SIMULATION OF THE IMPACT OF LAND COVER CHANGES ON WIND PATTERNS AND CIRCULATIONS IN INDONESIAâS NEW CAPITAL CITY
The development of the Nusantara Capital City (IKN) will significantly change its land cover. A previous study has shown that the projected increase in urban areas in the IKN is expected to contribute to temperature rise in the region. However, the impact of urban expansion goes beyond temperatur...
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| Format: | Final Project |
| Language: | Indonesia |
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| Online Access: | https://digilib.itb.ac.id/gdl/view/75976 |
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| Institution: | Institut Teknologi Bandung |
| Language: | Indonesia |
| Summary: | The development of the Nusantara Capital City (IKN) will significantly change its
land cover. A previous study has shown that the projected increase in urban areas
in the IKN is expected to contribute to temperature rise in the region. However, the
impact of urban expansion goes beyond temperature changes, it also affects wind
patterns and circulations. Therefore, simulating the impact of land cover changes
on wind patterns and circulations in the IKN is crucial for a comprehensive
understanding of its effects on the local weather.
This study conducted weather simulations using the mesoscale numerical weather
prediction model, Weather Research and Forecasting (WRF), coupled with the
Urban Canopy Model (UCM), on modified land cover based on the plans for the
development of the IKN. The simulation results were compared with weather
simulations on the land cover prior to the development of the IKN.
Based on the simulation results, under strong upwind and no rainfall conditions,
the presence of urban areas in the IKN region led to an increase in temperature, a
decrease in wind speed, and an increase in convergence in the area. However,
during nighttime simulations (6 p.m. to 12 a.m. local time), the increasing
temperature tends to occur mainly in the Core Government Center (KIPP) area.
Additionally, wind speed tends to increase around the KIPP area. Land cover
changes not only affected the IKN region but also had an impact on the downwind
area, resulting a significant decrease in wind speed (reaching >2 m/s) in that area
at night. This reduction in wind speed decreased turbulence during the night, which
consequently led to a significant temperature decrease (reaching >0.75 °C) in that
area. |
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