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Tidal component in the Java Sea are examined by using the model Ocean Tidal Inverse Solution (OTIS). Tidal components are examined is M2, N2, S2, K2, Q1, O1, P1 and K1. The data used and the model was entered into the amplitude and phase of the elevation in terms of open boundaries obtained from TOP...
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id-itb.:248232017-09-27T11:47:24Z#TITLE_ALTERNATIVE# ANGGA PUTRA (NIM : 12911011), YUNALDI Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/24823 Tidal component in the Java Sea are examined by using the model Ocean Tidal Inverse Solution (OTIS). Tidal components are examined is M2, N2, S2, K2, Q1, O1, P1 and K1. The data used and the model was entered into the amplitude and phase of the elevation in terms of open boundaries obtained from TOPEX/Poseidon elevation and bathymetry of the GEBCO data with a resolution of 1 minute. Other data used is the value of the amplitude and phase of the elevation in situ data obtained from Agency Geospatial Information (BIG) is used for verification. The results of the assimilation and without assimilation than with the value of the amplitude and phase of the tidal components obtained by BIG data and Tidal Model Driver (TMD). The area of study is the Java Sea with the model resolution is 1.5 KM and the dimensions of the grid is 451 x 151 grid. The boundaries of the area of study is 3-to-8 LS and 105 to 120 BT. <br /> <br /> <br /> Cophase map obtained from phase of tides components and corange map obtained from amplitude components of tides. The results of the verification and elevation graph assimilation data have smaller between non assimilation data and TMD text |
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Tidal component in the Java Sea are examined by using the model Ocean Tidal Inverse Solution (OTIS). Tidal components are examined is M2, N2, S2, K2, Q1, O1, P1 and K1. The data used and the model was entered into the amplitude and phase of the elevation in terms of open boundaries obtained from TOPEX/Poseidon elevation and bathymetry of the GEBCO data with a resolution of 1 minute. Other data used is the value of the amplitude and phase of the elevation in situ data obtained from Agency Geospatial Information (BIG) is used for verification. The results of the assimilation and without assimilation than with the value of the amplitude and phase of the tidal components obtained by BIG data and Tidal Model Driver (TMD). The area of study is the Java Sea with the model resolution is 1.5 KM and the dimensions of the grid is 451 x 151 grid. The boundaries of the area of study is 3-to-8 LS and 105 to 120 BT. <br />
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Cophase map obtained from phase of tides components and corange map obtained from amplitude components of tides. The results of the verification and elevation graph assimilation data have smaller between non assimilation data and TMD |
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Final Project |
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ANGGA PUTRA (NIM : 12911011), YUNALDI |
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ANGGA PUTRA (NIM : 12911011), YUNALDI #TITLE_ALTERNATIVE# |
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ANGGA PUTRA (NIM : 12911011), YUNALDI |
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ANGGA PUTRA (NIM : 12911011), YUNALDI |
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https://digilib.itb.ac.id/gdl/view/24823 |
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