The economic impact of extreme sea-level rise: Ice sheet vulnerability and the social cost of carbon dioxide

2014 ◽  
Vol 24 ◽  
pp. 99-107 ◽  
Author(s):  
Jonathan Pycroft ◽  
Lucia Vergano ◽  
Chris Hope
2021 ◽  
Vol 16 (9) ◽  
pp. 094037
Author(s):  
Jarmo S Kikstra ◽  
Paul Waidelich ◽  
James Rising ◽  
Dmitry Yumashev ◽  
Chris Hope ◽  
...  

Author(s):  
Jonathan Pycroft ◽  
Lucia Vergano ◽  
Chris Hope ◽  
Daniele Paci ◽  
Juan Carlos Ciscar

Author(s):  
Jonathan Pycroft ◽  
Lucia Vergano ◽  
Chris W. Hope ◽  
Daniele Paci ◽  
Juan Carlos Ciscar

2020 ◽  
Author(s):  
James Rising ◽  
Simon Dietz ◽  
Thomas Stoerk ◽  
Gernot Wagner

<div>Tipping points in the climate system are a key determinant of future impacts from climate change. Current consensus estimates for the economic impact of greenhouse gas emissions, however, do not yet incorporate tipping points. The last decade has, at the same time, seen publication of over 50 individual research papers on how tipping points affect the economic impacts of climate change. These papers have typically incorporated an individual tipping point into an integrated climate-economy assessment model (IAM) such as DICE to study how the the tipping point affects economic impacts of climate change such as the social cost of carbon (SC-CO2). This literature, has, however, not yet been synthesized to study the joint effect of the large number of tipping points on the SC-CO2. SC-CO2 estimates currently used in climate policy are therefore too low, and they fail to reflect the latest research.</div><div><br><div>This paper brings together this large and active literature and proposes a way to jointly estimate the impact of tipping points. In doing so, we bridge an important gap between climate science and climate economics. To do so, we develop a new integrated assessment model with frontier characteristics: a tractable geophysical module for each tipping point, damage functions based on recent climate econometric advances, and disaggregated climate change impacts at the national level, including from sea-level rise. In this model, we consider the following tipping points: the permafrost carbon feedback, the dissociation of ocean methane hydrates, Amazon forest dieback, the disintegration of the Greenland ice sheet, the disintegration of the West Antarctic ice sheet, the slowdown of the Atlantic Meridional Overturning Circulation, changed patterns of the India summer monsoon, and changes in surface albedo feedback (also referred to as Arctic sea-ice loss).</div> <div> </div> Our preliminary findings show that the geophysical tipping points tend to increase the economic impact of climate change, with a combined effect of increasing the social cost of carbon (SC-CO2) by 14%-43%. The largest contributions to this increase come from methane-related tipping points.</div>


Author(s):  
Patrick J. Applegate ◽  
K. Keller

Engineering the climate through albedo modification (AM) could slow, but probably would not stop, melting of the Greenland Ice Sheet. Albedo modification is a technology that could reduce surface air temperatures through putting reflective particles into the upper atmosphere. AM has never been tested, but it might reduce surface air temperatures faster and more cheaply than reducing greenhouse gas emissions. Some scientists claim that AM would also prevent or reverse sea-level rise. But, are these claims true? The Greenland Ice Sheet will melt faster at higher temperatures, adding to sea-level rise. However, it's not clear that reducing temperatures through AM will stop or reverse sea-level rise due to Greenland Ice Sheet melting. We used a computer model of the Greenland Ice Sheet to examine its contributions to future sea level rise, with and without AM. Our results show that AM would probably reduce the rate of sea-level rise from the Greenland Ice Sheet. However, sea-level rise would likely continue even with AM, and the ice sheet would not regrow quickly. Albedo modification might buy time to prepare for sea-level rise, but problems could arise if policymakers assume that AM will stop sea-level rise completely.


Author(s):  
Christoph Hambel ◽  
Holger Kraft ◽  
Eduardo Schwartz

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