Projection Until The End of Long Term Development Plan

When spring tide occurrence comes in next month of those each specific year, the impact of sea level change will be hugher than only by sea level rise and impacted area will be expanding. Spring tide in next 10 years Jan-2022 will increasing sea level and can reach 1.27 m above zero. With this level of sea surface, the land area that will be impacted will reach ±5,059 Ha with all of it landuse properties, infrastructure facilities road, and water channel. Spring tide in next 15 years Jan-2027 will increasing sea level and can reach 1.40 m above zero. With this level of sea surface, the land area that will be impacted will reach ± 5,581 Ha, covering ± 429 km of road, and ± 306 km of water channel. The ilustration of inundated area in next 10, 15 and 20 years can be seen in figure 4.11 Figure 4.11. Projecting inundated area in next 10, 15 and 20 tears from now In the end of RPJP Jan-2032 spring tide will impacted ± 6,041 Ha of land area with ± 465 km of road and ± 328 km of water channel passing those impacted land area. At that spring tide, sea level will reach 1.53 m so that the area that less than or equal to 1.53 m will be inundated by seawater. The properties that impacted by inundation in next 10, 15 and 20 year can be seen in table 4.7. Table 4.7. Properties that affecting by sea level rises combine with spring tide in next 10, 15 and 20 years LANDUSE TYPE INUNDATED AREA IN SPRING TIDE 2022 Ha INUNDATED AREA IN SPRING TIDE 2027 Ha INUNDATED AREA IN SPRING TIDE 2031 Ha Pond 72.976 75.395 78.145 Freshwater Pond 33.873 34.447 37.678 Shrub 4.219 4.219 4.219 Embankment 2412.283 2506.440 2545.451 Building 909.127 969.521 1022.798 Estuary forest 4.382 4.382 4.382 Planting Area 18.125 45.402 83.177 Settlement 1180.228 1421.042 1549.582 Marsh 17.313 21.381 23.174 Grassland 215.679 248.405 279.21 Irrigated Farming Area 162.153 204.884 274.806 Moor 29.463 45.644 139.325 ROAD TYPE INUNDATED BY SPRING TIDE IN 2022 Ha INUNDATED BY SPRING TIDE IN 2027 Ha INUNDATED BY SPRING TIDE IN 2031 Ha Bridge 372.875 372.875 372.875 Flying Bridge 109.393 109.393 109.393 Collector Road 0.000 0.000 0.000 Other Type of Road 4445.178 16721.724 23629.495 Local Road 347398.108 397571.141 424099.110 National Road 5954.630 7275.504 10080.393 Footpath 6634.104 6974.709 7028.548 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

Based on results of data analysis on eustatic and isostatic sea level rise and its impact to coastal area of Semarang City that experiencing subsidence especially in term of submergence area, there are some conclusions can be derived. Realistic tidal elevation data that has been derived using FVCOM was generated by included six tidal harmonic constituents S 2 , M 2 , N 2 , K 1 , P 1 , and O 1 altogether and didn’t count the effect of sea level rise to generate tides. As the result of tidal data analyst, the type of tides in Semarang coastal water is mixed mainly diurnal tide with highest peak tide value is 0.473 m. and lowest ebb tide value is -0.231 m. Global sea level change shown the linear increasing year by year since 1880 to 2009. The first time when sea level was equal to land was occurred in 1982 and had been passing this equality until unpredicted year. Regional sea level change in Indonesia’s area also shows the increasing by the time with increasing level 2.535. cmyear. As the impact sea level rise, sea level in Semarang City coastal water also increasing local sea level where height of sea level until 2010 was reached 94.669 cm MSL value and after correcting process using regional sea level rise, isostatic MSL in 2010 was 52.070 cm. Even subsidence is not the main object of the research, land subsidence level location where tide gauge located can be estimated by calculate the deviation between MSL data from tide gauge that experiencing subsidence and isostatic sea level. The result of estimation shows subsidence rate in Tanjung Mas area location where tide gauge located is 7.1 cmyear. As the impact of Sea level rise, submergence area that formed in 2011 was 1,043.527 Ha and predicted increase 4.4 times by spring tides. Seawater also covered ±149 km of road and ±67 km water channel, so that those facilities can run it function normally. Future projection shows that in next ten years submergence area will reach ± 3,627 Ha while in next 15 years submergence area will reach ± 4,364 Ha and in next 20 years submergence area will reach ± 4,641 Ha. When spring tides occur, the impact of sea level change will getting worst because area with altitude up to 0.47 from submergence area will be inundated by seawater.

