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DTSTAMP:20220812T074334Z
LOCATION:Singapore Room
DTSTART;TZID=Europe/Stockholm:20220628T110000
DTEND;TZID=Europe/Stockholm:20220628T113000
UID:submissions.pasc-conference.org_PASC22_sess148_msa239@linklings.com
SUMMARY:How on Earth Would a Moonquake Sound?
DESCRIPTION:Minisymposium\n\nHow on Earth Would a Moonquake Sound?\n\nPete
 r, Yang\n\nProbing the interior of our planet through seismic observations
  has led to many great insights and knowledge about internal structures an
 d processes. It has been such a successful endeavor, that seismic investig
 ations not only were carried out on Earth, but have been extended on to ot
 her planetary bodies such as Moon, Venus and most recently Mars. Regarding
  the Apollo missions to Moon, an essential scientific mission was to study
  the interior of Earth's only natural satellite by seismics. To that end, 
 several Apollo missions placed seismometers onto Moon's surface, listening
  to the interior rumblings of the celestial body. Today's knowledge about 
 its interior is mostly due those few missions and seismic recordings sent 
 back to Earth. Investigating these seismic recordings however remains a fa
 scinating and challenging undertake. Moonquakes exhibit very distinct grou
 nd shaking compared to earthquake signals, mostly due to strong scattering
  and weak attenuation regimes. In this talk, we will outline current attem
 pts to model seismic wave propagation for Moon and will provide an audible
  experience of a meteoroid impact recorded by the Apollo seismometers, hig
 hlighting the current state (and failure) of these computational efforts.\
 n\nDomain: Climate, Weather and Earth Sciences, Computer Science and Appli
 ed Mathematics, Physics
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