Demo · Cikarang, Indonesia · live archive, null result

Eight data centers, two years, nothing moving

Cikarang, east of Jakarta, holds most of Indonesia's new data center capacity, on the same alluvial plain that has made North Jakarta one of the fastest sinking cities on record. We measured the ground under eight data centers from the free Sentinel-1 radar archive: 61 satellite passes between September 2024 and September 2026, 119 interferograms, sampled at building coordinates taken from PeeringDB and OpenStreetMap.

Every one of them is flat to within our own measurement noise. Find your site in the table below. The full working, including a mistake we made and corrected in public, is further down the page.

–Data center sites at verified coordinates
–Range of line of sight rates across all of them
–Satellite passes in the stack
6.2 kmFrom the moving ground to the nearest data hall

Results by site

Rate of line of sight movement over the two years, from the median of the radar pixels within 400 m of each coordinate. The ± is one standard error, and a site reads as flat when its rate sits inside about two of them. Click a row to pick it out on the chart.

Data centerEstateRate, mm/yrPixelsCoordinate from

Estate reference points

One point per industrial estate, sampled in our first pass. They are points on the ground, not buildings, and not a verdict on a whole estate.

PointNoteRate, mm/yrPixels

The measurement

Median line of sight displacement inside 400 m of each data center, one point per satellite pass, relative to a reference strip south of the estates. Down means moving away from the satellite. Click a name to hide it.

Line of sight velocity map of the Cikarang area with eight verified data center sites marked and the first-pass estate point circled

Where everything sits

Line of sight velocity across the scene, red moving away from the satellite. The small circles are the verified data centers: DCI H1 in MM2100 to the west, EdgeConneX JKT01 in the middle, and six more in the GIIC cluster at Kota Deltamas to the south. The orange circle is the estate point we first sampled, on the southern flank of the subsiding area that covers the north east of the scene. That area looks like regional groundwater drawdown, not load from anything built on top of it.

What a null result is worth

Reading this the way an operator would

Nothing here clears its own error bar, and that is the finding. Free radar over two years puts the ground under all eight halls inside a few mm/yr of each other and of zero. An operator who was about to commission a ground survey on a hunch now has an ordering: none of these eight, and a subsiding area 6 km north east that would matter a great deal to anyone building in it.

What it is not is a certificate. Free radar over two years can tell flat ground from moving ground, but on tropical ground it cannot give an exact rate. When we checked our own rates against GNSS stations on tropical ground in Puerto Rico over six months, they were off by 54 mm/yr RMS, which spread across two years is still of order 20 mm/yr on an absolute rate. Nothing in the table clears that bar either, which is why this reads as a null and not as eight precise measurements.

The full research note, with every caveat and the method →

–MM2100 against Kota Deltamas, 12.2 km apart, two years
–Typical single-site scatter, one pass to the next
–Same scatter after differencing two neighbours in GIIC
119Interferograms, all of them usable
The correction · why coordinates come first

An estate centroid is not a building

The first version of this study sampled one point per industrial estate. The point for Kota Jababeka, an estate of about 5,600 hectares, read 23 mm/yr faster sinking than its neighbours, and we named the estate's data center tenant beside the number. That point sits 6.2 km from the nearest verified data hall, on the flank of a regional subsidence area. The ground at that point is moving, and no data center is on it. How much of that area falls inside the estate boundary is something we cannot see from outside.

The middle button on the chart puts that series back. It is the same pipeline, the same stack and the same inversion, sampled 6 km away, and it is a 23 mm/yr difference in the headline. That is why every study now starts from the coordinate of the building.

Your Asset · Live Archive Check

Now point it at your own.

Search for your site or click it on the map. This checks the real satellite record over that exact spot: the passes, the orbit, the freshness. Give it the coordinate of the building, not the name of the park.

Have a site like this?

We can point this at yours.

The same pipeline runs over a data center campus, a tailings dam, a slope, a reclamation site or a port. Name two sites and we will run the free archive over them at no cost, and send you the same record as this page.

Demo note. Every number and every line on this page is our own processing result, built from raw Sentinel-1 radar through the pipeline that runs our monitoring. Site coordinates come from PeeringDB and OpenStreetMap and are listed with their sources in the result file. Contains modified Copernicus Sentinel data 2024 to 2026, processed by ASF HyP3.

Disclaimer. Rheality provides decision-support monitoring data, not a safety guarantee. The duty of care for any asset remains with its owner and their engineer. See Terms & Disclaimer.