• Title/Summary/Keyword: water level estimation

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Flood Inflow Estimation at Large Multipurpose Dam using Distributed Model with Measured Flow Boundary Condition at Direct Upstream Channels (직상류 계측유량경계조건과 분포형모델을 이용한 대규모 다목적댐 홍수유입량 산정)

  • Hong, Sug-Hyeon;Kang, Boosik
    • KSCE Journal of Civil and Environmental Engineering Research
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    • v.35 no.5
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    • pp.1039-1049
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    • 2015
  • The inflow estimation at large multipurpose dam reservoir is carried out by considering the water balance among the discharge, the storage change during unit time interval obtained from the observed water level near dam structure and area-volume curve. This method can be ideal for level pool reservoir but include potential errors when the inflow is influenced by the water level slope due to backwater effects from upstream flood inflows and strong wind induced by typhoon. In addition, the other uncertainties arisen from the storage reduction due to sedimentation after the dam construction and water level noise due to mechanical vibration transmitted from the electric power generator. These uncertainties impedes the accurate hydraulic inflow measurement requiring exquisite hydrometric data arrangement for reservoir waterbody. In this study, the distributed hydrologic model using UBC-3P boundary setting was applied and its feasibility was evaluated. Finally, the modeling performance has been verified since the calculated determination coefficient has been in between 0.96 to 0.99 after comparing with observed peak inflow and total inflow at Namgang dam reservoir.

Study on Estimation and Application of the Fwl-D-F curves for Urban Basins (도시유역의 Fwl-D-F 곡선 산정 및 활용에 관한 연구)

  • Choi, Hyun-Il;Kim, Eung-Seok
    • Journal of the Korea Academia-Industrial cooperation Society
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    • v.11 no.7
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    • pp.2687-2692
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    • 2010
  • There have been performed many researched for flood magnitude analysis, for example, the Flood-Duration-Frequency relations in the west. Because flood water stage data are more available rather than flood amount data at flood gauge stations of Korea, this study developed Flood water level-Duration-Frequency (Fwl-D-F) curves using rainfall Intensity-Duration-Frequency(I-D-F) curves for the quantitative flood risk assessment in urban watersheds. Fwl-D-F curve is made from water level data for 18 years at Joongrayng bridge station of Joongrayng River basin in Han River drainage area. Fwl-D-F curve can estimate the occurrence frequency for a certain flood elevation, which can be used for urban flood forecasting. It is expected that the flood elevation can be estimated from the forecasted rainfall data using both Fwl-D-F and I-D-F curves.

TWSC Estimation using GRACE Satellite Gravity Data (GRACE 인공위성 중력 자료를 이용한 수자원변화량(TWSC) 산정)

  • Kim, Joon-Soo;Lee, Sang-Il
    • Proceedings of the Korea Water Resources Association Conference
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    • 2011.05a
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    • pp.377-381
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    • 2011
  • 지구는 지속적으로 변화하는 동력학적 시스템이며, 지표면 형상 및 지구 내부의 질량분포도 계속 변화하고 있다. 지구시스템의 질량재분배 과정에서 발생되는 밀도 차이는 중력장의 미세한 변이를 초래한다. 미 항공우주센터(NASA)와 독일 국립 항공우주연구센터(DLR)에서 공동으로 개발한 GRACE (Gravity Recovery And Climate Experiment) 인공위성은 지구의 중력장을 측정하는 위성으로, 2002년부터 현재까지 9년 동안 활동해왔다. 본 연구에서는 한반도(북위 $37.5^{\circ}\sim41.5^{\circ}$, 동경 $125.5^{\circ}\sim130.5^{\circ}$)의 월평균 수자원변화량(TWSC: Terrestrial Water Storage Change)을 산정하기 위해 미국 텍사스대학교 공간연구센터(CSR)에서 가우시안 필터링을 통해 구면조화함수의 계수 형태로 제공된 총 94개월(2002 년 8월~2010년 6월)의 자료(Level-2)를 이용하였다. Level-2 자료는 해양조석, 고체지구조석 및 지구자전으로 인한 극조석 등 조석의 영향과 대기와 해양의 변동성으로 인한 비조석 영향을 보정한 것이다. 이렇게 산정한 TWSC를 수자원관리정보시스템(WAMIS)과 전지구지표동계화시스템(GLDAS)을 통해 제공되는 자료와 비교 분석하였다. 본 연구를 통해 GRACE 중력장 자료가 수자원총량의 산정과 검증을 위한 대안으로 활용될 수 있음과, 수문요소의 불확실성을 낮출 수 있는 새로운 수문자료로의 활용 가능성을 확인하였다.

