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A successful prediction of the record CO(2) rise associated with the 2015/2016 El Niño

In early 2016, we predicted that the annual rise in carbon dioxide concentration at Mauna Loa would be the largest on record. Our forecast used a statistical relationship between observed and forecast sea surface temperatures in the Niño 3.4 region and the annual CO(2) rise. Here, we provide a forma...

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Autores principales: Betts, Richard A., Jones, Chris D., Knight, Jeff. R., Keeling, Ralph. F., Kennedy, John. J., Wiltshire, Andrew J., Andrew, Robbie M., Aragão, Luiz E. O. C.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: The Royal Society 2018
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6178439/
https://www.ncbi.nlm.nih.gov/pubmed/30297462
http://dx.doi.org/10.1098/rstb.2017.0301
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author Betts, Richard A.
Jones, Chris D.
Knight, Jeff. R.
Keeling, Ralph. F.
Kennedy, John. J.
Wiltshire, Andrew J.
Andrew, Robbie M.
Aragão, Luiz E. O. C.
author_facet Betts, Richard A.
Jones, Chris D.
Knight, Jeff. R.
Keeling, Ralph. F.
Kennedy, John. J.
Wiltshire, Andrew J.
Andrew, Robbie M.
Aragão, Luiz E. O. C.
author_sort Betts, Richard A.
collection PubMed
description In early 2016, we predicted that the annual rise in carbon dioxide concentration at Mauna Loa would be the largest on record. Our forecast used a statistical relationship between observed and forecast sea surface temperatures in the Niño 3.4 region and the annual CO(2) rise. Here, we provide a formal verification of that forecast. The observed rise of 3.4 ppm relative to 2015 was within the forecast range of 3.15 ± 0.53 ppm, so the prediction was successful. A global terrestrial biosphere model supports the expectation that the El Niño weakened the tropical land carbon sink. We estimate that the El Niño contributed approximately 25% to the record rise in CO(2), with 75% due to anthropogenic emissions. The 2015/2016 CO(2) rise was greater than that following the previous large El Niño in 1997/1998, because anthropogenic emissions had increased. We had also correctly predicted that 2016 would be the first year with monthly mean CO(2) above 400 ppm all year round. We now estimate that atmospheric CO(2) at Mauna Loa would have remained above 400 ppm all year round in 2016 even if the El Niño had not occurred, contrary to our previous expectations based on a simple extrapolation of previous trends. This article is part of a discussion meeting issue ‘The impact of the 2015/2016 El Niño on the terrestrial tropical carbon cycle: patterns, mechanisms and implications’.
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spelling pubmed-61784392018-10-22 A successful prediction of the record CO(2) rise associated with the 2015/2016 El Niño Betts, Richard A. Jones, Chris D. Knight, Jeff. R. Keeling, Ralph. F. Kennedy, John. J. Wiltshire, Andrew J. Andrew, Robbie M. Aragão, Luiz E. O. C. Philos Trans R Soc Lond B Biol Sci Articles In early 2016, we predicted that the annual rise in carbon dioxide concentration at Mauna Loa would be the largest on record. Our forecast used a statistical relationship between observed and forecast sea surface temperatures in the Niño 3.4 region and the annual CO(2) rise. Here, we provide a formal verification of that forecast. The observed rise of 3.4 ppm relative to 2015 was within the forecast range of 3.15 ± 0.53 ppm, so the prediction was successful. A global terrestrial biosphere model supports the expectation that the El Niño weakened the tropical land carbon sink. We estimate that the El Niño contributed approximately 25% to the record rise in CO(2), with 75% due to anthropogenic emissions. The 2015/2016 CO(2) rise was greater than that following the previous large El Niño in 1997/1998, because anthropogenic emissions had increased. We had also correctly predicted that 2016 would be the first year with monthly mean CO(2) above 400 ppm all year round. We now estimate that atmospheric CO(2) at Mauna Loa would have remained above 400 ppm all year round in 2016 even if the El Niño had not occurred, contrary to our previous expectations based on a simple extrapolation of previous trends. This article is part of a discussion meeting issue ‘The impact of the 2015/2016 El Niño on the terrestrial tropical carbon cycle: patterns, mechanisms and implications’. The Royal Society 2018-11-19 2018-10-08 /pmc/articles/PMC6178439/ /pubmed/30297462 http://dx.doi.org/10.1098/rstb.2017.0301 Text en © 2018 The Authors. http://creativecommons.org/licenses/by/4.0/ Published by the Royal Society under the terms of the Creative Commons Attribution License http://creativecommons.org/licenses/by/4.0/, which permits unrestricted use, provided the original author and source are credited.
spellingShingle Articles
Betts, Richard A.
Jones, Chris D.
Knight, Jeff. R.
Keeling, Ralph. F.
Kennedy, John. J.
Wiltshire, Andrew J.
Andrew, Robbie M.
Aragão, Luiz E. O. C.
A successful prediction of the record CO(2) rise associated with the 2015/2016 El Niño
title A successful prediction of the record CO(2) rise associated with the 2015/2016 El Niño
title_full A successful prediction of the record CO(2) rise associated with the 2015/2016 El Niño
title_fullStr A successful prediction of the record CO(2) rise associated with the 2015/2016 El Niño
title_full_unstemmed A successful prediction of the record CO(2) rise associated with the 2015/2016 El Niño
title_short A successful prediction of the record CO(2) rise associated with the 2015/2016 El Niño
title_sort successful prediction of the record co(2) rise associated with the 2015/2016 el niño
topic Articles
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6178439/
https://www.ncbi.nlm.nih.gov/pubmed/30297462
http://dx.doi.org/10.1098/rstb.2017.0301
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