We introduce a rapid and robust, energy-duration procedure, based on the Haskell, extendedsource
model, to obtain an earthquake moment and a moment magnitude, MED. Using seismograms
at teleseismic distances (30!–90!), this procedure combines radiated seismic energy
measures on the P to S interval of broadband signals and source duration measures on highfrequency,
P-wave signals. The MED energy-duration magnitude is scaled to correspond to the
Global Centroid-Moment Tensor (CMT) moment-magnitude, MCMT
w , and can be calculated
within about 20 min or less after origin time (OT). The measured energy and duration values
also provide the energy-to-moment ratio, !, used for identification of tsunami earthquakes.
The MED magnitudes for a set of recent, large earthquakes match closely MCMT
w , even for the
largest, great earthquakes; these results imply that the MED measure is accurate and does not
saturate. After the 2004 December 26 Sumatra-Andaman mega-thrust earthquake, magnitude
estimates available within 1 hr of OT ranged from M = 8.0 to 8.5, the CMT magnitude, available
about 3 hr after OT, was MCMT
w = 9.0, and, several months after the event, Mw = 9.1–9.3
was obtained from analysis of the earth normal modes. The energy-duration magnitude for
this event is MED = 9.2, a measure that is potentially available within 20 min after OT. After
the 2006 July 17, Java earthquake, the magnitude was evaluated at M = 7.2 at 17 min after
OT, the CMT magnitude, available about 1 hr after OT, was MCMT
w = 7.7; the energy-duration
results for this event give MED = 7.8, with a very long source duration of about 160 s, and a
very low ! value, indicating a possible tsunami earthquake
