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Reconstructions,of annual,(prior August-current,July) precipitation,and streamflow, 345 years in length (AD 1651-1995), are presented for northeastern,Mongolia,based,on tree-ring width,data. These,precipitation,and streamflow,reconstructions,account,for 54% and,48% of the respective variance,in instrumental,data,over,the past,50 years. Variations,in instrumental,precipitation,and,streamflow,are within,the range,of those reconstructed over the length of tree-ring record. However, there appear to be more,frequent,extended,wet,periods,during,the 20th century.,Multitaper spectral,analysis,revealed,statistically,significant,peaks,at 10.8 and,12.8 years for the precipitation reconstruction, and at 12.8 and 20.3-23.8 years for the streamflow reconstruction. Similarly, singular spectrum analysis identified,spectral,modes,of variation,at 12 and,21 years for both,series. These,spectra,resemble,those,found,for tree-ring based,precipitation reconstructions in central China as well as the western USA, and may reflect solar influences,on the climate,of Mongolia. 3

Hydrometeorological Reconstructions for Northeastern Mongolia Derived from Tree Rings: 1651–1995*