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Estimation of the Groundwater Movement Under the Heavyrainfall at Nanji Waste Landfill (집중호우시 발생하는 난지도 매립지내의 지하수 거동)

  • 구태훈;조원철
    • Journal of Soil and Groundwater Environment
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    • v.6 no.3
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    • pp.107-117
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    • 2001
  • The characteristics of groundwater movement under the heavy rainfall at Nan-ji waste landfill site are studied using HELP(Hydraulic Evaluation of Landfill Performance) program, which calculates the daily leachate in the Nan-ji waste landfill site. In this study, instead of the average recharge value, which is used in the past study, the real reacharge value is used to calculate the daily leachater. It is found about 70 times greater than thor average recharge value under the condition of heavy rainfall in the rainy season. The flow characteristics of groundwater for water level fluctuation is simulated using the ground water flow model MODFLOW(A Modular 3-D Finite Different Groundwater Flow Model) program, and the slurry layer is newly added. The result of the study is different from that of the ordinary simulation, which shows much higher ground water level than from the ordinary simulation.

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A Stduy on the Microflora of the Han River -Taxonomy of Phytoplankton for the South Han River and Estimation of Water Pollution Levels on the Central Area of the Han River- (한강의 Microflora에 관한 연구 (제6보) -남한강의 식물성플랑크톤에 대한 분류와 한강중심수역의 수질오탁판정-)

  • 정영호
    • Journal of Plant Biology
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    • v.15 no.s
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    • pp.1-32
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    • 1972
  • In order to utilize for the prevention and preservation of the Han River from the environmental pollution the present studies were carried out to clarify the microflora and estimation of the water pollution levels of the Han River. In addition to the above regional and seasonal fluctuation of the phytoplankton was also examined. Samples of phytoplankton were collected from 6 stations in the South Han River during the period from December, 1971 to October, 1972. The results obtained during the present studies are as follows: 1. The phytoplankton samples collected from 6 stations, Yeoju, Hajapo-ri, Yangpyeong, Daruraegi, Giduwon and Paldang were identified and classified by Engler's classification system(1954). It resulted in 2 phylum, 2 classes, 7 orders, 10 families, 29 genera, 137 species, 1 sub-species, 49 varieties, 6 forma and 2 variety-forma. The total numbers of phytoplankton identified were 195 species, of which 7 families, 27 species, 26 varieties, 4 forma and 2 variety-forma are new to Korea, that of 54 species are first described in Korea. 2. In lower area of the Han River it is found 53 species from Paldang and in middle area it is found 114 species from Giduwon, 95 species from Daruraegi, 66 species from Yangpyeong, 71 species from Hajapori and 81 species from Yeoju. In standpoint of seasonal fluctuation of phytoplankton, the total numbers of the plankton is more abundant in summer than in winter season and it shows bimodal pattern. 3. As compared with previous data which obtained from 30 stations covering estuary to upper area, both South and North Han River, during the period from 1965-1972 it is shown that 10 species of the South Han River and 11 species of the North Han River are found throughout all seasons. Among the above species two are common in both area. In the other hand it is found that 9 species in spring season and 6 species in fall season in the South Han River and 10 species in spring, 23 species in summer, 4 species in fall and 15 species in winter season in the North Han River shows their seasonal fluctuation in this area. Among the seasonal occurrence of phytoplankton 10 species were consider to be indicator for the estimation of biological water pollution levels. 4. According to Fjerdingstad's water pollution level system (1963) the total numbers of 1, 230 species which have been collected from the Han River since 1965 includes 27 species of phytoplankton as indicator; 3 species of blue-green algae, 20 species of diatom, and 4 species of green-algae. 5. With 27 indicator species new estimation of water pollution level system was arranged for water pollution in the Han River. 6. The lower part of the central area of the Han River indicates mesosaprobic. In central area of the Han River shows mesosaprobic and oligosaprobic, but predominant in mesosaporobic. And it is indicated that mesosaprobic, oligosaprobic, and polysaprobic factors mixed up in the North Han River. Compare with their water pollution level in the South and North Han River, with author's new system, it is estimated that North Han River is more polluted than South Han River. 7. The reason why North Han River is more polluted suggested that the selfpurification action was limited by their circulation speed. The rapid speed of water in the North Han River is mainly caused by their topography and water-drainage from waterpower plant. In conclusion the central area of the Han River consist of mesosaprobe zone, as a part with oligosaprobe zone. But the presence of polysaprobe zone in the North Han River gives us many problems in future for the nationa development programme and natural conservation in this area.

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Nutrient Loads Estimation at Paddy Field Using CREAM-PADDY Model (CREAMS-PADDY 모형을 이용한 논에서의 영양물질 부하 추정)

  • Chin, Young-Min;Park, Seung-Woo;Kim, Sang-Min;Kang, Moon-Sung;Kang, Min-Goo
    • Journal of Korean Society of Rural Planning
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    • v.8 no.1 s.15
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    • pp.60-68
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    • 2002
  • A Modified CREAMS model, CREAMS-PADDY was developed to simulate the hydrology and nutrient transport at an irrigated rice paddy. The hydrology at a paddy was simulated by a daily water balance routine which reflects daily inflow, outflow, and water level changes. The soil erosion was simulated using modified USLE. The nutrient transport for total nitrogen and phosphorus were depicted for various phases of each constitute such as extraction, percolation, mineralization, and plant uptakes. Field monitoring was conducted to investigate the water quality changes at a paddy field at three times a week during the growing season of 1996. The proposed model simulates the water quality of the paddy reasonably well, and is found to be applicable to field conditions.

