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신문섭(Moon Seup Shin),홍성근(Sung Kun Hong),장인규(In Kyoo Chang),임병용(Byeong Yong Lim) 군산대학교 수산과학연구소 1998 水産科學硏究 Vol.- No.14
The purpose of this study is to find sedimentation patterns variation in the Geum river estuary. Water circulations are calculated diagnostically from the observed water temperature and salinity data and wind data and tidal residual current. Three dimensional movements of injected particles due to currents, turbulence and sinking velocity are tracked by the Euler-lagrange methoed.
김영섭(Kim Young-seup),홍성근(Hong Sung-kun) 군산대학교 수산과학연구소 1985 水産科學硏究 Vol.- No.1
In order to provide the basic data required for setting up the proper strategies to minimize future marine environmental pollution on Kwangyang bay, the general water quality parameters, circulation pattern and dye study were investigated on January 19, 1984. Although TSS is somewhat high level, most suspended solid seem to composed of the inorganic materials. NH₃-N is also low level compared with that of other coastal areas so that the pollution by the nutrients is not serious yet. While COD is very high level in comparison with the results of other areas. The diffusive capability of this bay is assessed to be medium level.
신문섭(Moon Seup Shin),홍성근(Sung Kun Hong),장인규(In Kyoo Chang),박병룡(Byeong Yong Lim) 군산대학교 수산과학연구소 2004 군산대학교 수산과학연구소 연구논문집 Vol.4 No.-
The purpose of this study is to find sedimentation patterns variation in the Geum river estuary. Water circulations are calculated diagnostically from the observed water temperature and salinity data and wind data and tidal residual current. Three dimensional movements of injected particles due to currents, turbulence and sinking velocity are tracked by the Euler-lagrange methoed.
신문섭(Moon-Seup Shin),홍성근(Sung-Kun Hong) 군산대학교 수산과학연구소 2004 군산대학교 수산과학연구소 연구논문집 Vol.3 No.-
A measurements and numerical analysis of tidal current were carried out at around Siwha seawell in Ansan and Taebudo of Kyung Gi Do,to investigate the tidal current change attend on seawell constrection.The velocity and direction of tidal current are in accord with the numerical analysis. tidal current of most region are fast as 2.0m/sec over.Tidal current were on the increase as increase water level difference in outside and inside.
한영호(Young-Ho HAN),홍성근(Sung-Kun HONG),김영섭(Young-Seup KIM) 군산대학교 수산과학연구소 1994 군산대학교 수산과학연구소 연구논문집 Vol.1 No.-
The water quality and the budget of pollutant loading in the downstream of Nakdong River were surveyed at 3 sites along the main stream from Mulgum to Hadan and 1 site of Yangsan tributary with response to the tides in May and June, 1983. The level of TSS in the Yangsan tributary, 6.1~21.3mg/l, was higher than any other site. The mean vaIues of BOD were 1.16mg/l at Mulgum site. I.83mg/l Yangsan site, O.79mg/l Hwamyeong site and 3.56mg/l at Hadan site. The levels of NH₄+-N and PO₄3- -P were the highest at Hadan site, and the levels of zinc and copper were 2.11~5.98ppb and ND-50.00ppb at Yangsan tributary site. Although the flow rate of Yangsan stream accounted for only 4% of that of main stream, but the mean value of pollutant loading in the Yangsan stream amounted to 8.3% of the that of main steam.
신문섭(Moon-Seup Shin),홍성근(Sung-Kun Hong) 군산대학교 수산과학연구소 1994 水産科學硏究 Vol.- No.10
A measurements and numerical analysis of tidal current were carried out at around Siwha seawell in Ansan and Taebudo of Kyung Gi Do, to investigate the tidal current change attend on seawell constrection. The velocity and direction of tidal current are in accord with the numerical analysis. tidal current of most region are fast as 2.0m/see over. Tidal current were on the increase as increase water level difference in outside and inside.
김영섭,한영호,신수경,홍성근,KIM Young-Seup,HAN Young-Ho,SHIN Soo-Kyeong,HONG Sung-Kun 한국수산과학회 1994 한국수산과학회지 Vol.27 No.3
Characteristics of climate in the eastern coastal regions of Korean Peninsula were studied using the meteorological and coastal sea surface temperature (SST) data which were compiled from 1961 to 1990. In the winter half year (from October to March), air temperature (AT) and precipitation of the eastern coastal regions were considerably higher than those of the western and inland regions, but relative humidity was $8{\sim}15\%$ lower. AT of coastal regions was closely related to the variation of coastal SST. These characteristics were more noticeable in the eastern coastal areas and in lower latitude regions. Quantitatively, the $1.0^{\circ}C$ variation of coastal SST may have resulted in the $1.0^{\circ}C{\sim}1.5^{\circ}C$ variation for AT in coastal regions. In the same way as temperature, vapor pressure in coastal regions was also influenced by coastal SST. Relative humidity change corresponding to the $1.0^{\circ}C$ variation of coastal SST was $3.7\%{\sim}6.5\%$. Net heat exchange amounts were positive (sea surface gaining energy) in all coastal regions. Sea surface gained net heat from March to September, and lost it from October to February. Variation of AT in coastal regions was also related to the sensible and latent heat exchanges. Sensible and latent heat amount corresponding to the $1.0^{\circ}C$ variation of AT were $10Wm^{-2}$ at Kangnung, and $8Wm^{-2}$ at Pohang and $13Wm^{-2}$ at Pusan.