Download Film Fireball 2009 Sub Indo
Ailene Goldhirsh
This frightening collision and massive explosion isn't a behind-the-scenes look of a new action film. It's the result of a crash between a passenger train and a truck stuck on a railroad crossing in Indonesia. Miraculously, there were no deaths and in fact, a local report states there was just a single injury in all of this.
The crash occurred on July 18 in the city of Semarang, the capital of Central Java between Surabaya and Jakarta. Detik.com reports a truck was stuck on a crossing when the train came along. Attempts had been made to get the truck clear, so the driver obviously wasn't in the rig at the time of the collision. However, to make a bad situation even worse, the crossing was just before the Jalen Madukoro Bridge.
A video shared on Reddit shows the truck surviving the initial impact, and by surviving, we mean not erupting into a fireball. That happens as the truck is shoved into the steel beams of the bridge, and it's quite dramatic to say the least. The train comes to a halt shortly thereafter, still apparently on the bridge though the report says the locomotive was hanging over the river.
The condition of the bridge is unknown. but it's safe to assume the truck is pretty much done for. As for the one reported injury, that person's condition is also unknown, though the injury reportedly happened after jumping from the train into the river. As of our report on July 18, a cleanup effort was underway to get the train cars cleared from the area.
This certainly isn't the first time we've seen trucks hung up on railroad crossings. In March 2023 a truck hauling an excavator in Georgia got caught on a crossing with a slight incline. The driver appeared to disconnect the trailer from the rig seconds before the impact, but it still shoved the trailer and the massive excavator to the side like they were paperweights. Something similar occurred in Tennessee in December 2021 involving a truck towing a large concrete beam. Another truck's cargo was smashed to bits in Texas last August.
On October 8, 2009 about 03:00 Greenwich time, an atmospheric fireball blast was observed and recorded over an island region of Indonesia. The blast is thought to be due to the atmospheric entry of a small asteroid about 10 meters in diameter that, due to atmospheric pressure, detonated in the atmosphere with an energy of about 50 kilotons (the equivalent of 110 million pounds of TNT explosives).
A report from Elizabeth Silber and Peter Brown at the University of Western Ontario indicates that several international very-long wavelength infrasound detectors recorded the blast and fixed the position near the coastal city of Bone in South Sulawesi, island of Sulewesi. They note that the blast was in the 10 to 50 kT range with the higher end of this range being more likely.
Assuming an estimated size of about 5-10 meters in diameter, we would expect a fireball event of this magnitude about once every 2 to 12 years on average. As a rule, the most common types of stony asteroids would not be expected to cause ground damage unless their diameters were about 25 meters in diameter or larger.
On Oct 8, 2009, media reports appeared in the local press in Indonesia concerning a loud air blast occurring near 11am local time (0300 UT). Subsequent to these first media reports, additional English language reports appeared suggesting the event was meteoritic.
Indonesian language reports more clearly identify a bright fireball, accompanied by an explosion and lingering dust cloud as the origin of the air blast. Finally, a YouTube video posted on the same day appears to show a large dust cloud consistent with a bright, daylight fireball.
Based on these initial reports, a detailed examination was made of all International Monitoring System (IMS) infrasound stations of the Comprehensive Nuclear-Test-Ban Treaty Organization (CTBTO). From this initial examination, a total of 11 stations showed probable signals from a large explosion centered near 4.5S, 120E, with an origin time near 0300 UT on Oct 8, 2009, consistent with the media reports. This signal was notable for having been (a) detected at many IMS stations, including five at ranges over 10,000 km (and one at a nearly 18,000 km range) and (b) being confined to very low frequencies. Both of these observations suggest the explosion source was of very high total energy. All signal motions were between 0.27 - 0.32 km/s, consistent with stratospheric signal returns.
The yield estimates based on infrasonic amplitude are very uncertain in this instance as the propagation distances are much larger than is typical and outside the range limits where such relations have been developed (e.g. Edwards et al, 2006) and hence the period relationship (which was generated using a dataset of nuclear explosions having yields in this range) is more applicable.
Based on these infrasound records, it appears that a large (40-50 kT TNT) bolide detonation occurred near 0300 UT on Oct 8, 2009 near the coastal city of Bone in South Sulawesi, Indonesia. The infrasonic geolocation is not precise enough to determine if the bolide was over water or land, but it was relatively near the coast.
Using an average impact velocity for NEAs of 20.3 km/s, the energy limits (10 - 70 kT) suggested by this analysis correspond to an object 5-10 m in diameter. Based on the flux rate from Brown et al (2002), such objects are expected to impact the Earth on average every 2 - 12 years.
ReVelle D.O. 1997. Historical Detection of Atmospheric Impacts by Large Bolides using Acoustic-Gravity Waves, Annals of the New York Academy of Sciences, Near-Earth Objects - The United Nations International Conference, editor J.L. Remo, New York Academy of Sciences, 822, 284-302.
In each of the following the infrasound signals across each station have been array processed in windows (typically of 30-60 second length) to search for coherent signals with consistent back-azimuth measurements. The top panel in each display is the F-statistic, a measure of the relative coherency of the signal across the array elements in any particular window (essentially a SNR measure). The second window shows the apparent trace velocity of the acoustic signal across the array in the direction of the peak F-stat. Similarly, the third plot shows the best estimate for the signal back-azimuth in the direction of maximum F-stat for each window. The fourth plot shows the raw pressure signal for one array element bandpassed according to the chosen Low - High frequency combination, shown in the boxes of the lower plot.
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