• Title/Summary/Keyword: Tidal effects

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Physical Environment Changes in the Keum River Estuary by the Dyke Gate Operation: I. Mean Sea Level and Tide (하구언 수문작동으로 인한 금강 하구역의 물리적 환경변화: I. 평균해수면과 조석)

  • Kwon, Hyo-Keun;Lee, Sang-Ho
    • The Sea:JOURNAL OF THE KOREAN SOCIETY OF OCEANOGRAPHY
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    • v.4 no.2
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    • pp.93-100
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    • 1999
  • Analyzing the tide data taken at Kunsan inner and Outer ports, non-tidal and mean sea level and harmonic constants of major constituents are investigated to examine the effects of the dyke gate operation on the sea level change in Keum River estuary. Non-tidal and annual mean sea levels decrease at Kunsan Inner and Outer ports after the dyke gate operation, especially showing an abrupt drop of non-tidal sea level at Kunsan Inner port. This non-tidal sea level drop results in the mean sea level gradient change between the inner and outer port, which can be mainly explained in terms of the decrease of river discharge from the dyke. Amplitudes of the $M_2$ and $S_2$ tides at the Inner port increase after the dyke gate operation, showing an abrupt jump, and phases of both tides slightly decrease. Amplitude and phase of the $K_1$ and $O_1$ tides show slight changes after the dyke gate operation. This significant change of semi diurnal tide amplitude is believed as a result of superposition of incident tidal wave and reflected tidal wave from the dyke.

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Tidal Flat Simulation Characteristics of the Hydrodynamic Models (해수유동모형의 조간대 모의 특성)

  • Kang, Ju-Whan;Park, Seon-Jung;Kim, Yang-Seon;So, Jae-Kwi
    • Journal of Korean Society of Coastal and Ocean Engineers
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    • v.21 no.5
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    • pp.357-370
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    • 2009
  • EFDC, ESCORT and MIKE21 models are applied at the Gomso Bay to investigate each models' facilities of tidal flat simulation. Comparisons with observation data show that all models simulate hydrodynamic phenomena and tidal flat well. CPU time and WCM are examined to evaluate the efficiency of the models, and the effects of flooding/drying depth and bottom friction are examined to analyze models' facilities of simulating tidal flat. The EFDC model is considered to be fairly good in accuracy, stability and applicability, it is, however, poor in efficiency and its complexity. While the ESCORT model is superior to the EFDC in simulation of tidal flat, it is inferior to the EFDC in CPU time and simulation of bottom friction. The MIKE21 model is excellent in efficiency, but some numerical noise would be detected at low water, not permitting correction of the model.

A Study on the Environmental Assessment Guideline for Tidal Current Energy Development (조류발전 사업의 환경평가 가이드라인 연구)

  • Kim, Tae-Yun;Park, Jeong-Il;Maeng, Jun-Ho
    • Journal of the Korean Society of Marine Environment & Safety
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    • v.20 no.4
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    • pp.345-357
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    • 2014
  • This study aims to develop a guideline of environmental assessment for tidal current energy development in Korea. Based on an extensive discussion of the environmental effects of tidal current energy, this study provides an appropriate guideline for environmental assessment on tidal current energy development in Korea. The guideline includes a method for proper site selection and specific techniques for environmental impact assessment. The guideline for environmental impact assessment consists of four steps - including current condition investigation, impact predictions, identification and incorporation of mitigation measures, and post environmental monitoring - to effectively predict and assess impacts of tidal current energy development on the ocean environment. It is expected that the guideline can facilitate the often demanding environmental assessment review process and to reduce the time taken for it.

Seasonal Changes of Tidal-flat Sediments: Kwangyang Bay, South Coast of Korea (조간대 퇴적물의 계절적 변화 : 한국 남해안의 광양만)

  • 류상옥;김주용;이희준;조영길;안성모
    • The Sea:JOURNAL OF THE KOREAN SOCIETY OF OCEANOGRAPHY
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    • v.8 no.4
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    • pp.349-356
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    • 2003
  • A continuous monitoring of sedimentation rate and textural characteristics of surface sediments was carried out on the tidal flats in Kwangyang Bay, middle South Sea for two years on an every-two-monthly basis. This study shows that during the winter the tidal flats receive a thin surface layer of which texture becomes finer. In summer, the surface sediments were subject to rather abrupt erosion by occational typhoons and heavy rainfall resulting in a coarse-silt dominated texture. Due to nearly closed geomorphology of Kwangyang Bay, local waves created in the bay during winter are much subdued, in contrast to the rough wave climate and associated sedimentary cycle for open-type tidal flats in the Yellow Sea. In addition, unexpected artificial effects on the tidal-flat sedimentation by construction of a huge industrial complex along the shoreline of the bay are observed from a nearby tidal flat. Here, the sediments were consistently eroded without any sign of natural seasonal variations.

Tidal Propagation in the Han River (한강감조구간의 조석전파)

  • Choe, Seung-Ho;Lee, Jeong-Yeol;Seo, Gyeong-Seok
    • Water for future
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    • v.20 no.2
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    • pp.151-160
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    • 1987
  • The development of the tidal asymmetries and the effect of an increased discharge on tide propagating into the Han River was studied quantitatively via numerical integration of one-demensional equations. The model results indicated that some tidal components including $, $, $ were actually be amplified over a segment of the river. The computed results on the effects of increased discharges on the tide were in good agreement with theoretical inference(Godin, 1985).

