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| 1 | Precipitation variation in the northeastern Tibetan Plateau recorded by the tree rings since 850 AD and its relevance to the Northern Hemisphere temperature显示文摘Three well-dated Sabina Przewalskii ring-width chronologies from Dulan, China, have been used to reconstruct annual precipitation (from prior July to current June) variations on the northeast Tibetan Plateau since 850 AD. The reconstructions account of the instrumentally recorded precipitation variance are: 54.7% for the period of 1385-2000AD; 50.5% for 1099-1384AD and 45.7% for 850-1098AD. On the millenary scale, the precipitation variation over this region displays “W” shape, which has three peaks and two valleys. The precipitation is low during 1571-1879 AD, and high during 1880-2000 AD. 1900-2000 AD is the century with the highest precipitation over the northeast Tibetan Plateau in the last 1000 years, and 1962-2000 is the period with the highest pre- cipitation, and the highest variability of precipitation as well in the last 1000 years. The reconstructed series also reveals that the variability of annual precipitation is large when the precipitation is more, and contrarily, variability is small when the precipitation is low. With the temperature increasing obvi- ously in the 20th century, the precipitation in the study region significantly increased too, the variability of precipitation became larger, and drought and flooding occurred more frequently. The yearly tree-ring width (high frequency signal) series in this region reflects the local annually precipitation variation. However, the series with 40-year moving average (low frequency signal) cor- responds to the Northern Hemisphere temperature variations on the decadal to centurial scale. It correlates significantly with seven temperature curves of the Northern Hemisphere in the different time spans. For example, the correlation coefficients with the most temperature curves are around 0.9 during the period of 1852-1982 AD. In general, the temperature and the precipitation change syn- chronously in the Dulan region. It means that low temperature corresponds to low precipitation, andvice versa. This relationship may indicate that the climatic pattern is the combination of warm-wet and cold-dry on centenary to millenary scale over the Northern Tibetan Plateau in the past 1000 years. The departure series of 40-year moving average could be regarded as the millenarian temperature curve with annual resolution over the northeast Tibetan Plateau region. | John K. Kutzbach | 2006 | Science China Earth Sciences2006，49，4： | 44 |
| 2 | Asynchronous Holocene optimum of the East Asian monsoon显示文摘 | Zhisheng An Stephen C. Porter John E. Kutzbach Wu Xihao Wang Suming Liu Xiaodong Li Xiaoqiang Zhou Weijian | 2000 | Quaternary Science Reviews2000，，8： | 2 |
| 3 | Hemispheric insolation forcing in the Indian Ocean and Asian monsoon:local versus remote impacts显示文摘 | Liu X Liu Z Kutzbach J | | Journal of Climate0，19，23： | 1 |
| 4 | Pangaean climates:megamonsoons of the megacontinent显示文摘 | Kutzbach J E Gallimore R G | 1989 | Journal of Geophysical Research1989，，94： | 1 |
| 5 | Simulation of threshing and separation processes in threshing units显示文摘 | Miu P I Kutzbach H D | 2000 | Agrartechnische Forschung2000，，6： | 1 |
| 6 | Milankovitch forcing of fluctuations in the level of tropical lakes from 18~0 kyr BP显示文摘 | STREET-PERROTT F A | 1985 | Nature1985，317，： | 1 |
| 7 | Sensitivity of Eurasian Climate to surface up lift of the Tibetan Plateau显示文摘 | KUTZBACH J E PRELL W L RUDDIMAN W F | 1993 | Journal of Geology1993，101，： | 1 |
| 8 | The sensitivity of climate to late Cenozoic uplift in southeast Asia and the American southwest:Numerical experiments显示文摘 | GUETTER P J RUDDIMAN W F | 1989 | J Geophys Res1989，94，18： | 1 |
| 9 | Characteristics of gouty arthritis in the Guatemalan population显示文摘 | Gareia CO Kutzbach AG Espinoza LR | 1997 | Clin Rheumatol1997，16，1： | 1 |
| 10 | Vegetation and soil feedbacks on the response of the African monsoon to orbital forcing in the Early to Middle Holocene显示文摘 | BONAN G FOLEY J | 1996 | Nature1996，384，： | 1 |
| 11 | Mathematical model of material kinematics in an axial threshing unit显示文摘 | Miu P I Kutzbach H D | 2007 | Computers and Electronics in Agriculture2007，58，2： | 1 |
| 12 | Evolution of Asian Monsoons and Phased Uplift of the Himalaya Tibetan Plateau Since Late Miocene Times显示文摘 | An Z S Kutzbach J E Prell W L | 2001 | Nature2001，411，： | 1 |
| 13 | Sectoral iris hetevochromia and retinal pigment variation in 13q-syndrome 显示文摘 | Kutzbach B Mendelsohn N Rath P Summers CG | 2007 | J Am Assoc Pediatr Ophthalmol Strabismus2007，11，5： | 1 |
| 14 | Evolution of Asian mon soons and phased uplift of the Himalayan-Tibetan plateau since late Miocene times显示文摘 | An Z S Kutzbach J E Prell W L | 2001 | Nature2001，411，6833： | 1 |
| 15 | Sensitivity of Eurasian climate to surface uplift of the Tibetan Plateau 显示文摘 | Kutzbach J E Prell W L Ruddiman W F | 1993 | Journal of Geology1993，101，2： | 1 |
| 16 | Forcing of late Cenozoic northern hemisphere climate by plateau uplift in southern Asia and the American west 显示文摘 | Ruddiman W F Kutzbach J E | 1989 | Journal of Geophysical Research1989，94，18： | 1 |
| 17 | Sensitivity of Eurasian Climate to surface uplift of the Tibetan Plateau显示文摘 | Kutzbach J E Prell W L Ruddiman W F | 1993 | Journal of Geology1993，101，： | 1 |
| 18 | Sensitivity of the Indian monsoon to forcing parameters and implications for its evolution 显示文摘 | Prell W L Kutzbach J E | 1992 | Nature1992，360，： | 1 |
| 19 | Projected distribu- tions of novel and disappearing climates by 2100 AD显示文摘 | Williams J W Jackson S Kutzbach J | 2007 | Proceedings of the National Academy of Science2007，104，： | 1 |
| 20 | Evolution of Asian monsoons and phased uplift of the Himalaya-Tibetan plateau since late Miocene times显示文摘 | An Z S Kutzbach J E Prell W L | | 0，，： | 1 |
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