Gunsan coastal area is one of region increasing pollution problems. To improve water quality, the reduction of these nutrients loads should be indispensible. In this study, the three-dimensional numerical hydrodynamic and ecosystem model were applied to analyze the processes affecting the eutrophication. In field survey, the average concentrations of dissolved inorganic nitrogen (DIN) and dissolved inorganic phosphorus(DIP) at surface waters were found to be 0.43㎎/ℓ and 0.03㎎/ℓ respectively, which were exceeding second grade of water quality criteria. In hydrodynamic modelling, the comparison between the simulated and observed tidal ellipses showed fairly good agreement. The ecosystem model was calibrated with the observed data in study area. The simulated results of DIN were fairly good coincided with the observed values within relative error of 32.39%, correlation coefficient(r) of 0.99. In the case of DIP, the simulated results were fairly good coincided with the observed values within relative error of 24.26%, correlation coefficient(r) of 0.82. The simulations of DIN and DIP concentrations using ecosystem model were performed under the conditions of 20～80% reductions for pollutant loading. At simulation results, concentration of DIN and DIP were reduced to 20～80% and under 10% in case of the 80% reduction of polltuant loading, respectively.

Diurnal variations of air quality due to the characteristic features of local weather phenomena over Kunsan, Taegu, and Pohang are analyzed using various synoptic wind fields and the characteristics of local weather during the period of 1990 to 1992. The air pollutants analyzed are sulfur dioxide(SO_2), nitrogen dioxide(NO_2), and oxidants (O_3). The synoptic wind fields estimated at over the 850 hPa geopotential height are divided in terms of four wind directions and two wind speed categories for each season. The synoptic weather conditions are also classified into two categories depending on the total cloud amounts. The present study shows that the SO_2 concentration over Kunsan, and Taegu was maximum at the two or three hours after sunrise and second primary was three or four hours after sunset. On the other hand, its concentration over Kunsan was maximum at 1900 LST or 2000 LST. The O_3 concentration over the three cities shows its maximum in the afternoon when the solar radiation is strong. The NO_2 concentration over Kunsan shows in reverse proportion to the 0_3 concentration over the Kunsan.