IDENTIFICATION OF METOCEAN PARAMETERS AFFECTING COASTAL FLOODS IN THE CITY OF SEMARANG, CENTRAL JAVA, INDONESIA
Coastal flooding is a phenomenon where sea water enters and inundates the land. Semarang City is one of the coastal areas in Indonesia that is vulnerable to coastal flooding. Some of the factors that affect coastal flooding include tides, sea level rise, land subsidence, and meteorological fac...
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Format: | Final Project |
Language: | Indonesia |
Online Access: | https://digilib.itb.ac.id/gdl/view/85224 |
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Institution: | Institut Teknologi Bandung |
Language: | Indonesia |
Summary: | Coastal flooding is a phenomenon where sea water enters and inundates the land.
Semarang City is one of the coastal areas in Indonesia that is vulnerable to coastal
flooding. Some of the factors that affect coastal flooding include tides, sea level
rise, land subsidence, and meteorological factors. The phenomenon of non-tidal
elevation, associated with sea surface height anomaly (SSHA) data, wind speed,
and rainfall, was the subject of this research. The Meteorology, Climatology, and
Geophysics Agency at the Tanjung Emas Maritime Meteorological Station
Semarang and the University of Hawaii Sea Level Center (UHSLC) at Semarang
Station provided the sea level elevation data used in this study for a period of 4.8
years (May 2018–December 2022). The threshold for the definition of coastal
flooding used in this study is the non-tidal elevation that exceeds the data's standard
deviation. According to the calculation results, the threshold used for coastal
flooding in this study varies depending on the scenario. This study used five
scenarios, with scenarios 1 and 3 being the closest to the news coastal flood event.
The results of the analysis showed that the highest occurrence and intensity of the
analyzed coastal floods occurred in May and June, whose periods coincided with
the dry season. Analysis of the composite average of coastal flood events shows that
the metocean parameters that have the most influence on the occurrence of
analyzed coastal floods are SSHA and wind speed.
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