• 대한원격탐사학회:학술대회논문집
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• 대한원격탐사학회 2005년도 Proceedings of ISRS 2005
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• pp.671-674
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• 2005

Atmospheric correction over the ocean part is more important than that over the land because the signal from the ocean is very small about one tenth of that reflected from land. In this study, the Spectral Shape Matching Method (SSMM) developed by Ahn and Shanmugam (2004) is evaluated using Landsat imagery acquired over the highly turbid Saemangeum Coastal Area. The result of SSMM is compared with COST model developed by Chavez (1991 and 1997). In principle, SSMM is simple and easy to implement on any satellite imagery, relying on both field and image properties. To assess the potential use of these methods, several field campaigns were conducted in the Saemangeum coastal area corresponding with Landsat-7 satellite's overpass on 29 May 2005. In-situ data collected from the coastal waters of Saemangeum using optical instruments (ASD field spectroradiometer) consists of ChI, Ap, SS, aooM, F(d). In order to perform SSMM, we use the in-situ water-leaving radiance spectra from clear oceanic waters to estimate the the path radiance from total signal recorded at the top of the atmosphere (TOA), due to the reason that the shape of clear water-leaving radiance spectra is nearly stable than turbid water-leaving radiance spectra. The retrieved water-leaving radiance after subtraction of path signal from TOA signal in this way is compared with that estimated by COST model. The result shows that SSMM enabled retrieval of water-leaving radiance spectra that are consistent with in-situ data obtained from Saemangeum coastal waters. The COST model yielded significantly high errors in these areas.

• Ocean and Polar Research
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• 제28권3호
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• pp.339-352
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• 2006

Seasonal and tidal variations of density stratification in the Saemangeum waters are investigated based on synoptic CTD observations between July 2003 and September 2005. CTD data used in this study are those obtained after closing the dike No. 4 and before closing the two final gaps, the Sinsi and the Garyeok, on the Saemangeum tidal harrier. A total of 19 field campaigns comprehend a wide temporal spectrum, that is, few seasons, spring and neap tides, and high and low waters. In addition, ADCPs were anchored and CTDs were cast at three stations for 25 h in July 2005. Water columns are vertically homogeneous in autumn and winter. The vertical homogeneity persists in spring but with an occasional weak stratification in i:he northern part of the Gogunsan Islands. Increased reshwater runoff tends to stabilize the water columns and strong density stratification is established in summer. The mean potential energy anomaly (PEA) in summer used as a stratification parameter is the largest $(27.7\;J\;m^{-3})$ in the northern part of the Gogunsan Islands where the Geum River discharge dominates, the smallest $(16.9\;J\;m^{-3})$ is in the inner area of the barrier, in between the two $(21.6\;J\;m^{-3})$ in the southern part of the Gogunsan Islands. Whereas the stratification is generally strengthened in summer, strong winds or large tidal currents over the shallow depths frequently destratify the water column near the mouth of river runoff inside the tidal barrier. Periodic stratification, the development of stratification on the ebb and its breakdown on the flood, occurs in the mid-area inside the barrier induced by the tidal straining, which can also be found in the results of 25 h observation.

• 환경영향평가
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• 제20권2호
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• pp.199-205
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• 2011

The Saemangeum embankment construction have changed the flowing on the topography of the coastal marine environment. However, the variety of ecological factors are changing from outside of Saemangeum embankment area. The ecosystem of various marine organisms have led to changes by sea surface temperature. The aim of this study is to monitoring of sea surface temperature(SST) changes were measured by using thermal infrared satellite imagery, MODIS and Landsat. The MODIS data have the high temporal resolution and Landsat satellite data with high spatial resolution was used for time series monitoring. The extracted informations from sea surface temperature changes were compared with the dyke to allow them inside and outside of Saemangeum embankment. The spatial extent of the spread of sea water were analyzed by SST using MODIS and Landsat thermal channel data. The difference of sea surface temperature between inland and offshore waters of Saemangeum embankment have changed by seasonal flow and residence time of sea water in dyke.

• 한국수산과학회지
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• 제36권3호
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• pp.298-305
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• 2003

Seasonal variation in species composition of fish in the estuary of Saemangeum water in the western coast of Korea was determined using seasonal samples collected by an otter trawl from April 2001 to February 2002. Species compositions did not differ significantly among the 4 stations (p>0.05, Wilcoxon signed-rank test). The cumulative number of species and species diversity (H') approached asymptote after four 30-min trawl hauls. Therefore 30-min trawl samples from each of the four stations were pooled to represent each season. A total of 45 species 2758 individuals and 30,346.8 g of fish were collected during the study period. Of the fish collected Leiognathus nuchalis, Synechogobius hasta, Neosalanx jordani, Konosirus punctatus and Chaeturichthys stigmatias predominated in abundance accounting for $68\%$ of the total number of individuals. Seasonal variation of fish abundance showed a similar trend to those of the other western coastal waters of Korea. The resident species were collected only in spring and autumn. Number of species and biomass were highest in summer due to the catch of many migrating species. In winter catch amount was low, and only 7 species were collected.. Brackish water fishes were more abundant in the study area, and Johnius grypotus and Cynoglossus joyneri were not premominated compared to the other coastal waters. This difference in species compositions may be related to the lower salinity in this estuarine habitat than in the other western coastal waters of Korea.