5.2. Recommendations

Study on sea level change and its effect to submergence area in Semarang City coastal area has formulated several points of recommendations to local and national government, peoples in Semarang City, researcher and all readers such as follows: 1. Future study can be examining the model of sea level change using different tools and method like ROMS Regional Ocean Modeling System, HYCOM HYbrid Coordinate Ocean Model, or POM Princeton Ocean Model so that the result of FVCOM software that used in this research can be compared. 2. A deep survey and analysis of the latest condition about subsidence, inundation data record, water transport from upland through river to complement the result of this study so that the impact of total flood can be measured. Counting economic lost also can complement the result of this study. 3. Sea level change and subsidence that has been occur in Semarang and threaten human life and welfare because the lost as the impact of this hazard will be so huge need serious, integrated and sustainable effort to solve. Local government must be make strict rule to stop over water pumping one of the factors of land subsidence in Semarang City. 4. Build retaining materials, mangrove reforestation, and deepen the embankment have to do to block sea water inundated land area and contain the water that has been covered land area R E F E R E N C E S Abidin, H. Z, H. Andreas, I. Gumilar, T.P. Sidiq, M. Gamal, D. Murdohardono, Supriyadi and Y. Fukuda. 2010. Studying Land Subsidence in Semarang Indonesia Using Geodetic Methods. FIG Congress Sydney, Australia Allen, A. S. 1970. Type of Land Subsidence. In Guidebook to Studies Land Subsidence Due to Ground Water Withdrawal; 133-142. Burchard, H., K. Bolding, T. P. Rippeth, A. Stips, J. H. Simpson, and J. Sündermann. 2002. Microstructure of turbulence in the northern north sea: comparative study of observations and model simulations. Journal of Sea Research, vol. 47, pp. 223-238 Dasgupta, S and C. Meisner. 2009. Climate Change and Sea Level Rise; A Review of the Scientific Evidence. Washington, World Bank. Indonesian Geological Bureau, 2008. Land Subsidence in Semarang Municipality. Pusat Lingkungan Geologi, Bandung. IPCC Intergovernmental Panel on Climate Change. 2001. Climate Change; The Scientific Basis. Cambridge University Press, UK. IPCC Intergovernmental Panel on Climate Change . 2007. Climate Change 2007: The Physical Science Basis, Summary for Policymakers. Cambridge University Press, UK. IPCC Intergovernmental Panel on Climate Change . 2007. Climate Change; Synthesis Report. Cambridge University Press, UK. Kuehn, F, A. Hoffman-Rothe, D. Albiol, G. Cooksley, J. Duro, J. Granda, S. Haas and D. Murdohardono. 2009. Detection of Land Subsidence in SemarangIndonesia Using Persistent Scatterer Interferometry. Semarang, Indonesia. Levitus, S., J.I. Antonov, and T.P. Boyer. 2005. Warming of the World Ocean, 1955-2003. Geophysical Research Letter Vol. 32. Marsudi. 2004. Prediksi Laju Amblesan Tanah di Daratan Aluvial Semarang Propinsi Jawa Tengah. Doctoral Dissertation, ITB, Bandung. Merritts, D., DeWet, A. Menking, K. 1998. Environmental Geology: An Earth System Science Approach. W. H. Freeman and Company, New York. NASA retrieved on January 3, 2012. http:science.nasa.govscience- newsscience -at-nasa200226feb_bigmoonshine Nicholls, R. J., N. Marinova, J. A. Lowe, S. Brown, P. Vellinga, D. de Gusmao, J. Hinkel, R. S. J. Tol. 2011. Sea-level rise and its possible impacts given a ‘beyond 4°C world in the twenty-first century. Journal of Phylosophical Transactions of The Royal Society, 369: 161-181. Peltier, W.R. 1999. Global Sea Level Rise And Glacial Isostatic Adjusment. Journal of Global and Planetary Change 20: 93-123 Plag, H.P. 2006. Recent Relative Sea-Level Trends: An Attempt To Quantify The Forcing Factors. The Royal Society Publising vol. 364, pp. 821-844. Prameswari, F.W. 2007. Studi perubahan ketinggian dan genangan rob di pesisir kecamatan saying kabupaten Demak. Undip, Semarang Skripsi Ross, A. 1997. Tides and Tidal Currents. IHE Institute for Water Education, Delft. Sawicki, Mikolaj. 2005. Myths About Gravity and Tides. John A. Logan College, USA Schlesinger, W. H. 1991. Biogeochemistry: An Analysis of Global Change. Academic Press, Inc., New York, NY. Smith, K and Ward R. 1998. Floods: Physical Processes and Human Impacts. John Wiley and Sons, Chichester, USA. Sodr, Bagir. 2011. Pemodelan spasial dampak kenaikan muka laut terhadap penggenangan lahan pada tahun 2020 dan 2030 di pesisir kabupaten pekalongan, Jawa Tengah. Undip, Semarang Skripsi Sofian, Ibnu. 2007. Simulation Of Java Sea using an Oceanic General Circulation Model, J. Geomatika, Vol. 13 No. 2, 1-14. Bogor USGS United States Geological Survey. 2000. Land Subsidence in the United States. Virginia, USA. Vellinga, M., and R.A. Wood. 2001. Global Climatic Impacts of A Collapse of The Atlantic Thermohaline Circulation. Berkshire, United Kingdom Wahr, J. 1995. Global Earth Physics, A Handbook of Physical Constants. AGU Reference Shelf, Colorado. Widyastuti, Rahma. 2010. Pemodelan Pola Arus Laut Permukaan di Perairan Indonesia dengan Menggunakan Data Satelit Altimetri Jason-1. ITS- Surabaya Skripsi Wirasatria, A. 2005. Kenaikan muka laut sebagai landasan penanggulangan rob di pesisir kota semarang. Undip, Semarang World Bank retrieved on December 15, 2011. http:siteresources.worldbank. org DATASTATISTICSResourcestable3_13.pdf. Yanagi, T and T. Akaki. 1994. Sea Level Variation in Eastern Asia, Journal of Oceanography vol 50 pp 643 to 651. Japan APPENDICES Appendix 1. 1. List of countries by CO 2 emissions from World Bank Countries with the highest CO 2 Emissions Country CO2 Emissions per year 10 6 tons in 2006 Percentage of global total Avg. emissions per Km 2 of its land Tons China 6,103 21.5 636 United States 5.752 20.2 597 Russia 1,564 5.5 91 India 1,510 5.3 459 Japan 1,293 4.6 3421 Germany 805 2.8 2254 United Kingdom 568 2.0 2338 Canada 544 1.9 54 South Korea 475 1.7 4758 Italy 474 1.7 1573 2. Most polluted city by particulate matter from World Bank Particulate matter, gm 3 City 168 Cairo, Egypt 150 Delhi, India 128 Kolkata, India 125 Tianjin, China 123 Chongqing, China 109 Kanpur, India 109 Lucknow, India 104 Jakarta, Indonesia 101 Shenyang, China