Exact(11)
Possibly, after some cultural and typological discontinuity, perhaps caused by the maximum cold of the last phase of the Würm glaciation, the Baradostian was replaced by a local Upper Paleolithic industry called the Zarzian.
During the final period of maximum cold temperatures (23,000 to 16,500 years ago) in the latter part of the Pleistocene Ice Age (which ended 11,700 years ago), species that now constitute the taiga were displaced as far south as 30° N latitude by the continental glaciers of Europe, Asia, and North America and by the hyperarid and extremely cold environments of unglaciated Asia and North America.
The maximum cold heading force is calculated.
Carbon conversions of up to 0.79 were achieved, and maximum cold gas ratio and solar-to-fuel efficiency were 1.16 and 22%, respectively.
A maximum cold power of 19 W with a corresponding limited temperature difference of 5 K was achieved across a 0.5 m distance.
The results show that the optimum value of d∗c for the maximum cold air temperature difference and efficiency is d∗c = 0.5.
Similar(49)
The maximum cold-water solubility was obtained when treated at 400 W of applied power for 27.38 min.
The results show that, as compared with the single-stage counterpart, a significant improvement in the maximum cold-end temperature drop (ΔTc,max) is observed for the two-stage TEC.
The most recent peak was during the last glacial maximum, a cold period 25,000 years ago that preceded the end of the last ice age.
Maximal grassland expansion and Atlantic rainforest reduction were found during the last glacial maximum, reflecting cold and relatively dry climatic conditions.
This period coincides with the Early Upper Paleolithic (EUP) period, prior to the Last Glacial Maximum, but cold and dry enough to force a North African coastal route.
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