Climate model simulations of the Last
Glacial Maximum show an even stronger Bodélé LLJ compared with that of the present, and dated evidence points to the conditions under which deflation would have been capable of excavating the depression which was later partly filled by paleolake Megachad (31).
Not exact matches
The results of these simulations
show that dust − climate feedbacks, perhaps set off by orbital forcing, push the system in and out of extreme cold conditions such as
glacial maxima.
He makes the following statement, which is misleading if not outright wrong: Paleo records
shows that both temperature and sea level have been mostly rising since last
glacial maximum and more recently, since the so called little ice age.
As part of ENSO cycles such droughts come and go — and have been typical for the region for (at least) all of the Holocene up to the Last
Glacial Maximum some 20,000 years ago, research
shows.
al (2012)
showed that the simulated global - mean cooling during the Last
Glacial Maximum (LGM, 19 - 23 ka before present) is inversely correlated to ECS in CMIP3 models.
Results
show that the coldest
glacial maxima temperatures are a product of the dust − climate feedbacks considered here (Fig. 5B).
Visual inspection of Fig. 2
shows maximum dust fluxes for
maximum glacial cooling.
They made a retrodiction for Last
Glacial Maximum sea surface temperatures which was inconsistent with the paleo evidence, and better paleo evidence
showed the models were right.
«Here, we
show central China is a region that experienced a much larger temperature change since the Last
Glacial Maximum than typically simulated by climate models... We find a summertime temperature change of 6 — 7 °C that is reproduced by climate model simulations presented here.»