VARIASI DAN TREN JANGKA PANJANG (1988â2011) ENERGI GELOMBANG DI PERAIRAN SELATAN JAWA DAN BARAT SUMATRA MENGGUNAKAN MODEL SIMULATING WAVES NEARSHORE (SWAN)
This study explores to reveal the characteristic (variability and climatic long term trend) of The West Sumatra and South Java Sea Significant Wave Height (SWH) and wave power density for the period 1988–2011 using hindcasting data from Simulating WAve Nearshore (SWAN). The wind data input is com...
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Format: | Final Project |
Language: | Indonesia |
Online Access: | https://digilib.itb.ac.id/gdl/view/44797 |
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Institution: | Institut Teknologi Bandung |
Language: | Indonesia |
Summary: | This study explores to reveal the characteristic (variability and climatic long term
trend) of The West Sumatra and South Java Sea Significant Wave Height (SWH) and wave
power density for the period 1988–2011 using hindcasting data from Simulating WAve
Nearshore (SWAN). The wind data input is coming from Cross-Calibrated Multi-Platform
(CCMP) with grid resolution 0.25°×0.25°. Unstructured grid is implemented in the model for
better flexibility rather than nesting method.
Results show that (1) significant wave height output from simulation gives good
agreement with buoy and satelite observation in Indonesian inner sea. Verification result at
the main study region is not as good as Indonesian inner sea result because the size of the
model domain does not include incoming swell from high latitude area, (2) highest seasonal
mean of significant wave height and wave power density occuring in JJA, (3) West Sumatra
and South Java Sea generally exhibits an increasing trend in SWH 1.04 cm/year and wave
power density 94.6 W/m/year. (4) there is a noticeable great potential of SWH and wave power
density in South of west Sumatranean waters and West of South Java Sea with average SWH
of 1.21 m and wave power density of 4.42 kW/m, The trend of SWH and wave power density in
this region also exhibits a significant increasing trend with value of SWH is 1.39 cm/year and
wave Power density trend 0.10 [(kW/m)/year], (5) El Ni????????o Phenomenon can decrease the
average value of significant wave height and wave power density in study area, (6) the
increasing wind speed trend is possibly happened because the duration of the research is
coincide with transition time from warm phase to cold phase in Pasific Decadal Oscillation
(PDO) index, (7) there is an increasing of SWH and wave power density in most part of West
Sumatra and South Java Sea with the most noticeable trend occuring in DJF and MAM rather
than JJA and SON. |
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