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Insights on global warming

Seinfeld, John H. (2011) Insights on global warming. AIChE Journal, 57 (12). pp. 3259-3284. ISSN 0001-1541. https://resolver.caltech.edu/CaltechAUTHORS:20111221-114535592

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Abstract

The global temperature increase over the last century and a half (∼ 0.8°C), and the last three decades in particular, is well outside of that which can be attributed to natural climate fluctuations. The increase of atmospheric CO_2 over this period has been conclusively demonstrated to be a result largely of fossil fuel burning. The global mean temperature change that results in response to a sustained perturbation of the Earth's energy balance after a time sufficiently long for both the atmosphere and oceans to come to thermal equilibrium is termed the Earth's climate sensitivity. The purely radiative (blackbody) warming from a doubling of CO_2 from its preindustrial level of 280 parts-per-million (ppm) to 560 ppm is ∼ 1.2°C; the actual warming that would result is considerably larger owing to amplification by climate feedbacks, including that owing to water vapor. Increases in greenhouse gas (GHG) levels are estimated to have contributed about +3.0 W m^(−2) perturbation (radiative forcing) to the Earth's energy balance. Particles (aerosols), on the whole, exert a cooling effect on climate, with a total forcing estimated by the Intergovernmental Panel on Climate Change (2007)1 as −1.2 W m^(−2), a value that is subject to considerable uncertainty. If the actual magnitude of aerosol forcing is close to the low end of its estimated uncertainty range, then it offsets a considerably smaller fraction of the GHG forcing and the total net forcing is at the high end of its range, ∼ 2.4 W m^(−2); at the other extreme, if the actual aerosol cooling is at the high end of its range, then aerosol forcing is currently offsetting a major fraction of GHG forcing, and the total net forcing is only ∼ 0.6 W m^(−2). To explain the actual global increase in temperature of ∼ 0.8°C, these two extremes have major implications in terms of the Earth's climate sensitivity. Climate sensitivity is determined by the strength of feedbacks, of which cloud feedback is the most uncertain. That the Earth has warmed and that GHGs are responsible is unequivocal; the Earth's climate sensitivity and the effect of aerosols complicate answers to the question: how much warming and how soon?


Item Type:Article
Related URLs:
URLURL TypeDescription
http://dx.doi.org/10.1002/aic.12780DOIUNSPECIFIED
http://onlinelibrary.wiley.com/doi/10.1002/aic.12780/abstractPublisherUNSPECIFIED
ORCID:
AuthorORCID
Seinfeld, John H.0000-0003-1344-4068
Additional Information:© 2011 American Institute of Chemical Engineers. Manuscript received Jul. 5, 2011, and revision received Sept. 12, 2011. Article first published online: 11 OCT. 2011.
Subject Keywords:global warming; climate sensitivity; greenhouse gases
Issue or Number:12
Record Number:CaltechAUTHORS:20111221-114535592
Persistent URL:https://resolver.caltech.edu/CaltechAUTHORS:20111221-114535592
Official Citation:Seinfeld, J. H. (2011), Insights on global warming. AIChE Journal, 57: 3259–3284. doi: 10.1002/aic.12780
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:28548
Collection:CaltechAUTHORS
Deposited By: Jason Perez
Deposited On:21 Dec 2011 21:12
Last Modified:03 Oct 2019 03:33

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