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dc.contributor.advisorSitumorang, Marhaposan
dc.contributor.advisorSinambela, Marzuki
dc.contributor.authorMarpaung, Christen Ordain Novena
dc.date.accessioned2022-11-01T07:32:46Z
dc.date.available2022-11-01T07:32:46Z
dc.date.issued2021
dc.identifier.urihttps://repositori.usu.ac.id/handle/123456789/52161
dc.description.abstractOne of the high risk area for tidal flood is Belawan. Tidal flood in Belawan occur due to the interaction of tides, significant wave, and swell that influence each other. A tidal flood is the inundation of sea water on the mainland coast caused by high tides. The existence of high tide and low tides will affect to the condition of inundation occurred. The purpose of this research was conducted to determine the dynamics of those three sea-level phenomena during the tidal floods in Belawan on 2020. The tidal’s data of Geospatial Information Center, significant wave high, and swell are the result processing of Wavewatch-III model, and sea level high data is the result of Jason-2 altimetri satellite. The analysis of tidal’s data processing from Geospatial Information Center shows that the maximum tide happened on 17 October 2020 with value 2,47 meters, there is a shift of the highest tide’s peak in 3-4 days of spring tide position. The verification results of Geospatial Information Center and Jason-2 Altimetri satellite has good correlation value but the Jason-2 altimetri satellite data tends to be under estimated.en_US
dc.language.isoiden_US
dc.publisherUniversitas Sumatera Utaraen_US
dc.subjectTidal Flooden_US
dc.subjectOcean Wavesen_US
dc.subjectSwellen_US
dc.subjectWavewatch – IIIen_US
dc.subjectJason-2 Altimetri Satelliteen_US
dc.titleKajian Pasang Surut, Gelombang, dan Swell pada Saat Kejadian Banjir Rob di Belawanen_US
dc.typeThesisen_US
dc.identifier.nimNIM197026005
dc.identifier.nidnNIDN0030105504
dc.identifier.kodeprodiKODEPRODI45101#Fisika
dc.description.pages105 Halamanen_US
dc.description.typeTesis Magister


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