Analysis on the estimation errors of the lowest and highest astronomical tides for the southwestern 2.5 GW offshore wind farm, Korea
For the design of wind-power facilities, the highest and lowest astronomical tides (HAT and LAT, respectively) are needed for the tidal-water levels regarding international designs; however, the approximate highest high water and approximate lowest low water AHHW and ALLW, respectively, have been us...
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Language: | English |
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Elsevier
2018-01-01
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Series: | International Journal of Naval Architecture and Ocean Engineering |
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Online Access: | http://www.sciencedirect.com/science/article/pii/S2092678216307117 |
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author | Dong Hui Ko Shin Taek Jeong Hong-Yeon Cho Keum-Seok Kang |
author_facet | Dong Hui Ko Shin Taek Jeong Hong-Yeon Cho Keum-Seok Kang |
author_sort | Dong Hui Ko |
collection | DOAJ |
description | For the design of wind-power facilities, the highest and lowest astronomical tides (HAT and LAT, respectively) are needed for the tidal-water levels regarding international designs; however, the approximate highest high water and approximate lowest low water AHHW and ALLW, respectively, have been used in Korea. The HAT and LAT in the wind-farm test-bed sea should be estimated to satisfy the international standard. In this study, the HAT and LAT are therefore estimated using the hourly tidal-elevation data of the Eocheongdo, Anmado, Younggwang, Gunsan, Janghang, and Seocheon tidal-gauging stations that are located in the adjacent coastal sea. The nodal variation patterns of the major lunar components, such as M2, O1, and K1 are analyzed to check the expected long-term lunar cycle, i.e., 18.61 year's nodal-variation patterns. The temporal amplitude variations of the M2, O1, and K1 clearly show the 18.61-years periodic patterns in the case of the no-nodal correction condition. In addition, the suggested HAT and LAT elevations, estimated as the upper and lower confidence limits of the yearly HAT and LAT elevations, are 50 cm greater than the AHHW and 40 cm lower than the ALLW, respectively. |
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issn | 2092-6782 |
language | English |
last_indexed | 2024-12-22T01:36:26Z |
publishDate | 2018-01-01 |
publisher | Elsevier |
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series | International Journal of Naval Architecture and Ocean Engineering |
spelling | doaj.art-d02cb944e7d145278816dac2ef3318a92022-12-21T18:43:22ZengElsevierInternational Journal of Naval Architecture and Ocean Engineering2092-67822018-01-01101859410.1016/j.ijnaoe.2017.03.004Analysis on the estimation errors of the lowest and highest astronomical tides for the southwestern 2.5 GW offshore wind farm, KoreaDong Hui Ko0Shin Taek Jeong1Hong-Yeon Cho2Keum-Seok Kang3Coastal Development Research Center, Coastal Engineering Division, Korea Institute of Ocean Science & Technology, 787 Haean-ro, Sangnok-gu, Ansan, Gyeonggi-do 15627, Republic of KoreaDepartment of Civil and Environmental Engineering, Wonkwang University, 460, Iksandae-ro, Iksan, Jeolla-bukdo 54538, Republic of KoreaOcean Data Science Section, Korea Institute of Ocean Science and Technology, 787, Haean-ro, Sangnok-gu, Ansan, Gyeonggi-do 15627, Republic of KoreaRenewable Energy Group, KEPCO Research Institute, 105 Munji-ro, Yuseong-gu, Daejeon 34056, Republic of KoreaFor the design of wind-power facilities, the highest and lowest astronomical tides (HAT and LAT, respectively) are needed for the tidal-water levels regarding international designs; however, the approximate highest high water and approximate lowest low water AHHW and ALLW, respectively, have been used in Korea. The HAT and LAT in the wind-farm test-bed sea should be estimated to satisfy the international standard. In this study, the HAT and LAT are therefore estimated using the hourly tidal-elevation data of the Eocheongdo, Anmado, Younggwang, Gunsan, Janghang, and Seocheon tidal-gauging stations that are located in the adjacent coastal sea. The nodal variation patterns of the major lunar components, such as M2, O1, and K1 are analyzed to check the expected long-term lunar cycle, i.e., 18.61 year's nodal-variation patterns. The temporal amplitude variations of the M2, O1, and K1 clearly show the 18.61-years periodic patterns in the case of the no-nodal correction condition. In addition, the suggested HAT and LAT elevations, estimated as the upper and lower confidence limits of the yearly HAT and LAT elevations, are 50 cm greater than the AHHW and 40 cm lower than the ALLW, respectively.http://www.sciencedirect.com/science/article/pii/S2092678216307117Wind-farm test-bed seaHighest astronomical tide (HAT)Lowest astronomical tide (LAT)AHHW and ALLWNodal correction |
spellingShingle | Dong Hui Ko Shin Taek Jeong Hong-Yeon Cho Keum-Seok Kang Analysis on the estimation errors of the lowest and highest astronomical tides for the southwestern 2.5 GW offshore wind farm, Korea International Journal of Naval Architecture and Ocean Engineering Wind-farm test-bed sea Highest astronomical tide (HAT) Lowest astronomical tide (LAT) AHHW and ALLW Nodal correction |
title | Analysis on the estimation errors of the lowest and highest astronomical tides for the southwestern 2.5 GW offshore wind farm, Korea |
title_full | Analysis on the estimation errors of the lowest and highest astronomical tides for the southwestern 2.5 GW offshore wind farm, Korea |
title_fullStr | Analysis on the estimation errors of the lowest and highest astronomical tides for the southwestern 2.5 GW offshore wind farm, Korea |
title_full_unstemmed | Analysis on the estimation errors of the lowest and highest astronomical tides for the southwestern 2.5 GW offshore wind farm, Korea |
title_short | Analysis on the estimation errors of the lowest and highest astronomical tides for the southwestern 2.5 GW offshore wind farm, Korea |
title_sort | analysis on the estimation errors of the lowest and highest astronomical tides for the southwestern 2 5 gw offshore wind farm korea |
topic | Wind-farm test-bed sea Highest astronomical tide (HAT) Lowest astronomical tide (LAT) AHHW and ALLW Nodal correction |
url | http://www.sciencedirect.com/science/article/pii/S2092678216307117 |
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