Estimation of water level over Hwanggang Dam using satellite image (위성영상을 활용한 북한 황강댐 수위 추정)

  • Choi, Sunghwa;Lee, Jaehee
    • Proceedings of the Korea Water Resources Association Conference
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    • 2018.05a
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    • pp.385-388
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    • 2018
  • 군남댐의 운영은 북한지역에 위치한 저수지와 하천 상황, 특히 황강댐 방류에 절대적으로 의존하는 특성이 있음에도 불구하고, 수위 상황 등 자료수집의 한계로 군남댐 운영에 어려움이 많다. 이러한 상황에서 위성원격탐사 영상자료는 미계측 북한 접경지역의 수문상황을 판단하는 데 유용한 자료가 될 수 있다. 위성을 통한 수위 추정 방법은 위성영상에서 탐지된 수표면을 DEM과 중첩하여 판독하는 방법인 imaging 기법과 레이더고도계로 불리는 altimeter로 위성에서 수표면까지의 거리를 직접 측정하여 산출하는 profiling 기법 등 크게 두 가지 방법이 있다. 본 연구에서는 위성영상으로 산출된 DEM과 ESA의 Sentinel-1 C-밴드 SAR 영상을 중첩하여 황강댐 수위를 추정해 보았다. 정확도 문제가 있겠지만, 황강댐 수위 변화의 경향성은 확인할 수 있었으므로, 향후 개선을 통해 황강댐 수위변동 추세 분석과 상황별 적절한 사전 대응에 활용할 수 있을 것으로 판단된다.

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Seasonal Variations of Marine Water Quality and Eutorphication Index in Mokpo Harbour (목포항의 수질 및 부영양도의 계절 변화)

  • Kim Kwang Soo
    • Journal of the Korean Society for Marine Environment & Energy
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    • v.4 no.3
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    • pp.3-15
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    • 2001
  • The in situ observations and the seawater analyses were conducted for 3 years from August 1996 to August 1999 in order to elucidate and evaluate seasonal variations of marine water quality and trophic state in Mokpo harbour of Korea. Compared the seasonal seawater qualities of Mokpo harbour with the OECD standards of trophic classification in parameters such as Secchi depth, dissolved inorganic nitrogen, phosphate phosphorus and chlorophyll-a, the trophic level of seawater in Mokpo harbour was evaluated to be in mesotrophic or eutrophic state through all 4 seasons and to be in eutrophic state, particularly In summer. The estimation of pollution index by eutrophication showed the seawater quality of Mokpo harbour to deteriorate and fall under the regular grades through all 4 seasons, although the seawater quality of Mokpo harbour was evaluated to be equivalent to the second or third class of the Korean seawater quality standards in view of COD values. The results of eutrophication index estimation showed the high potentiality of red tide occurrence In Mokpo harbour, particularly in summer or fall. In the light of the average atomic ratio of N/P in seawater, the limiting nutrient factor against the growth of phytoplankton was concluded to be phosphorus rather than nitrogen in Mokpo Harbour.

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Estimation of Groundwater Recharge Ratio Using Cumulative Precipitation and Water-level Change (누적 강수량과 지하수위 곡선을 이용한 지하수 함양률 추정 기법)

  • 문상기;우남칠
    • Journal of Soil and Groundwater Environment
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    • v.6 no.1
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    • pp.33-43
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    • 2001
  • A calculation technique which estimates natural recharge using groundwater level change was proposed and prepared with the existing techniques using groundwater recession curve during dry days. As a part of estimating natural groundwater recharge nation wide, the reliable data from the national groundwater monitoring network were used and the methodology was applied to the three sites which have enough data (Chungju, Jinju and Kwangju). For this study, seasonal variation of groundwater level change, an analysis of lagging time on groundwater level and cumulative precipitation, and a comparative study for groundwater recharge were conducted.

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ESTIMATION OF SEAWATER LEVEL ON SEA FARMS USING L-BAND RADAR INTERFEROMETRY

  • Kim, Sang-Wan;Won, Joong-Sun
    • Proceedings of the KSRS Conference
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    • 2002.10a
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    • pp.312-316
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    • 2002
  • Satellite radar interferometry data shows a strong coherent signal on oyster sea farms where artificial structures installed on the bottom. We obtained 21 highly coherent interferograms from eleven JERS-1 SAR data sets despite of large orbital baseline (~2 km) or large temporal baseline (~l year). The phases observed in sea farms are probably induced by double bouncing on sea surface, and consequently reveal a tide height variation. To restore the absolute sea level changes we counted the number of wrapping by exploiting the intensity of backscattering. Backscattering intensity is closely correlated with the change in water surface height, while interferometry gives the detailed variation within the limit of 2$\pi$ (or 15.3 cm). Comparing the radar measurements with the tide gauge records yielded a correlation coefficient of 0.96 and an ms error of 6.0 cm. The results demostrate that radar interferometry is promising to measure sea level.

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