CTBTO's Initial Findings on the DPRK's 2009 announced nuclear test
23 primary and 16 auxiliary seismic stations registered the event on 25 May 2009.
Higher magnitude than in 2006
Only after further analysis at the International Data Centre in Vienna, using data from the 16 auxiliary seismic stations that recorded the event as well, will it be possible to confirm that the signal was manmade and not an earthquake.
Comparison of the initial estimations of the origin of the 2006 and the 2009 announced DPRK nuclear tests.
Nuclear character yet to be established
On-site inspection would be possible If the CTBT were in force, an on-site inspection could be dispatched to corroborate the findings and present them to its Member States to pronounce the final verdict. An on-site-inspection will only be possible after the CTBT has entered into force. However, the initial seismic findings of today’s event have already homed in on it precisely enough to request an on-site inspection under the Treaty’s rules. These foresee that an area for an on-site inspection must be no larger than 1,000 km². At the first stage of analyzing the available seismic data, the potential area of origin of today’s event could already be narrowed down to 860 km² - roughly the size of the city of Berlin – and will further decrease significantly in the coming days. The CTBTO has often trained its ability to conduct on-site inspections, most recently in a major exercise at the former Soviet Union nuclear test site Semipalatinsk in September 2008 during the so-called Integrated Field Exercise 2008.
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Click for animation: A method called atmospheric transport modelling is used to calculate the potential trajectory of an airborne radioactive particle - here the dispersion of the radioactive noble gas Xenon 133 after the 2006 DPRK nuclear test.
Only nine ratifications missing for entry into force
An OSI inspector prepares to search for underground cavities that could be assosiated with a nuclear test.