• 해양환경안전학회지
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• 제29권4호
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• pp.297-306
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• 2023

새만금호는 우리나라 최대의 인공호수로 호수의 수질은 갈수록 악화되어 가고 있어 호수의 특성에 맞는 새로운 수질관리 대책이 필요하다. 이에 새만금호의 국가수질측정망 자료를 이용하여 통계분석 기법에 의한 새만금호의 시공간적 수질특성을 분석하였다. 수질항목간의 상관성에서 수온과 TP는 상관성이 있고, 염분과 TN, 그리고 pH와 COD가 상관성이 높았다. 그 외 항목들 간에는 낮은 상관성을 나타내어 관련성이 낮았다. 주성분 분석을 이용한 새만금호의 공간적 수질특성을 보면, 크게 4개의 그룹으로 구분되었는데, 담수 영향구역과 해수 영향구역, 해수와 담수가 혼합되는 중간 수역이 2개 그룹으로 구분되어 각각 다른 수질특성을 나타내었다. 주성분분석을 이용한 시간적 수질특성은 계절적으로 4가지 그룹으로 구분되었다. 그룹I은 늦봄과 초여름에 해당되는 5, 6월이고, 그룹 II는 계절적으로 초봄(3, 4월)과 늦가을(11, 12월)에 해당되는 시기로 나타났으며, 그룹 III은 낮은 수온에 의한 용존산소의 증가가 나타나는 계절인 겨울철(1, 2월)의 수질 특성을 보였고, 그룹 IV는 하계(7, 8, 9, 10월) 성층의 발달로 저층 퇴적물의 높은 인농도와 하계 고수온의 상관성을 가지는 그룹으로 구분되었다. 이는 새만금호가 인위적으로 조성된 호수로써 상류 만경강과 동진강의 유입 영향을 받는 것과 동시에 새만금 방조제에 설치된 가력과 신시갑문을 통한 외해수 유입의 영향을 받음으로써 수질의 변동요소가 달라진 것으로 평가된다. 새만금호의 목표수질을 달성하기 위해서는 상류 유역의 오염원 관리 대책과 함께 새만금호의 수질관리 대책을 수립할 필요가 있다.

• 한국해양학회지:바다
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• 제13권1호
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• pp.56-66
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• 2008

서해 중부에 위치한 새만금 연안역에서 HF radar를 이용하여 2002년 7월과 2004년 9월부터 11월 초까지 표층해류를 관측하였다. 관측 자료로부터 조하주기대(subtidal) 표층해류가 해안선 변화, 바람과 담수 방류량의 변화에 대하여 시 공간적으로 어떻게 변동하는지 조사하였다. 2002년 7월 관측 기간 동안 바람이 약 0.5 m/s로 불었으며, 일 평균 금강 담수 방류량이 $0.88{\times}10^7$ 톤이었다. 시간평균된 표층해류($\overline{U}$)는 금강하구입구에서 $7{\sim}10\;cm/s$의 크기로 북서쪽으로, 방조제 개방구간에서 13 cm/s 이상의 크기를 갖고 서쪽으로, 고군산군도 북측에서는 북서방향의 분포를 보였다. 이는 금강 담수와 새만금 방조제 개방구간에서 유출된 조석 잔차류에 의해 형성된 흐름이다. 또한 를 제거한 표층해류의 공간평균치(<$U-\overline{U}$>)의 방향변화가 바람방향변화와 상대적으로 높은 상관관계(r=0.98)를 보였다. 2004년 9월부터 11월에는 북북서풍이 2.5 m/s로 불었으며, 일평균 담수 방류량이 $11.9{\times}10^7$ 톤이었다. 표층해류($\overline{U}$)는 대부분의 연안에서 크기가 작았고, 새만금 방조제와 고군산군도가 이루는 해안선을 따라서 약 10 cm/s의 상대적으로 빠른 해류가 남서방향으로 흘렀다. 이는 강한 북서풍이 금강 담수를 새만금 방조제 쪽으로 이동시켜 형성된 흐름이다. 2004년도에는 방조제 개방구간에서 유출되는 조석 잔차류가 없어졌으며, 공간평균()된 표층해류의 방향변화가 바람방향변화와 0.69의 상관관계를 보였다.