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Response to Comment on “Contrasting carbon cycle responses of the tropical continents to the 2015–2016 El Niño”
Liu, J.; Bowman, K.W.; Schimel, D.S.; Parazoo, N.C.; Jiang, Z.; Lee, M.; Bloom, A.A.; Wunch, D.; Frankenberg, C.; Sun, Y.; O’Dell, C.W.; Gurney, K.R.; Menemenlis, D.; Gierach, M.; Crisp, D.; Eldering, A. (2018). Response to Comment on “Contrasting carbon cycle responses of the tropical continents to the 2015–2016 El Niño”. Science (Wash.) 362(6418): eaat1211. https://dx.doi.org/10.1126/science.aat1211
In: Science (Washington). American Association for the Advancement of Science: New York, N.Y. ISSN 0036-8075; e-ISSN 1095-9203, more
Peer reviewed article  

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Authors  Top 
  • Liu, J.
  • Bowman, K.W.
  • Schimel, D.S.
  • Parazoo, N.C.
  • Jiang, Z.
  • Lee, M.
  • Bloom, A.A.
  • Wunch, D.
  • Frankenberg, C.
  • Sun, Y.
  • O’Dell, C.W.
  • Gurney, K.R.
  • Menemenlis, D.
  • Gierach, M.
  • Crisp, D.
  • Eldering, A.

Abstract
    Chevallier showed a column CO2 (XCO2) anomaly of ±0.5 parts per million forced by a uniform net biosphere exchange (NBE) anomaly of 2.5 gigatonnes of carbon over the tropical continents within a year, so he claimed that the inferred NBE uncertainties should be larger than presented in Liu et al. We show that a much concentrated NBE anomaly led to much larger XCO2 perturbations.

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