Abstract
Long-term variations in the effective moisture of deserts are linked both to glacial–interglacial climatic cycles and, through the Milankovitch theory, to orbitally induced changes in solar radiation intensity1–4. For southwestern North America, comparison of palaeobotanical data with model predictions of palaeoclimate reveals two distinct pluvial regimes during the late Wisconsin and early Holocene (23–8 kyr BP). Southward displacement of the Aleutian low-pressure centre and strengthened westerlies from ∼40° to 30° N were important features of the full-glacial (∼ 18 kyr BP) pluvial maximum. Increased cyclonic storms and weakened monsoons led to a winter precipitation regime, a feature seen both in the fossil record5,6 and climate models7,8. Dominantly zonal flow during this period contrasts with the latest Wisconsin and early Holocene (12–8 kyr BP), when meridional circulation transported maritime tropical air into the desert interior. We now show that plant macrofossil assemblages from packrat (Neotoma spp.) middens9 in the Mojave Desert provide evidence for increased temperatures and summer rainfall during this period10–12. The anomalously late persistence (to ∼8 kyr BP) of woodland in low-latitude, low-elevation deserts of the south-west13 is attributed to enhanced monsoonal circulation3.
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Spaulding, W., Graumlich, L. The last pluvial climatic episodes in the deserts of southwestern North America. Nature 320, 441–444 (1986). https://doi.org/10.1038/320441a0
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DOI: https://doi.org/10.1038/320441a0
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