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Seasonal Variation of Heterotrophic Activity in the Estuary of Naktong River over Half Tidal Cycle and Salinity Effect (낙동강 하구의 조석변화에 따른 Heterotrophic Activity의 계절적 변화와 염분의 영향)

  • 안태영;박중찬;하영칠
    • Korean Journal of Microbiology
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    • v.29 no.5
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    • pp.339-343
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    • 1991
  • Heterotrophic activity, total bacteria and salinity were determined seasonally in the estuary of Naktong River over half tidal cycle. Heterotrophic activity was determined by the uptake of [U- $^{14}$ C]glucose. Heterotrophic activity fluctuated with the tides and was decreased as salinity increased. Teh great activity occurred near low ebb tide at all seasons except summer. The main environmental factor affecting hetreotrophic activity was the salinity rather than water temperature in the estuary of Naktong River. In order to estimate the effect of salt, salt was added to estuarine water. Vmax for glucose of salt-added water was 17% and 77% of original estuarine water at station 1 and 2 respectively and slight increase was observed at station 3. Respiration rate and Kt+Sn for glucose of salt-added sample increased at all 3 stations. The increase of the Kt value implies the reduced affinity of bacterial population for glucose. The effects of salinity on the heterotrophic activity were more extensive in the upper region of estuary than at the mouth.

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Interference Effects on the Performance of Multi-arrayed HAT TCP Devices (복합배치 수평축 조류발전 로터의 간섭성능 고찰)

  • Jo, Chul-Hee;Lee, Kang-Hee;Yim, Jin-Young;Rho, Yu-Ho
    • The KSFM Journal of Fluid Machinery
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    • v.13 no.2
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    • pp.36-40
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    • 2010
  • Tidal current power system is the energy converter which converts the kinetic energy of tidal stream into electric energy. The performance of the rotor which initially converts the energy is determined by various design factors and it should be optimized by the ocean environment of the field. Flow direction changes due to rise and fall of the tides, but horizontal axis turbine is very sensitive to direction of flow. To investigate the rotor performance considering the interaction problems with incidence angle of flow, series of experiments have been conducted. The results and findings are summarized in the paper.

Difference of Clay Mineral Compositions between Holocene and Late Pleistocene Tidal Deposits in the Haenam Bay, Korea: Evidence of Subaerial Exposure and Weathering

  • Park, Yong-Ahn;Choi, Jin-Yong;Lim, Dhong-Il
    • Journal of the korean society of oceanography
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    • v.32 no.3
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    • pp.138-144
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    • 1997
  • The tidal deposits in the Haenam Bay, southwest coast of Korea, are stratigraphically divided at least into two units (Unit I of Holocene and Unit II of late Pleistocene) based on the obtained vibracoring sediments. In Unit I, clay minerals of illite, chlorite, kaolinite and smectite are observed as similar to those of the other modern tidal deposits. Of note, however, is the absence of smectite and chlorite in the upper part of Unit II compared with the clay mineral compositions of Unit I. It is concluded that the subaerial weathering and diagenetic effects rather than depositional processes are responsible for the positive and characteristic differences in clay mineral compositions between two units, that is, the upper part of Unit II was exposed subaerially and weathered diagenetically prior to the late Holocene transgression. Therefore, the bounding relationship between Unit I and Unit II is unconformable.

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HAT Tidal Current Rotor Performance as per various Design Parameter (조류발전 로터 설계변수에 따른 성능 검토)

  • Jo, Chul-Hee;Yim, Jin-Young;Lee, Kang-Hee;Song, Seung-Ho
    • 한국신재생에너지학회:학술대회논문집
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    • 2009.11a
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    • pp.590-593
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    • 2009
  • Tidal current power system is one of ocean renewable energies that can minimize the environmental impact with many advantages compared to other energy sources. Not like others, the produced energy can be precisely predicted without weather conditions and also the operation rate is very high. To convert the current into power, the first device encountered to the incoming flow is the rotor that can transform into rotational energy. The performance of rotor can be determined by various design parameters including numbers of blade, sectional shape, diameter, and etc. The stream lines near the rotating rotor is very complex and the interference effects around the system is also difficult to predict. This paper introduces the experiment of rotor performance and also the effect of design parameter on the performance of HAT rotor by CFD.

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TIDAL EVOLUTION OF LUNAR ORBIT AND EARTH ROTATION

  • Na, Sung-Ho
    • Journal of The Korean Astronomical Society
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    • v.45 no.2
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    • pp.49-57
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    • 2012
  • In this study, I calculate the past and future dynamical states of the Earth-Moon system by using modified Lambeck's formulae. I find that the ocean tidal effect must have been smaller in the past compared to its present amount. Even though the Moon is already in the spin-orbit synchronous rotational state, my calculation suggest that it will not be in geostationary rotational state in the next billion years or so. This is due to the associated Earth's obliquity increase and slow retardation of Earth's spin and lunar orbital angular velocities. I also attempt to calculate the precessional period of the Earth in the future. To avoid uncertainties in the time scale, the future state is described by using the Earth-Moon distance ratio as independent parameter. Effects due to solar tidal dissipation are included in all calculations.