#TITLE_ALTERNATIVE#
Sea level rise for the year 2013-2030 in South Sumatera was calculated from the sea level rise projection from global climate model used by IPCC with SRES A1B, tide influenced which is HHWL and MHWL, La-Niña influenced to the sea level, sea level rise due to storm surge, and annual flood in the s...
Saved in:
| Main Author: | |
|---|---|
| Format: | Final Project |
| Language: | Indonesia |
| Online Access: | https://digilib.itb.ac.id/gdl/view/18688 |
| Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
| Institution: | Institut Teknologi Bandung |
| Language: | Indonesia |
| Summary: | Sea level rise for the year 2013-2030 in South Sumatera was calculated from the sea level rise projection from global climate model used by IPCC with SRES A1B, tide influenced which is HHWL and MHWL, La-Niña influenced to the sea level, sea level rise due to storm surge, and annual flood in the study area. Tide is the most influential parameter of sea level rise variation. Sea level rise which affected by MHWL has maximum duration 13 hours every month for 4-5 days in spring tide condition and occurred for 1-3 hours every day. Sea level rise which affected by HHWL has maximum duration 3 hours every month for 2-3 days in spring tide condition and occurred for 1-1,5 hours every day. All of parameters will later accumulate on to hazard scenario of sea level rise and sea level rise hazard map. The highest prediction of sea level rise occurs in December 2025-Februari 2026 with 298 cm for the dominant influence of MHWL and 338 cm for the dominant influence of HHWL. All the sea level risk map scenario in South Sumatera yield 9.64-15.54 % flooded area on 2013 and 9,78-15,63 % on 2030 of total area South Sumatera. The city or district that will be flooded are Palembang City, District of Banyuasin, District of Musi Banyuasin, District of Ogan Komering Ilir, District of Ogan Ilir and District of Muara Enim |
|---|