The Methane Diurnal Variation and Microseepage Flux at Gale Crater, Mars as Constrained by the ExoMars Trace Gas Orbiter and Curiosity Observations
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Authors
Moores, John
King, Penelope
Smith, Christina L.
Martinez, German M.
Newman, Claire E.
Guzewich, Scott D.
Meslin, Pierre‐Yves
Webster, Christopher R.
Mahaffy, Paul R.
Atreya, Sushil K.
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American Geophysical Union
Abstract
The upper bound of 50 parts per trillion by volume for Mars methane above 5 km established
by the ExoMars Trace Gas Orbiter, substantially lower than the 410 parts per trillion by volume average
measured overnight by the Curiosity Rover, places a strong constraint on the daytime methane flux at the
Gale crater. We propose that these measurements may be largely reconciled by the inhibition of mixing near
the surface overnight, whereby methane emitted from the subsurface accumulates within meters of the
surface before being mixed below detection limits at dawn. A model of this scenario allows the first precise
calculation of microseepage fluxes at Gale to be derived, consistent with a constant 1.5 × 10−10 kg·m−2
·sol−1
(5.4 × 10−5 tonnes·km−2
·year−1
) source at depth. Under this scenario, only 2.7 × 104 km2 of Mars's surface
may be emitting methane, unless a fast destruction mechanism exists.
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Geophysical Research Letters
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