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• W2064983008 endingPage "1068" @default.
• W2064983008 startingPage "1055" @default.
• W2064983008 abstract "There is a strong chance that 20th century warming will cause differences in precipitation distribution, hydrological cycle and effective moisture changes over the globe. Arid central Asia (ACA), a unique dry-land area whose atmospheric circulation is dominated today by the westerlies, is one of the specific regions that are likely to be strongly impacted by global warming. An understanding of past variations in effective moisture in such regions is an important prerequisite for the prediction of future hydrological change. Here we evaluate spatial and temporal patterns of effective moisture variations documented by different proxies from 17 records in ACA, and synthesize a decadal-resolution moisture curve for ACA over the past millennium, using 5 of the 17 records selected on the basis of reliable chronologies and robust proxies. The high- and low-resolution data all show that, over the past millennium, ACA has been characterized by a relatively dry Medieval Warm Period (MWP; the period from ∼1000 to 1350 AD), a wet Little Ice Age (LIA; from ∼1500 to 1850 AD) and increasing moisture during recent decades. As a whole, the LIA in the ACA was not only relatively humid but also had high precipitation. Over the past millennium, the multi-centennial moisture changes in ACA show a generally inverse relationship with the temperature changes in the Northern Hemisphere, China, and western central Asia. The effective moisture history in ACA also shows an out-of-phase relationship with that in monsoon Asia (especially during the LIA). We propose that the humid LIA in ACA, possibly extending to Mediterranean Sea and Western Europe, may have resulted from increased precipitation due to more frequent mid-latitude cyclone activities as a result of the strengthening and equator-ward shift of the westerly jet stream, and the predominantly negative North Atlantic Oscillation conditions, coupled with a decrease in evapotranspiration caused by the cooling at that time." @default.
• W2064983008 created "2016-06-24" @default.
• W2064983008 creator A5011762910 @default.
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• W2064983008 creator A5055078491 @default.
• W2064983008 creator A5066384428 @default.
• W2064983008 creator A5066905603 @default.
• W2064983008 date "2010-04-01" @default.
• W2064983008 modified "2023-10-14" @default.
• W2064983008 title "Moisture changes over the last millennium in arid central Asia: a review, synthesis and comparison with monsoon region" @default.
• W2064983008 cites W130772771 @default.
• W2064983008 cites W1491837801 @default.
• W2064983008 cites W158388062 @default.
• W2064983008 cites W1820825883 @default.
• W2064983008 cites W1867582763 @default.
• W2064983008 cites W1894858710 @default.
• W2064983008 cites W1965943112 @default.
• W2064983008 cites W1966359065 @default.
• W2064983008 cites W1969842583 @default.
• W2064983008 cites W1970460919 @default.
• W2064983008 cites W1973110714 @default.
• W2064983008 cites W1973460574 @default.
• W2064983008 cites W1974992986 @default.
• W2064983008 cites W1975675071 @default.
• W2064983008 cites W1976278229 @default.
• W2064983008 cites W1979693604 @default.
• W2064983008 cites W1981733710 @default.
• W2064983008 cites W1986344936 @default.
• W2064983008 cites W1995470375 @default.
• W2064983008 cites W1996932107 @default.
• W2064983008 cites W1997083589 @default.
• W2064983008 cites W1999538456 @default.
• W2064983008 cites W1999745977 @default.
• W2064983008 cites W2003999641 @default.
• W2064983008 cites W2007619330 @default.
• W2064983008 cites W2010530988 @default.
• W2064983008 cites W2017977879 @default.
• W2064983008 cites W2019702130 @default.
• W2064983008 cites W2024532862 @default.
• W2064983008 cites W2024897559 @default.
• W2064983008 cites W2025181120 @default.
• W2064983008 cites W2027745714 @default.
• W2064983008 cites W2030174121 @default.
• W2064983008 cites W2031236252 @default.
• W2064983008 cites W2034795620 @default.
• W2064983008 cites W2034882391 @default.
• W2064983008 cites W2037799531 @default.
• W2064983008 cites W2039003315 @default.
• W2064983008 cites W2041756570 @default.
• W2064983008 cites W2042859974 @default.
• W2064983008 cites W2043514774 @default.
• W2064983008 cites W2045026668 @default.
• W2064983008 cites W2048608554 @default.
• W2064983008 cites W2054167751 @default.
• W2064983008 cites W2057468256 @default.
• W2064983008 cites W2062457444 @default.
• W2064983008 cites W2064315155 @default.
• W2064983008 cites W2065148284 @default.
• W2064983008 cites W2067383298 @default.
• W2064983008 cites W2070015210 @default.
• W2064983008 cites W2070843428 @default.
• W2064983008 cites W2072732165 @default.
• W2064983008 cites W2073432436 @default.
• W2064983008 cites W2074476121 @default.
• W2064983008 cites W2074833779 @default.
• W2064983008 cites W2074964089 @default.
• W2064983008 cites W2077600132 @default.
• W2064983008 cites W2083869894 @default.
• W2064983008 cites W2085873135 @default.
• W2064983008 cites W2086192317 @default.
• W2064983008 cites W2094049607 @default.
• W2064983008 cites W2099196698 @default.
• W2064983008 cites W2101522077 @default.
• W2064983008 cites W2107939894 @default.
• W2064983008 cites W2108766392 @default.
• W2064983008 cites W2113361120 @default.
• W2064983008 cites W2116196335 @default.
• W2064983008 cites W2123765309 @default.
• W2064983008 cites W2124579984 @default.
• W2064983008 cites W2126147651 @default.
• W2064983008 cites W2128246514 @default.
• W2064983008 cites W2130256070 @default.
• W2064983008 cites W2131532072 @default.
• W2064983008 cites W2131562505 @default.
• W2064983008 cites W2132506844 @default.
• W2064983008 cites W2138644576 @default.
• W2064983008 cites W2148275090 @default.
• W2064983008 cites W2151746416 @default.
• W2064983008 cites W2154957597 @default.
• W2064983008 cites W2159715259 @default.
• W2064983008 cites W2160336235 @default.
• W2064983008 cites W2165126803 @default.
• W2064983008 cites W2166586570 @default.
• W2064983008 cites W2168566790 @default.

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