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AH dkk 08 LandsubSmg

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Aplic a t ion of Ge om a t ic T e c hnology for La nd-subside nc e M a pping of Se m a ra ng Coa st a l Cit y

Abst ra c t

Several natural phenomena especially at coastal zone that later become natural disaster in our daily life, among others are flooding, high water-tide flood (known locally as “rob”), land slide, mount eruption, tsunami waves and specific natural phenomena that happened at Semarang coastal city was subsidence. Aims of the research are field measurement of actual land-subsidence, by means of land height differences by time and built a spatial plot and data base. Field measurement was done with measurement of land height differences by means of land-height differences based 60 Geodetic Land Height positions set by Indonesian Bireau of Land Mapping (Titik Tinggi Geodesi -Bakosurtanal) and private Bench Mark (BM) at Semarang, with its geodetic positions by GPS (Global Positioning System).

Both field and geodetic data collected was then transformed into a numeric series of data to be processed for geostatistic known as Kriging method become a raster layer data, that later used for spatial analysis using ER_Mapper 6.4 (Licensed user) and Arc_GIS software. Geodetic datum used was WGS84 on UTM map projection. Beside the field data that transformed into a arster layer data, a Spaceshuttle Radar for Terrain Model (SRTM) data for contur and 3 dimention analysis and a Landsat_ETM satellite data was also used as value added to the data (metadata).

Based on the analysis of field data measurement and spatial plot revealed that the rate of land-subsidence at Semarang coastal city ranged from 1 – 9 cm/year, widely distributed throughout the city, espescialy at the most densed populated zone. Therefore a remapping and re-evaluation of the City Spatial Planning and Regulations was inevitable.

Key words : land-subsidence, coastal zone,Semarang

*)Centre of Spatial Database

Fisheries and Marine Geomatic. Diponegoro University. Semarang e-mail : [email protected]

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