Conclusions Recommendations Membangun Peta Bahaya Banjir Rob di Wilayah Pesisir (Studi Kasus: Surabaya, Jawa Timur, Indonesia).

42 V . C O N C L U S I O N S A N D R E C O M M E N D A T I O N

5.1 Conclusions

From the foregoing discussion, the following conclusions are derived: 1. Hazard map could be established using combination between sea level projection data, vulnerability data, and field survey data. 2. The MRI-CGCM model was quite good to predict sea level rise having accuracy of 93.3. 3. The tidal flood predicted will mostly occurred in Northern and Eastern part of Surabaya. The predominantly vulnerable areas are residential, warehouse building, and embankment. 4. The total loss estimation for 2010, 2030 and 2100 respectively are 370 billion, 2 trillion and 3.6 trillion rupiahs.

5.2 Recommendations

The following are some recommendation proposed: 1. A deep survey and analysis of the latest condition about asset price of the land use, recorded data about duration of usual inundation by tidal flood characteristic, socio-economic intangible impact, small scope site area and measurement of penetration flood energy to the mainland - relief of front coast material, calculation rapid sedimentation model are required to make prediction of loss damage more accurate. 2. Future study should examine the reliability of the sea level projection equation model in other site. The standard price of land use type to the natural disaster in Indonesia is required to make estimation of loss more easily. 3. Actions that should be performed to reduce the tidal flood impact are: re- planning vulnerable area by relocates the settlements within 6 km from the coastline, mangrove reforestation and development of the breakwater. 43 R E F E R E N C E S Abidin, H.Z., H. Andreas, I. Gumilar, M. Gamal, Y. 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Sensitivity Analysis on Lake Biwa under the A1B SRES Climate Change Scenario Using Biwa-3D Integrated Assessment Model: Part I – Projection of Lake Temperature. Disaster Prevention Research Institute, Kyoto University, Gokasho, Uji City, Kyoto, Japan. 48 A P P E N D I C E S Appendix 1: SOI Southern Oscillation Index Source from: CGD 2010. 49 Appendix 2: Oceanic Nino Index ONI 1950 – 2010 source from NOAA 2010 Year DJ F JF M FM A MA M AM J MJ J JJ A JA S AS O SO N ON D ND J 1950 -1.7 -1.5 -1.3 -1.4 -1.3 -1.1 -0.8 -0.8 -0.8 -0.9 -0.9 -1 1951 -1 -0.9 -0.6 -0.3 -0.2 0.2 0.4 0.7 0.7

0.8 0.7

0.6 1952

0.3 0.1 0.1 0.2 0.1 -0.1 -0.3 -0.3 -0.2 -0.2 -0.1 1953 0.2 0.4 0.5 0.5 0.5

0.5 0.4

0.4 0.4 0.4 0.4 0.4 1954 0.5 0.3 -0.1 -0.5 -0.7 -0.7 -0.8 -1 -1.2 -1.1 -1.1 -1.1 1955 -1 -0.9 -0.9 -1 -1 -1 -1 -1 -1.4 -1.8 -2 -1.9 1956 -1.3 -0.9 -0.7 -0.6 -0.6 -0.6 -0.7 -0.8 -0.8 -0.9 -0.9 -0.8 1957 -0.5 -0.1 0.3

0.6 0.7

0.9 0.9 0.9 0.9 1 1.2

1.5 1958