Land subsidence characteristics of Jakarta between 1997 and 2005, as estimated using GPS surveys

Abidin, Hasanuddin Z.; Andreas, Heri; Djaja, Rochman; Darmawan, Dudy; Gamal, M.

doi:10.1007/s10291-007-0061-0

Cited by 145 publications

(74 citation statements)

References 6 publications

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“…Groundwater depletion can also lead to significant land subsidence, which, in extreme cases as in the San Joaquin Valley of California, has reached values of 1.2 m, impacting pipelines and transport systems. Other regions with severe subsidence include Bangkok, Thailand (Giao and Nutalaya 2006) and Jakarta, Indonesia (Abidin et al 2008), increasing flood risks.…”

Section: Introductionmentioning

confidence: 99%

Groundwater Storage Changes: Present Status from GRACE Observations

Chen

Famigliett

Scanlon

et al. 2016

Space Sciences Series of ISSI

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Satellite gravity measurements from the Gravity Recovery and Climate Experiment (GRACE) provide quantitative measurement of terrestrial water storage (TWS) changes with unprecedented accuracy. Combining GRACE-observed TWS changes and independent estimates of water change in soil and snow and surface reservoirs offers a means for estimating groundwater storage change. Since its launch in March 2002, GRACE time-variable gravity data have been successfully used to quantify long-term groundwater storage changes in different regions over the world, including northwest India, the High Plains Aquifer and the Central Valley in the USA, the North China Plain, Middle East, and southern Murray-Darling Basin in Australia, where groundwater storage has been significantly depleted in recent years (or decades). It is difficult to rely on in situ groundwater measurements for accurate quantification of large, regional-scale groundwater storage changes, especially at long timescales due to inadequate spatial and temporal coverage of in situ data and uncertainties in storage coefficients. The now nearly 13 years of GRACE gravity data provide a successful and unique complementary tool for monitoring and measuring groundwater changes on a global and regional basis. Despite the successful applications of GRACE in studying global groundwater storage change, there are still some major challenges limiting the application and interpretation of GRACE data. In this paper, we present an overview of GRACE applications in groundwater studies and discuss if and how the main challenges to using GRACE data can be addressed.

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Section: Introductionmentioning

confidence: 99%

Groundwater Storage Changes: Present Status from GRACE Observations

Chen

Famigliett

Scanlon

et al. 2016

Space Sciences Series of ISSI

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“…Land subsidence in Jakarta has been observed using several geodetic techniques and has been widely reported for many years (Rismianto and Mak, 1993;Murdohardono and Sudarsono, 1998;Purnomo et al, 1999;Rajiyowiryono, 1999;Abidin et al, 2001Abidin et al, , 2004Abidin et al, , 2008Abidin et al, , 2010Abidin et al, , 2011Abidin et al, , 2013Koudogbo et al, 2012;Ng et al, 2012;Chaussard et al, 2013). According to those studies, land subsidence in Jakarta has spatial and temporal variations with typical rates of about 3 to 10 cm year −1 .…”

Section: Introductionmentioning

confidence: 99%

On correlation between urban development, land subsidence and flooding phenomena in Jakarta

et al. 2015

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Abstract. Jakarta is the capital city of Indonesia with a population of about 10.2 million people, inhabiting an area of about 660 square-km. It is located within a deltaic plain and passes by 13 natural and artificial rivers. In the last three decades, urban development of Jakarta has grown very rapidly in the sectors of industry, trade, transportation, real estate and many others, which has caused several negative environmental impacts. In turns Jakarta is then prone toward a few natural hazards mainly land subsidence and flooding. In general, based on geodetic measurement methods (e.g. Leveling, GPS surveys, and InSAR), conducted since 1982 up to 2014, it is obtained that land subsidence in Jakarta exhibits spatial and temporal variations, with the typical rates of about 3 to 10 cm year −1 . In general, the impacts of land subsidence in Jakarta can be seen in the forms of cracking of permanent constructions and roads, changes in river canal and drain flow systems, wider expansion of coastal and/or inland flooding areas, and malfunction of drainage system. Several areas along the coast of Jakarta already have experienced tidal flooding during high tide periods. These coastal flooding usually occurs in the areas with relatively large subsidence rates. Subsidence in the areas along the rivers which are flowing throughout Jakarta will also worsen the impacts of riverine flooding. The changes in river canal and drain flow systems and malfunction of drainage system due to land subsidence will also aggravate the flooding. Land subsidence will have direct and indirect affects with the flooding in Jakarta, both in coastal or inland areas.

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“…To verify the validity of numerical modeling results, comparisons had been made with subsidence monitoring results by PSI method using SAR images for the period of year 2002-2006(Kuehn et.al, 2009) and subsidence monitoring results by GPS measurement for the period of 2008(Abidin et.al, 2010 . The inferred monitoring results and comparison tables for each time period are presented in Figure 11 and Table 2 (PSI survey) and Figure 12 and Table 3 (GPS survey).…”

Section: Verification Of Numerical Modelling Results With the Monitormentioning

confidence: 99%

“…It could occur as the result of human activities such as excessive groundwater withdrawal, load of construction etc and also due to natural geological actions. Subsidence has become a significant problem worldwide, particularly in the urban areas, such as Jakarta (Abidin et al, 2008), Shanghai (Chai et al, 2004), New Jersey (Sun et al, 1999), Bangkok (Bergado et al,1988). Besides Jakarta, land subsidence is also known to occur in Semarang and Bandung (Abidin et.al., 2006;Abidin et.al 2008 ).…”

Section: Introductionmentioning

confidence: 99%

Modelling of Land Subsidence Along Tanah Mas -Pelabuhan Section Semarang City Using Finite Element Method

Sarah¹,

Syahbana²,

Lubis³

et al. 2011

J.Ris.Geo.Tam

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Land subsidence has been an apparent problem in the northern part of Semarang city, Central Java, which has caused enormous physical and economical impacts. This area is underlain by alluvium sediments of clay, silt, sand and gravel. The nature of the alluvium soil is soft and highly compressible which induces natural consolidation to occur. The lowering of groundwater table due to exploitation and loads of building and earth fill accelerate the rate of consolidation settlement. A study of land subsidence modeling was carried out in the northern part of Semarang city. Collection and analysis of data on the geology, hydrology, soil properties and monitored settlements were conducted. Modeling of land subsidence involved stress deformation analysis using finite element method. The settlements computed for selected section of the city of Semarang were compared with measurements of settlement in the city area. The simulation results appear to be in reasonably good agreement with the measurement results. Sarah, Dwi et al

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Land subsidence characteristics of Jakarta between 1997 and 2005, as estimated using GPS surveys

Cited by 145 publications

References 6 publications

Groundwater Storage Changes: Present Status from GRACE Observations

Groundwater Storage Changes: Present Status from GRACE Observations

On correlation between urban development, land subsidence and flooding phenomena in Jakarta

Modelling of Land Subsidence Along Tanah Mas -Pelabuhan Section Semarang City Using Finite Element Method

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