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The numerical meta analysis of 92 proxy records (72 sites) of moisture and/or temperature change confirms earlier findings that the dominant trends of climatic evolution in monsoonal central Asia since the Last Glacial roughly parallel changes in Northern Hemisphere summer Insolation i e the period following the Last Glacial Maximum was characterized by dry and cold conditions until 15 cal kyr BP followed by a warm wet period coincident with the Bolling/Allerod warm period and terminated by a cold dry reversal during the Younger Dryas period After an abrupt increase at the start of the Holocene warm and wet conditions prevailed until ca 4 cal kyr BP when moisture levels and temperatures started to decrease

Ordination of moisture records reveals strong spatial heterogeneity in moisture evolution during the last 10 cal kyr The Indian Summer Monsoon (ISM) areas (northern India Tibetan Plateau and southwest China) exhibit maximum wet conditions during the early Holocene while many records from the area of the East Asian Summer Monsoon indicate relatively dry conditions especially in north central China where the maximum moisture levels occurred during the mid-Holocene We assign such phenomena to strengthened Hadley Circulation centered over the Tibetan Plateau during the early Holocene which resulted in subsidence in the East Asian monsoonal regions leading to relatively dry conditions Our observations of the asynchronous nature of the two Asian monsoon subsystems on millennial time scales have also been observed on annual time-scales as well as implied through the spatial analysis of vertical air motion patterns after strong ascending airflows over the Tibetan Plateau area that were calculated from NCEP/NCAR reanalysis data for the last 30 years Analogous with the early Holocene the enhancement of the ISM in a future warming world will result in an increase in the asynchronous nature of the monsoon subsystems this trend is already observed in the meteorological data from the last 15 years (c) 2010 Published by Elsevier B V