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Alternating wet and dry phases exert strong selection that imposes trade-offs and leads to multiple strategies for spreading risk through space and time.
Based on the datasets, we discern Late Pleistocene dry phases in the region during the Last Glacial Maximum, the Heinrich 1 event and the Younger Dryas.
The temporal dynamics of rainfall are modeled via a reward alternating renewal process that describes wet and dry phases of storms.
Additionally, we recognize at least six dry phases during the Holocene (after 6500 BCE, 4900 BCE, 3700 BCE, 1000 BCE, 450 CE and 1750 CE).
A fluvial regime around 48 ka and 30 21 ka with comparatively arid conditions and dry phases interspersed by flooding is documented.
The amount-effect based monsoon reconstruction showed that two distinct dry phases at 75 ka to 60 ka and 30 ka to 10 ka were punctuated by a wet phase from 60 ka to 30 ka.
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In the post-Gamblian dry phase, microlithic tools appear for the first time in an assemblage known as the Magosian.
The MJO has the ability to influence monsoonal circulation and rainfall by adding moisture during its cyclonic (wet) phase and reducing convection during its anticyclonic (dry) phase.
On a microscopic scale, model prebiotic nucleotide yields can increase when dried subunit mixtures are regularly rehydrated8, apparently because wet phases enable redistribution of unreacted molecules to more favorable locations/orientations for nucleotide formation during the next dry phase.
The modeling and testing are dedicated to the study of the re-irradiation and the dry phase.
A sedimentary hiatus after ∼40 ka BP is interpreted as a pronounced pre-LGM dry phase with landscape erosion/deflation.
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