# Atmospheric CO2 response to volcanic eruptions

Author(s) Frölicher, Thomas L., Joos, Fortunat, Raible, Christoph C., Sarmiento, Jorge L.
Publication Type Journal Items, Publication Status: Published
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## Detailed Information

Title Atmospheric CO2 response to volcanic eruptions
Subtitle The role of ENSO, season, and variability
Author(s) Frölicher, Thomas L.
Joos, Fortunat
Raible, Christoph C.
Sarmiento, Jorge L.
Journal or Series Title Global biogeochemical cycles
Volume Number 27
Issue Number 1
Start Page 239
End Page 251
ISSN 0886-6236
1944-9224
Publisher American Geophysical Union
Publication Place Washington, DC
Publication Date 2013-03
Keyword(s) Carbon cycle
Modeling
Volcanoes
Abstract [1] Tropical explosive volcanism is one of the most important natural factors that significantly impact the climate system and the carbon cycle on annual to multi-decadal time scales. The three largest explosive eruptions in the last 50 years—Agung, El Chichón, and Pinatubo—occurred in spring/summer in conjunction with El Niño events and left distinct negative signals in the observational temperature and CO2 records. However, confounding factors such as seasonal variability and El Niño-Southern Oscillation (ENSO) may obscure the forcing-response relationship. We determine for the first time the extent to which initial conditions, i.e., season and phase of the ENSO, and internal variability influence the coupled climate and carbon cycle response to volcanic forcing and how this affects estimates of the terrestrial and oceanic carbon sinks. Ensemble simulations with the Earth System Model (Climate System Model 1.4-carbon) predict that the atmospheric CO2 response is ˜60% larger when a volcanic eruption occurs during El Niño and in winter than during La Niña conditions. Our simulations suggest that the Pinatubo eruption contributed 11 ± 6% to the 25 Pg terrestrial carbon sink inferred over the decade 1990–1999 and −2 ± 1% to the 22 Pg oceanic carbon sink. In contrast to recent claims, trends in the airborne fraction of anthropogenic carbon cannot be detected when accounting for the decadal-scale influence of explosive volcanism and related uncertainties. Our results highlight the importance of considering the role of natural variability in the carbon cycle for interpretation of observations and for data-model intercomparison.
DOI 10.1002/gbc.20028
Additional Notes Published online by: Wiley
Received 5 July 2012, Revised 10 December 2012, Accepted 27 January 2013, Published online 27 March 2013
Document Type Article
Publication Status Published
Language English
Assigned Organisational Unit(s) 03731
Organisational Unit(s)
NEBIS System Number 000041178
Source Database ID FORM-1384957210
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@article{Frlchr2013,
author = "Fr{\"{o}}licher, Thomas L. and Joos, Fortunat and Raible, Christoph C. and Sarmiento, Jorge L.",
title = "{A}tmospheric {C}{O}2 response to volcanic eruptions: {T}he role of {E}{N}{S}{O}, season, and variability",
journal = "Global biogeochemical cycles",
year = 2013,
volume = "27",
number = "1",
pages = "239--251",
month = mar,
}


E-Citations record created: Wed, 20 Nov 2013, 14:20:13 CET