Hello.
I remember reading about this more in depth a while ago and see it crop up in various discussions every now and again on this forum, but was hoping somebody could point me in the right direction for the current state of the science on this.
I'm referring to the fact that at certain conditions the Hadley cells rearrange to a single cell (per hemisphere) system, leading to a 'Greenhouse' Climate with much more equable conditions from the equator to the poles.
I have tried to find what I can but have not found very much.
I found this paper:
http://www.fields.utoronto.ca/programs/scientific/10-11/biomathstat/Langford_W.pdfWhich seems to suggest it is the temperature gradient between the equator and the poles that governs this switch, and that the system exhibits hysteresis between the two states.
I also found this one which had quite a bit on the switch between the states:
http://www.seas.harvard.edu/climate/eli/research/equable/hadley.htmlThere were a few other papers I found but none seemed to give me the kind of answers I was hoping to find.
Basically, is there science now supporting the fact that as the temperature gradient decreases the Hadley Cell system will switch states? And if so, have they got an estimated range for that value? Then obviously I would like to know how far away from that point we are now!
If the Hadley Cell does flip to a single cell 'Greenhouse' Climate (which it seems the hemispheres can do independently) this will have massive implications for the changes we can expect, especially to the cryoshpere. The GIS will surely disappear much faster than currently predicted, as will the permafrost. Possibly even the clathrates.
So does anyone have any up to date information on this aspect of the science? Are the jet stream and Hadley cells exhibiting behaviour that should be getting us worried?
Thanks for any contribution you may have to offer.
(If there is an existing thread for this please let me know, I couldn't find one)