Published November 30, 2018
| public
Journal Article
Response to Comment on "Contrasting carbon cycle responses of the tropical continents to the 2015–2016 El Niño"
Chicago
Abstract
Chevallier showed a column CO_2 (X_CO_2) 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 X_(CO_2) perturbations.
Additional Information
© 2018 American Association for the Advancement of Science. This is an article distributed under the terms of the Science Journals Default License. Received 8 February 2018; accepted 4 October 2018. This research was carried out at the Jet Propulsion Laboratory, California Institute of Technology, under a contract with NASA. This work was in part supported by NASA Carbon Monitoring System program grant 14-CMS14-0054 and by NASA Orbiting Carbon Observatory Science team program grants 14-OCO2_14-0007 and 11-OCO211-0024. K.R.G. was supported by NSF CAREER award 0846358.Additional details
- Eprint ID
- 91412
- Resolver ID
- CaltechAUTHORS:20181204-065852692
- NASA/JPL/Caltech
- NASA
- 14-CMS14-0054
- NASA
- 14-OCO2_14-0007
- NASA
- 11-OCO211-0024
- NSF
- AGS-0846358
- Created
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2018-12-04Created from EPrint's datestamp field
- Updated
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2023-06-01Created from EPrint's last_modified field
- Caltech groups
- Division of Geological and Planetary Sciences (GPS)