises or lowers. 2D Advective Pollutant Transport Model As input it uses the data obtained from the circulation model and processes them through mathematical equations that describe the phenomena of advection and diffusion of pollutants. The output is the concentration of the pollutant at each point after a certain period of time. The two models in total provide what is so called Coastal Zone Management (CZM), providing valuable data for scientists, engineers and decision-makers. They have been used in the past by IMBC MDNS (Institute of Marine Biology Crete Marine Dynamics and Numerical Simulations) in a great number of projects with the most recent:
The project took place in July 99 at IMBC MDNS. The hardware used was an SGI O2 system linked to an ORIGIN 200 server. As programming language FORTRAN 77 was chosen and GrADS was the animation package. The bathymetry data were retrieved from maps provided by the Geographical Service of Defense. The domain of Agia Pelagia Milatos was divided in squares with grid dx = 463 m, each one with its own depth. Creating the code was the next step. The Circulation model accepts as inputs:
The process of data occurs according to the following mathematical equation: where: h: depth, z : surface elevation, U: horizontal component of velocity, V: vertical component of velocity, : horizontal surface friction ( stands for density), : vertical surface friction, : horizontal bottom friction, : vertical bottom friction, : Coriolis coefficient, dt: time step (set to 2,2 sec for stability reasons). The equation is solved using the finite differences in stagger grid method. The output is the horizontal and vertical velocity components as well as the surface elevation.
The transport model as input accepts U, V and z calculated in the circulation model. The user can define the following parameters:
The process of data occurs according to the following mathematical equation: Where: C: the pollutants unknown concentration, Du: vertical eddy diffusion coefficient, Dh horizontal eddy diffusion coefficient and l : decay coefficient. The output is the concentration of the pollutant at each point after a certain period of time. These results are read through animation programs and become visible and easily understandable. The animations accomplish the following conditions: Wind Direction : NW Wind Velocity : 8 beaufort Origin : 25.187E, 35.350N Effects Duration : 96 hrs The wind direction is not by chance NW. As climatogical researches have shown NW wind in the area of Heraklion is the most common eight months per year (PENNAS 1977). The first animation is the resemblance of a conservative pollutant, such as an oil spill, where bacteria and the others micro-organisms do not interfere with the pollutant. The second animation follows the scenary of a non-conservative pollutant, e.g. the outflow of a sewage pipeline, where bacteria and the others micro-organisms do interfere with the pollutant. A demo guide and a demo animation can be found in the Internet in the following site: http://kos.ics.forth.gr on the banners à Thetis presentation à Waste Disposal. (The animation at this moment is under construction).
The practice and the presentation wouldnt have been accomplished unless:
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