<> <http://www.w3.org/2000/01/rdf-schema#comment> "The repository administrator has not yet configured an RDF license."^^<http://www.w3.org/2001/XMLSchema#string> .
<> <http://xmlns.com/foaf/0.1/primaryTopic> <http://digilib.unila.ac.id/id/eprint/464> .
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<http://digilib.unila.ac.id/id/eprint/464> <http://purl.org/dc/terms/title> "STUDYANALIS$ SPEKTRUM\r\nFREKUENSI KOMPONEN PASANG SURUT\r\n(Study Kasus Pasang Surut Stasiun Tanjung Priok)(STUDY SPECTRALANALYSIS OF TIDE TREQUENCIES\r\n(Case study: tide observation from Statiop of Tanjung Priok))"^^<http://www.w3.org/2001/XMLSchema#string> .
<http://digilib.unila.ac.id/id/eprint/464> <http://purl.org/ontology/bibo/abstract> "Kejadian pasang surut yang sering disebut pasut merupakan kejadian proses naik\r\nturunnya air laut secara periodik yang ditimbulkan adarrya gayatarik-menarik dari\r\nbenda-benda angkasq yang terutama sekali disebabkan oleh gaya tarik matahari\r\ndan gaya tarik bulan terhadap massa air bumi.\r\nGaya penggerak pasang surut yang rumit ini dapat diuraikan sebagai hasil\r\ngabungan sejumlah komponen harmonik pasut {harmonic constituerzfs). Doodson\r\nmengembangkan metode sederhana unfuk menenfukan komponen- komponen\r\n(constituents) utama pasang surut, Principal Lunsr (M2), Principal Solar (Sz),\r\nLarge Lunar Elliptic (Nz), Lunar-Solar (K2), Luni Solar Diurnal (Kr), Principal\r\nLunar Diurnal (Or), Principol Lunar Diurnal (Pr), Komponen Laut Dangkal\r\n(M+), dan Komponen Laut Dangkal (MS+), dengan menggunakan panjang data\r\npengamatan pasang surut 15 dan 29 hari dengan pengamatan jam-jaman.\r\nBiasanya didalam menganalisis pasang surut, kebanyakan dad para peneliti\r\nmenggwrakan 9 konstanta harmonik. Tetapi didalam studi ini, metode analysis\r\nspektrum dipergunakan untuk menghasilkan frekuensi pasang surut. Data pasang\r\nsurut dari stasiun Tanjung Periok dipergunakan untuk mempelajari frekuensi\r\nharmonik pasang surut. Didalam analisis, panjang data 15 hari dan 30 hari\r\ndipergunakan. Dari hasil penelitian ditunjukkan bahwa komponen pasang surut\r\ndari stasiun tanjung periok mempunyai 7 komponen dominan untuk data 15 hari\r\n(Kl, ol, Pl ,h42, s2, N2, K2) dan 6 komponen dominan untuk data 30 hari (K1,\r\n01, Pl, l:&dz,S2,Y\\2>.\r\nKnta kunci : Pasang Surut, analysis spektum, Tanjung Priok (The tides are the process of ups and downs of seawater periodically posed the\r\nexistence style athaction of celestial bodies, which most notably caused by\r\ngravitational forces of the Sun and the Moon pull style of water masses of the\r\nEarth.\r\nTidal oscillations can be deseribed as a combined result of a number of\r\ncomponents of the tide harmonics (harmonic constifuents). Doodson developed a\r\nsimple method to determine the components (constituents), Principal Main of the\r\nLunar tides (M2), the Principal Solar (S2), a Large Lunar Elliptic (N2), Lunar-\r\nSolar {Y.2), Luni Solar Diurnal (Kl), a Principal Lunar Diurnal (Ol), Principal\r\nLunar Diurnal (P1), Shallow Sea Components (M4), and Shallow Sea\r\nComponents (MS4), using tidal observations data length of 15 and 29 days with\r\nhourly observations.\r\nCommonly, in tide analysis, the most of researchers use I tide harmonic\r\nconstituents. But in this study, spectral analysis method is used to generate tidal\r\nfrequencies. Tide data from the station of Thnjung Periok is used to study\r\nfrequencies of tide harmonics. In the analysis, data length of 15 (fifteen) days and\r\nthirfy (30) days are used. From the results are presented that tidal constituents\r\nfrom station of Timjung Priok having 7 dominant constituents for the data of 15\r\ndays (K1,01, Pl, M2,g:2,N2, K2) and 6 dominantconstituents forthe data of 30\r\ndays (K1, Ol, Pl ,M2, 52, K2).\r\nKeywords : tides, spectral analysis, Thnjung Priok)"^^<http://www.w3.org/2001/XMLSchema#string> .
<http://digilib.unila.ac.id/id/eprint/464> <http://purl.org/dc/terms/date> "2013-09-23" .
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<http://digilib.unila.ac.id/id/document/31709> <http://eprints.org/relation/isVersionOf> <http://digilib.unila.ac.id/id/document/31575> .
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<http://digilib.unila.ac.id/id/document/31716> <http://eprints.org/relation/isVolatileVersionOf> <http://digilib.unila.ac.id/id/document/31579> .
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<http://digilib.unila.ac.id/id/document/31716> <http://eprints.org/ontology/hasFile> <http://digilib.unila.ac.id/464/45/preview.jpg> .
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<http://digilib.unila.ac.id/id/eprint/464> <http://eprints.org/ontology/hasDocument> <http://digilib.unila.ac.id/id/document/31717> .
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<http://digilib.unila.ac.id/id/document/31717> <http://eprints.org/relation/isVersionOf> <http://digilib.unila.ac.id/id/document/31579> .
<http://digilib.unila.ac.id/id/document/31717> <http://eprints.org/relation/isVolatileVersionOf> <http://digilib.unila.ac.id/id/document/31579> .
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<http://digilib.unila.ac.id/id/document/31717> <http://purl.org/dc/terms/hasPart> <http://digilib.unila.ac.id/464/46/medium.jpg> .
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<http://digilib.unila.ac.id/id/document/31721> <http://purl.org/dc/terms/hasPart> <http://digilib.unila.ac.id/464/50/medium.jpg> .
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<http://digilib.unila.ac.id/id/eprint/464> <http://eprints.org/ontology/hasDocument> <http://digilib.unila.ac.id/id/document/31730> .
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<http://digilib.unila.ac.id/id/subject/QE> <http://www.w3.org/1999/02/22-rdf-syntax-ns#type> <http://www.w3.org/2004/02/skos/core#Concept> .
<http://digilib.unila.ac.id/id/subject/QE> <http://www.w3.org/2004/02/skos/core#prefLabel> "QE Geology"@en .
<http://digilib.unila.ac.id/id/eprint/464> <http://purl.org/dc/terms/subject> <http://digilib.unila.ac.id/id/subject/QE> .
<http://digilib.unila.ac.id/id/subject/T1> <http://www.w3.org/1999/02/22-rdf-syntax-ns#type> <http://www.w3.org/2004/02/skos/core#Concept> .
<http://digilib.unila.ac.id/id/subject/T1> <http://www.w3.org/2004/02/skos/core#prefLabel> "Teknologi (General)"@id .
<http://digilib.unila.ac.id/id/eprint/464> <http://purl.org/dc/terms/subject> <http://digilib.unila.ac.id/id/subject/T1> .