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In the past decade, a new generation of geophysical instruments and data-processing methods has expanded the spectrum of what is audible, from true earthquakes, which last seconds or minutes, to slow-slip events, which last days, to low-frequency tremor episodes, which last weeks or months.
He is a researcher of geophysical instruments.
The considerable distance between the Descartes site and previous Apollo landing sites would be beneficial for the network of geophysical instruments, portions of which were deployed on each Apollo expedition beginning with Apollo 12.
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From 2008 to present, he has been a researcher with the China University of Geosciences, where he works on geophysical instrument development.
Measurements of recent swarm activity have been possible after the installation of modern geophysical instruments, with swarm events measured in 2001, 2006, 2008 2009, 2013, and 2015 (e.g., Harada et al. 2013; Itadera et al. 2015).
This expansion of capacity enabled us to increase the payload mass of the lander to deploy geophysical instruments and to land on a wider region on the Moon including polar regions.
The time sequence of the 2015 eruption of Hakone volcano was well observed by geophysical instruments installed around the eruption center; however, its relationship with surface volcanic phenomena is not well known because of very poor visibility.
Tremors are therefore common in this region, but the November 14th event was the largest since 1929 and the first of this magnitude to be monitored with modern geophysical instruments.
This would mean the ash would not only affect geophysical instruments powered by PV-modules in the near field of the volcano, but also industrial and private instruments in the mid and far field.
The Polaris geophysical project emplaced geophysical instruments in several locations in Canada (Bastow et al. 2015) including the east shore of Hudson Bay and southward, as the Hudson Bay Lithospheric Experiment (HuBLE).
However, no signals associated with the ash fall or fluid discharge was observed by geophysical instruments.
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