TY - JOUR
T1 - Hydrodynamic and Sediment Transport Modelling of Suralaya Coastal Area, Cilegon, Indonesia
AU - Fattah, A. H.
AU - Suntoyo,
AU - Damerianne, H. A.
AU - Wahyudi,
N1 - Publisher Copyright:
© Published under licence by IOP Publishing Ltd.
PY - 2018/3/28
Y1 - 2018/3/28
N2 - The coastal zone of Suralaya is located in the district Pulomerak, Cilegon City, Province Banten. This region is a part of the Sunda Strait region that is very important area to support the ongoing activities such as, industries, power plant, ports, and tourism. However, those various activities will certainly give effect to the surrounding environment. To determine the environmental conditions of Suralaya Coast, it is necessary to study the hydrodynamics analysis and sediment transport modelling including the analysis of currents patterns. Tidal elevation observation was conducted for 15 days used to validate the water elevation simulation results, in which a good agreement between the observed data and the model result was obtained with the error value of 1.6%. The dominant current direction is from northeast in west season, while in the east season predominant current direction is from northwest with a speed average current 12,44 cm/s. The dominant wave direction is from the west. The average temperature is at 27°C and the bottom sediment dominant form is fine sand.
AB - The coastal zone of Suralaya is located in the district Pulomerak, Cilegon City, Province Banten. This region is a part of the Sunda Strait region that is very important area to support the ongoing activities such as, industries, power plant, ports, and tourism. However, those various activities will certainly give effect to the surrounding environment. To determine the environmental conditions of Suralaya Coast, it is necessary to study the hydrodynamics analysis and sediment transport modelling including the analysis of currents patterns. Tidal elevation observation was conducted for 15 days used to validate the water elevation simulation results, in which a good agreement between the observed data and the model result was obtained with the error value of 1.6%. The dominant current direction is from northeast in west season, while in the east season predominant current direction is from northwest with a speed average current 12,44 cm/s. The dominant wave direction is from the west. The average temperature is at 27°C and the bottom sediment dominant form is fine sand.
UR - http://www.scopus.com/inward/record.url?scp=85045660693&partnerID=8YFLogxK
U2 - 10.1088/1755-1315/135/1/012024
DO - 10.1088/1755-1315/135/1/012024
M3 - Conference article
AN - SCOPUS:85045660693
SN - 1755-1307
VL - 135
JO - IOP Conference Series: Earth and Environmental Science
JF - IOP Conference Series: Earth and Environmental Science
IS - 1
M1 - 012024
T2 - 4th International Seminar on Ocean and Coastal Engineering, Environmental and Natural Disaster Management, ISOCEEN 2016
Y2 - 13 December 2016 through 13 December 2016
ER -