[ABSTRAK
Jika dilakukan observasi, bentuk permukaan bumi setiap saat selalu berubah-ubahatau mengalami deformasi. Hal ini dapat dipengaruhi oleh faktor alam, manusiaataupun gabungan dari keduanya. Beberapa perubahan bentuk ini dapatmenyebabkan bencana kalau tidak kerugian. Sehingga perlu adanya suatu metodeuntuk melakukan pengukuran dan pemetaan deformasi permukaan tanah.Pada penulisan ini dilakukan study-case pemetaan deformasi yang terjadi padaarea Bandung dan sekitarnya. Fokus dari percobaan adalah mengamati lajudeformasi pertahun pada area tersebut. Teknik PSInSAR dengan kerangka kerjaStaMPS digunakan untuk mengolah data citra PALSAR satelit ALOS menjadipeta laju deformasi.Pemetaan dengan citra radar dipilih karena kemampuan akuisisi citranya yangdapat digunakan pada hampir semua kondisi. Sinyal sensor SAR dapat menembusawan sehingga dapat mengatasi kesulitan dalam menganalisis kawasan yangdiselimuti awan, seperti Bandung. Sensor ini juga dapat bekerja siang-malam,karena sensor bekerja secara aktif dalam memancarkan dan menangkap sinyalnya.Ketelitian hingga ukuran mm per tahun dapat diperoleh dengan menggunakanteknik SAR persistent scatterrer interferometry. Selain itu dengan melakukananalisis ampitudo dan fase pada beberapa interferogram menggunakan kerangkakerja StaMPS, pengukuran juga dapat dilakukan walaupun pada area yangberkoherensi rendah. Misalnya sebagian besar area terselimuti oleh vegetasiataupun keadaan atmosfir yang menyelimuti, seperti kawasan Bandung dansekitarnya.Dari hasil pemetaan dapat diamati bahwa terjadi penurunan permukaan tanah padahampir seluruh kawasan perkotaan Bandung. Penyusutan dengan nilai tertinggiterjadi pada daerah Cimahi dan Bojong sebesar 13.5 cm per tahun. Didugapenurunan muka tanah pada area perkotaan Bandung diakibatkan oleh pemakaianair tanah yang berlebih terutama pada kawasan industri.

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ABSTRACT
If the observation is made, it is observable that earth surface is always changing orconstantly undergo a deformation. This can be caused by natural factors, human,or a combination of both. Some of these deformation can lead to disaster if notlosses. Because of that, it important to have method to measure and ultimatelymap the ground surface deformation.In this study-case, the map of deformation that occurs in Bandung and itsurrounding areas was made. The focus of the experiment was to observe thedeformation rate per year in these areas. PSInSAR technique with StaMPSframework was used to processed PALSAR images of ALOS satellite.Mapping with radar images was chosen because of radar imaging system have thecapabilities to operate at almost any condition. SAR sensor signal can penetrateclouds this can be used to overcome the difficulties in analyzing the cloudy areas,such as Bandung. This sensor can also work day and night, because it is activesensor, it emit and recieve it's own signal.Using the SAR persistent scatterrer interferometry technique, measurementaccuracy up to mm per year can be obtained. In addition, by analyzing amplitudeand phase of multiple interferograms using StaMPS framework, the measurementeven with low coherence image can be done. For example, most of the area-ofinterestis covered by vegetation or randomly high atmosphere retardation atsurrounds area, such as Bandung and it?s surrounding areas.Form the deformation map, can be observed that there was a subsidence in almostall urban areas in Bandung. The highest value of ground shrinkage occurred inCimahi and Bojong with 13.5 cm per year. Suspected, land subsidence of urbanareas in Bandung was caused by excessive use of ground water, especially in theindustrial area.;If the observation is made, it is observable that earth surface is always changing orconstantly undergo a deformation. This can be caused by natural factors, human,or a combination of both. Some of these deformation can lead to disaster if notlosses. Because of that, it important to have method to measure and ultimatelymap the ground surface deformation.In this study-case, the map of deformation that occurs in Bandung and itsurrounding areas was made. The focus of the experiment was to observe thedeformation rate per year in these areas. PSInSAR technique with StaMPSframework was used to processed PALSAR images of ALOS satellite.Mapping with radar images was chosen because of radar imaging system have thecapabilities to operate at almost any condition. SAR sensor signal can penetrateclouds this can be used to overcome the difficulties in analyzing the cloudy areas,such as Bandung. This sensor can also work day and night, because it is activesensor, it emit and recieve it's own signal.Using the SAR persistent scatterrer interferometry technique, measurementaccuracy up to mm per year can be obtained. In addition, by analyzing amplitudeand phase of multiple interferograms using StaMPS framework, the measurementeven with low coherence image can be done. For example, most of the area-ofinterestis covered by vegetation or randomly high atmosphere retardation atsurrounds area, such as Bandung and it?s surrounding areas.Form the deformation map, can be observed that there was a subsidence in almostall urban areas in Bandung. The highest value of ground shrinkage occurred inCimahi and Bojong with 13.5 cm per year. Suspected, land subsidence of urbanareas in Bandung was caused by excessive use of ground water, especially in theindustrial area., If the observation is made, it is observable that earth surface is always changing orconstantly undergo a deformation. This can be caused by natural factors, human,or a combination of both. Some of these deformation can lead to disaster if notlosses. Because of that, it important to have method to measure and ultimatelymap the ground surface deformation.In this study-case, the map of deformation that occurs in Bandung and itsurrounding areas was made. The focus of the experiment was to observe thedeformation rate per year in these areas. PSInSAR technique with StaMPSframework was used to processed PALSAR images of ALOS satellite.Mapping with radar images was chosen because of radar imaging system have thecapabilities to operate at almost any condition. SAR sensor signal can penetrateclouds this can be used to overcome the difficulties in analyzing the cloudy areas,such as Bandung. This sensor can also work day and night, because it is activesensor, it emit and recieve it's own signal.Using the SAR persistent scatterrer interferometry technique, measurementaccuracy up to mm per year can be obtained. In addition, by analyzing amplitudeand phase of multiple interferograms using StaMPS framework, the measurementeven with low coherence image can be done. For example, most of the area-ofinterestis covered by vegetation or randomly high atmosphere retardation atsurrounds area, such as Bandung and it’s surrounding areas.Form the deformation map, can be observed that there was a subsidence in almostall urban areas in Bandung. The highest value of ground shrinkage occurred inCimahi and Bojong with 13.5 cm per year. Suspected, land subsidence of urbanareas in Bandung was caused by excessive use of ground water, especially in theindustrial area.]