Please use this identifier to cite or link to this item: http://hdl.handle.net/20.500.12666/1047
Title: Background levels of methane in Mars’ atmosphere show strong seasonal variations
Authors: Webster, Christopher R.
Mahaffy, Paul R.
Atreya, Sushil K.
Moores, John E.
Flesch, Gregory J.
Malespin, Charles A.
McKay, Christopher P.
Martínez, Germán M.
Smith, Christina L.
Martín Torres, Javier
Gómez Elvira, J.
Paz Zorzano, M.
Wong, Michael H.
Trainer, Melissa G.
Steele, Andrew
Archer, Doug
Sutter, Brad
Coll, Patrice J.
Freissinet, Caroline
Meslin, Pierre-Yves
Gough, Raina V.
House, Christopher H.
Pavlov, Alexander
Eigenbrode, Jennifer L.
Glavin, Daniel P.
Pearson, John C.
Keymeulen, Didier
Christensen, Lance E.
Schwenzer, Susanne P.
Navarro González, R.
Pla García, J.
Rafkin, Scot C. R.
Vicente Retortillo, Álvaro
Kahanpää, H.
Viúdez Moreiras, Daniel
Smith, Michael D.
Harri, Ari-Matti
Genzer, María
Hassler, Donald M.
Lemmon, M. T.
Crisp, Joy
Sander, Stanley P.
Zurek, Richard W.
Vasavada, Ashwin R.
Issue Date: 8-Jun-2018
Publisher: Science
DOI: 10.1126/science.aaq0131
Published version: https://www.science.org/doi/10.1126/science.aaq0131
Citation: Science 360(6393): 1093-1096(2018)
Abstract: Variable levels of methane in the martian atmosphere have eluded explanation partly because the measurements are not repeatable in time or location. We report in situ measurements at Gale crater made over a 5-year period by the Tunable Laser Spectrometer on the Curiosity rover. The background levels of methane have a mean value 0.41 ± 0.16 parts per billion by volume (ppbv) (95% confidence interval) and exhibit a strong, repeatable seasonal variation (0.24 to 0.65 ppbv). This variation is greater than that predicted from either ultraviolet degradation of impact-delivered organics on the surface or from the annual surface pressure cycle. The large seasonal variation in the background and occurrences of higher temporary spikes (~7 ppbv) are consistent with small localized sources of methane released from martian surface or subsurface reservoirs.
URI: http://hdl.handle.net/20.500.12666/1047
E-ISSN: 1095-9203
ISSN: 0036-8075
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