1. Shutting down the
thermohaline circulation
David Anthoff
University of California, Berkeley
Francisco Estrada
Universidad Nacional Autónoma de Mexico
Richard S.J. Tol
University of Sussex, Vrije Universiteit Amsterdam,
Tinbergen Institute, CESifo
2.
3.
4.
5.
6. Key concern
• Climate change could lead to
• More rain over the North Atlantic
• Melting of the Greenland Ice Sheet
• This would lead to a drop in salinity and may slow-
down – or even shut-down – the thermohaline
circulation
16. -25.0
-22.5
-20.0
-17.5
-15.0
-12.5
-10.0
-7.5
-5.0
-2.5
0.0
2.5
5.0
-1.5 -1.0 -0.5 0.0 0.5 1.0 1.5 2.0 2.5 3.0 3.5 4.0 4.5 5.0 5.5 6.0 6.5
Welfare-equivalentincomechange(inpercent)
Global warming (in degrees centrigrade)
Fit same function per country:
Optimum temperature:
0.3K, range -3 - +7K above today
Slopes vary from zero to 28%Y/K
17. Hosing
• Coupled atmosphere-ocean general circulation
models project a slight weakening of the
thermohaline circulation
• The impact of a more drastic weakening are studied
using so-calling hosing experiments, in which a
Death Star suddenly appears to spout freshwater
into the North Atlantic
22. Wrap-up
• Warming is bad, cooling is worse
• The cooling due to a shut- or slowdown of the
thermohaline circulation is modest relative to the
warming that would induce that.
• Reduced warming would lead to a welfare gain in
most countries