LOL It is deniers that use blogs and other non-science avenues to citique published scientific theory.
How can you say that with any credibility?
I specified blogs without good source links.
Your link only gave other internal links. No source links.
If you notice, I rarely link blogs. The few blogs that a few skeptics here do link, are very, very well source.
I hace to ask. Are you a troll? You most certainly aren't contributing to a debate.
There are certainly many scientific papers on the relationship of Glacier melt and Ocean circulations. Here is but one
Yes, and I have a subscription to nature Climate change. I go by what journals say. Not bloggers like your precious Planet Extinction. Who knows how much they hyped up.
Not to mention the already observed weakening of the Gulf Stream.
Melting glaciers are slowing down the Gulf Stream - UPI.com
Whoop-t-do...
A news organization.
These things are cyclical. So what?
Besides, nobody is saying it isn't occurring. There are both natural and anthropogenic forces at play. Just throwing out a blog doesn't do much.
Notice that the letter in the September edition of Nature Climate Change is not a peer reviewed paper either. It is a letter!
Consider the implications of this paragraph:
Observations, proxies and model simulations suggest that a recent
weakening of the AMOC has occurred. Furthermore, models
predict that such a slowdown will continue as a result of increasing
greenhouse gas concentrations. Such a weakening of the
AMOC would have drastic impacts on the climate of the North Atlantic
and western Europe. Although there is considerable debate
regarding the dynamics of the AMOC (ref. 29), one proposed mechanism
for its present and predicted decline is a freshening of the
surface waters -- for instance, due to enhanced meltwater emanating
from the Greenland Ice Sheet -- that reduces their density, making it
more difficult for oceanic convection to occur. However, much of
the freshwater discharge from the Greenland Ice Sheet is apt to be exported
equatorwards via the boundary current system surrounding
Greenland, with limited direct spreading into the interior basins
adjacent to the ice sheet where oceanic convection occurs. Further
work is thus necessary to determine how and where -- and on what
timescales -- this fresh water pervades the northwest Atlantic. Our
results suggest that other possible mechanisms for such a slowdown
in the AMOC may be at work; such as a reduction in the magnitude
of the surface heat fluxes that trigger the overturning.
Note, that this is speculation as to the causes. "Models suggest," etc. then some blogger gets a hold of such cautious language and states these as facts!