The references in the list at the end of this post discuss positive feedback mechanisms (and related topics), that in my opinion, were not adequately accounted for in IPCC's AR5 (nor in the AVOID model projections).
While I do not have time to do any of this findings justice; nevertheless, I will say that to whatever RCP scenario that your value system allows you to accept as realistic, you need to add the following factors that were left out of AR5 (and AVOID) projections:
(a) Sherwood et al (2014) and Fasullo & Trenberth (2012) show that the most likely value for ECS is about 4.5 degrees C instead of the assumed mean value of 3 degrees C; therefore, you should multiply the old projections by a factor of about 1.5, due to the low amount of cloud cover near the equator.
(b) Pistone et al. (2014) shows that the decrease in Arctic albedo (including land snow, sea ice and black carbon effects) beyond that previously assumed results in additional radiative forcing equal to ¼ of the CO₂ in the atmosphere.
(c) Schuur & Abbott (2011) shows that the permafrost emits about 2% of its carbon emissions as methane instead of as CO₂ (as assumed by AVOID), and as over a one hundred year period, methane has a global warming potential at least 35 times that of CO₂, this means at least a 70% error in the carbon emissions from the permafrost degradation. See also Monday et al. (2014) and Isaksen et al. (2011).
(d) Cowtan & Way (2013); England et al. (2014); Santer et al (2014); and Rosenfeld (2014); all provide solid evidence that the current mean global temperature has been masked by such causes as: limited data; the negative phase of the PDO cycle; volcanoes, and aerosols, respectively. Furthermore, once corrections are applied to the GCM projections to account for these masking mechanisms, one will find that the ECS is actually higher than previously assumed, which supports my points (a), (b) and (c).
(e) Hansen et al. (2013) and Previdi (2013) show that the inclusion of slow-response feedback mechanisms can cause Earth Systems Sensitivity to be as high as 6 degrees C (while work such as Pistone et al. (2014) shows that the "slow response" feedback mechanisms are occurring very quickly).
I do not have time to comment on the other excellent references cited below, but I would also like to say many negative feedback mechanisms are shrinking quickly (such as the absorption of CO₂ by plankton, etc.), so that it is not only positive feedback mechanisms that we need to be realistic about.
Best,
Abrupt SLR
References:
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http://dx.doi.org/10.1126/science.1227465.[5] Frederick, J.M., and Buffett, B.A., (2014), "Taliks in relict submarine permafrost and methane hydrate deposits: Pathways for gas escape under present and future conditions", Journal of Geophysical Research: Earth Surface, DOI: 10.1002/2013JF002987.
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