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Malaysia Water Research Journal<br />
4.3 Hydrodynamic Model<br />
The hydrodynamic modelling only considered the tidal effect. Based on the<br />
hydrodynamic modeling, the average current speed in the study area is 0.1 - 0.8<br />
m/s which the highest speed occured at the estuary. Results also showed that<br />
the maximum current speed for the study area is 1.8 m/s and along the river it<br />
reaches up to 0.7 m/s. The current speed was lower in the ocean compared to<br />
the river with a difference of 0.2 m/s. Modelling of the study area for the projected<br />
sea level rise for 2020 with 0.034 m show increment in current speed. The average<br />
current speed is expected to be 0.15 - 0.85 m/s. Analysis for 2020 showed the<br />
estuary has the highest current speed of 0.85 m/s while the river recorded an<br />
average flow velocity of 0.3 - 0.5 m/s. The maximum current speed in Kuala<br />
Pahang reaches up to 1.8 m/s and the river can go up to 0.9 m/s. Projected sea<br />
level rise of 0.144 m in year 2060 predicted that the study area will experience<br />
an increase of average current speed between 0.2 - 0.88 m/s. Statistical analysis<br />
showed the maximum current speed of the study area can reach between 0.8<br />
- 1.9 m/s.<br />
Projected sea level rise of 0.307 m in year 2100 showed the average current<br />
speed in Kuala Pahang ranges between 0.3 - 0.9 m/s and can reach a maximum<br />
speed of between 0.6 - 1.9 m/s. The maximum difference of current speed at<br />
the estuary showed increment of 0.1 - 0.2 m/s while the island area, meanders<br />
of the river and the southern estuary experienced a decline of 0.06 - 0.1 m/s.<br />
Models comparison for 2020 and 2014 show an increment in the average current<br />
speed to 0.02 - 0.04 m/s and the maximum speed can go to 0.02 - 0.1 m/s.<br />
The analysis also showed a reduction in the current speed between 0.001 - 0.02<br />
m/s. Comparison of model years 2060 and 2014 show the average difference<br />
between the current speed 0.02 to 0.05 m/s and the maximum difference is<br />
0.05 to 0.06 m/s. The analysis also showed that the area recorded a decrease<br />
in current speed between 0.02 to 0.05 m/s near the island and south of Kuala<br />
Pahang. Comparative analysis of model for years 2100 and 2014 shows the<br />
study area having increment in the average current speed between 0.03 to 0.18<br />
m/s in the estuary and a slight decrease in the average current speed in the<br />
river and southern estuary of 0.01 m/s. See Table 3 for the predicted average<br />
and maximum current speed, residual current speed for the prospective years<br />
discussed here. The residual current speed at the estuary mouth for the future<br />
years was calculated based on the variation between the predicted sea level<br />
and the base level obtained on year 2014. The residual current speed profiles are<br />
shown in Figure 7.<br />
22<br />
Institut Penyelidikan Hidraulik Kebangsaan Malaysia (NAHRIM)<br />
National Hydraulic Institute of Malaysia (NAHRIM)