Not exact matches
* Circulation changes in the Faeroe - Shetland Channel correlating
with cold events
during the last
glacial period (58 - 10 ka).
Using climate models to understand the physical processes that were at play
during the
glacial periods, the team were able to show that a gradual rise in CO2 strengthened the trade winds across Central America by inducing an El Nino - like warming pattern
with stronger warming in the East Pacific than the Western Atlantic.
They compared them
with mammals that lived at seven Eurasian sites
during the last
glacial period 35,000 to 12,000 years ago.
During the last part of the Pleistocene there were actually five major
periods of glaciation
with four
periods of warmer non
glacial conditions between them.
For example, the uniform lowering of tropical snowline by about 900 meters
during the Last
Glacial Maximum is generally attributed to cooling [Porter 2001], and indeed provided the first indication that something was wrong with plankton - based estimates of tropical cooling during the glacial
Glacial Maximum is generally attributed to cooling [Porter 2001], and indeed provided the first indication that something was wrong
with plankton - based estimates of tropical cooling
during the
glacial glacial period.
ABSTRACT BODY: The high - latitude, shallow ESAS has been alternately subaerial and inundated
with seawater
during glacial and interglacial
periods respectively.
Some unknown natural forcing exists
with a
period of 1470 yrs, and the climate system is subject to stochastic resonance
during glacials.
It seems increasingly clear that D - O events must involve major sea ice changes (and there is not much sea ice left, by comparison
with what was present
during the
glacial period (20000 + years ago, when these events happened), so D - O events are increasingly unlikely in the future).
The kind of switch operating
during glacial periods, leading to D - O events, is unlikely to work in a warm climate
with relatively little ice.
It is virtually certain that millennial - scale changes in atmospheric CO2 associated
with individual antarctic warm events were less than 25 ppm
during the last
glacial period.
The planet went from interglacial warm to
glacial cold
during the Younger Dryas
period with cooling for around 1000 years.
It rose more than that going from the
glacial period to the Younger Dryas (about 120 m), and may have risen about 24 m to 36 m from the Younger Dryas to the Holocene, but has only slowly varied
during the Holocene,
with variation less than 1 m over the last 6,000 y. I don't think NYC is in any danger.
Similarly, a colder climate
with generally decreased humidity q O could be closer to the critical threshold, which might be the reason for less - stable monsoon circulations
during glacial periods.
During the same
period, the terminus of the glacier thinned.2 The correlation of these
glacial changes
with rising temperatures implies that warming influences glacier motion almost immediately.1, 2,7,8
Manabe and Stouffer (1993) pioneered the demonstration of a transition under future warming; an improved model showed a shutdown was especially likely
with rapid increase of greenhouse gas emissions, Stocker and Schnitter (1997); see also Broecker (1997); Wood et al. (1999); summary: Rahmstorf (1999); Ganopolski and Rahmstorf (2001) for instability
during a
glacial period; IPCC (2001a), pp. 439 - 40.
Our record shows that CO2 variations
during the
glacial period have a clear relationship
with abrupt climate changes in the Northern Hemisphere that continues into the deglacial
period.
1998 was near the tail end of a decade that jumped well above the mean average longer term rate of increase (there is a thing called climate variability, it didn't disappear
with climate change, and if anything probably only intensified;, and ocean warming and
glacial melt both accelerated
during this
period, taking more energy out of the air — see below).
Similarly, warm
periods with glacial retreat occurred within the late Cenozoic cool
period during the late Oligocene and early Miocene epochs.
The duration and severity of the
glacial periods increased
during this
period,
with a particularly sharp change occurring between 900,000 and 600,000 years ago.