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• W2400264115 abstract "The Tibetan plateau, with a mean elevation of more than 4.000 m asl. and an area of more than 2.000.000 km, acts as a heating surface during spring and summer and plays a key role in driving the different branches of the Asian summer monsoon circulation (Murakami 1987). During the last decades, temperature conditions on the Tibetan plateau (TP) have increased in a considerable higher magnitude than the northern hemispheric mean (Wang et al. 2001; Liang et al. 2009; Liu et al. 2010), especially during winter. This leads to higher snow precipitation during winter and a decrease of constantly frozen ground (Zhao et al. 2004). Model scenarios predict an intensification of the summer monsoon system under increasingly warmer climatic conditions (Liu et al. 2009), which is supported by positive precipitation trends in most regions of China (Zhao et al. 2004; Wu et al. 2006), with an increasing trend of heavy rainfall events (Liu et al. 2005). In order to derive realistic estimates on future water availability and/or flood risks, understanding the relationships between temperature and precipitation variations, glacier fluctuations and the variability of the Southwestand East Asian Summer Monsoon as well as the Winter Monsoon is a crucial task. Climate stations were not installed on the TP before 1950. In addition, as big differences in altitude occur in comparatively short distances, spatial interpolation of temperature and precipitation between distant data points may be questionable. Since different branches of the summer monsoon system react differently to atmospheric circulation patterns like ENSO, reconstructing and predicting changes in monsoonal patterns is a complex task that can only be assessed by a combination of approaches. Previous studies on the TP revealed that maximum latewood density (MXD) is a good indicator of regional summer temperature (Brauning & Mantwill 2004, Wang et al. 2010). High-frequency densitometry is a quick, non-destructive alternative to X-ray densitometry (Schinker et al. 2003). Tree-ring density variables, especially for maximum latewood density from cold moist sites, have great potential for reconstructing summer or growing season temperature (Duan et al. 2010)." @default.
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• W2400264115 date "2012-01-01" @default.
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• W2400264115 title "Preliminary results from ring width and latewood density measurements from the southeast Tibetan Plateau, China" @default.
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