Not exact matches
During what are
called Heinrich events — natural but still largely unexplained fluctuations in the
global climate — the Atlantic Ocean's
circulation slows substantially.
At a
global scale, the increased melting of the ice sheet contributes to rising sea level and may impact
global ocean
circulation patterns through the so -
called «thermohaline
circulation'that sustains among others, the Gulf Stream, which keeps Europe warm.
The principal engine of this
global circulation, often
called the Ocean Conveyor, is the difference in salt content between the Atlantic and Pacific Oceans.
What you
call an «ocean pump» is not in fact a pump, but is a current that is part of what some
call the
global thermohaline
circulation.
In context of the criticism of your paper, and of the problems and failures in
global circulation models (now being
called global climate models by the way!)
Motivated by findings that major components of so -
called cloud «feedbacks» are best understood as rapid responses to CO2 forcing (Gregory and Webb in J Clim 21:58 — 71, 2008), the top of atmosphere (TOA) radiative effects from forcing, and the subsequent responses to
global surface temperature changes from all «atmospheric feedbacks» (water vapour, lapse rate, surface albedo, «surface temperature» and cloud) are examined in detail in a General
Circulation Model.
The closing of the Central American Seaway intensified the Gulf Stream, the upper limb of a conveyor - like
global ocean
circulation called the Ocean Conveyor.
That
global warm spell,
called the Mid-Pliocene Warm Period, may also have been related to the closing of the Central American Seaway and the consequent rearrangement of
global ocean
circulation.
The principal engine of this
global circulation, often
called the Ocean Conveyor, is the difference in salt content between the Atlantic and Pacific Oceans.