Atmospheric lifetime of fossil-fuel carbon dioxide
By D. Archer, M. Eby, V. Brovkin, A. Ridgwell, Long Cao, Uwe Mikolajewicz, K. Caldeira, Katsumi Matsumoto, G. Munhoven, Á. Montenegro and 1 more. 2009
856 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change, Renewable Energy, Sustainability and the Environment
View Paper: https://www.semanticscholar.org/paper/4e7e8ab4bb2da459b55dbf38ce991c858b063246
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Atmospheric Science
- J. Hansen
- A. Ridgwell
- G. Tselioudis
- Columbia Univ. Earth Institute
- L. Nazarenko
- F. Joos
- Malte Meinshausen
- Andrew A. Lacis
In Global and Planetary Change
- J. Hansen
- A. Ridgwell
- D. P. Vuuren
- Joeri Rogelj
- G. Tselioudis
- Keywan Riahi
- Columbia Univ. Earth Institute
- T. Kleinen
In Renewable Energy, Sustainability and the Environment
- Joeri Rogelj
- D. P. Vuuren
- Malte Meinshausen
- Katsumasa Tanaka
- N. Edwards
- Keywan Riahi
- David A. Weisbach
- G. P. Peters
Citations in the corpus
- The Geological Record of Ocean Acidification (2011, background): “(82), a simple terrestrial weathering feedback is implemented in GENIE.”
- An overview of the Earth system science of solar geoengineering (2016, background): “Even slowly phasing out solar geoengineering would mean that the warming that had been offset by solar geoengineering would occur as a substantial fraction of emitted CO2 will remain in the atmosphere on a timescale of millennia.(113,114) This has led to suggestions that solar geoengineering be used”
- Global warming in the pipeline (2022, background): “If human emissions ceased, atmospheric CO 2 would initially decline a few ppm per year, but uptake would soon slow—it would take millennia for CO 2 to reach preindustrial levels [131].”
- Climate Impacts on Economic Growth as Drivers of Uncertainty in the Social Cost of Carbon (2014, positive): “Atmospheric CO2 perturbations in DICE disappear within centuries while larger models show them persisting on the order of 10,000 years (Archer et al, 2009; Glotter et al, 2013).”
- Ulva rigida in the future ocean: potential for carbon capture, bioremediation and biomethane production (2018, background): “To meet the Paris Agreement goal of maintaining the global temperature rise to below 2 °C above preindustrial levels (Schreurs, 2016) will necessitate a reduction in CO2 emissions and a sweeping programme of CO2 capture and storage (Archer et al., 2009).”
- Emission pathways consistent with a 2[thinsp][deg]C global temperature limit (2011, background): “because a significant fraction of CO 2 emissions, the dominant anthropogenic GHG, is removed very slowly from the atmospher”
- Carbon dioxide and climate impulse response functions for the computation of greenhouse gas metrics:a multi-model analysis (2012, positive): “This evolution is consistent with earlier model results (Maier-Reimer and Hasselmann, 1987; Cao et al., 2009; Siegenthaler and Joos, 1992; Sarmiento et al., 1992; Enting et al., 1994; Archer et al., 2009; Eby et al., 2009).”