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The Future: Hotter Than We Think?

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" ... it is likely that the future will be hotter than we think."
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Torn, M. S., and J. Harte (2006), Missing feedbacks,asymmetric
uncertainties, and the underestimation of future warming.
Geophysical Research Letters, 33, L10703, doi:10.1029/2005GL025540.

Received 19 December 2005; revised 17 March 2006; accepted 24 March
2006; published 26 May 2006.

Abstract:
Historical evidence shows that atmospheric greenhouse gas (GhG)
concentrations increase during periods of warming, implying a
positive feedback to future climate change. We quantified this
feedback for CO2 and CH4 by combining the mathematics of feedback
with empirical ice core information and general circulation model
(GCM) climate sensitivity, finding that the warming of 1.5-4.5 C
associated with anthropogenic doubling of CO2 is amplified to 1.6-6.0
C warming, with the uncertainty range deriving from GCM simulations
and paleo temperature records. Thus, anthropogenic emissions result
in higher final GhG concentrations, and therefore more warming, than would be predicted
in the absence of this feedback. Moreover, a symmetrical uncertainty
in any component of feedback, whether positive or negative, produces
an asymmetrical distribution of expected temperatures skewed toward
higher temperature. For both reasons, the omission of key positive
feedbacks and asymmetrical uncertainty from feedbacks, it is likely
that the future will be hotter than we think.

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"One study estimated that more than half (59 percent) of 1598 species
exhibited measurable changes in their phenologies and/or
distributions over the past 20 to 140 years .... high proportion of
species responding to recent, relatively mild climate change (global
average warming of 0.6 C)."

Parmesan, Camille. ' Ecological and Evolutionary Responses to Recent
Climate Change.' Annual Review of Evolution, Ecology, and
Systematics. 2006. 37: 637-69
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