Possibility to detect earthquake precursors using cubesats

Since the late 80s of the past century observations from space have been intensely used to study the possibility of detecting earthquake precursors. Compared to ground observations, one obvious advantage is their global coverage. Based on previous experiments, the possible mechanisms of lithosphere-atmosphere-ionosphere coupling are discussed. Some new relations that confirm recently proposed amplification mechanisms in the atmosphere are suggested and corresponding parameters to study in future space experiments are proposed. It is concluded that given the current state of space technology, a low-cost multi-satellite mission could be realized both from scientific and technological points of view. Finally, a possible payload composition for cubesats is recommended.