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| 1 | Glacial distribution and mass balance in the Yarlung Zangbo River and its influence on lakes显示文摘Glaciers in the Yarlung Zangbo River witness severe glacial retreat nowadays,which gives important influence on lake processes in the region.We have studied glacial distribution,glacial mass balance and found large deficit in glacial mass and its impact in the region.Our study also integrated the variation in glacial-fed lakes of the Nam Co and Ranwu Lake,and presented an initial assessment of the impact of glacial mass balance on lakes.The study has shown a significant contribution of glacial melting to recent lake expansion and lake level rising. | YAO TanDong LI ZhiGuo YANG Wei GUO XueJun ZHU LiPing KANG ShiChang WU YanHong YU WuSheng | 2010 | Chinese Science Bulletin2010，55，20： | 34 |
| 2 | Seasonal variations of stable isotope in precipitation and moisture transport at Yushu,eastern Tibetan Plateau显示文摘Precipitation δ 18O at Yushu, eastern Tibetan Plateau, shows strong fluctuation and lack of clear seasonality. The seasonal pattern of precipitation stable isotope at Yushu is apparently different from either that of the southwest monsoon region to the south or that of the inland region to the north. This different seasonal pattern probably reflects the shift of different moisture sources. In this paper, we present the spatial comparison of the seasonal patterns of precipitation δ 18O, and calculate the moisture transport flux by using the NCAR/NCEP reanalysis data. This allows us to discuss the relation between moisture transport flux and precipitation δ 18O. This study shows that both the southwest monsoon from south and inland air mass transport from north affected the seasonal precipitation δ 18O at Yushu, eastern Tibetan Plateau. Southwest monsoon brings the main part of the moisture, but southwest transport flux is weaker than in the southern part of the Tibetan Plateau. However, contribution of the inland moisture from north or local evaporation moisture is enhanced. The combined effect is the strong fluctuation of summer precipitation δ 18O at Yushu and comparatively poor seasonality. | TIAN LiDe MA LingLong YU WuSheng LIU ZhongFang YIN ChangLiang ZHAO ZhongPing TANG Wei WANG Yu | 2008 | Science China Earth Sciences2008，51，8： | 9 |
| 3 | Climatic significance of δ^(18)O records from precipitation on the western Tibetan Plateau显示文摘Analysis of daily precipitation samples for stable oxygen isotopes (δ18O) collected at the Shiquanhe and Gêrzê (Gaize, Gertse) stations in the Ngari (Ali) region on the western Tibetan Plateau indicates that air temperature affects the δ18O variations in precipitation at these stations. In summer, Shiquanhe and Gêrzê show strongly similar trends in precipitation δ18O, especially in simultaneous precipitation events. Moreover, both stations experienced low δ18O values in precipitation during the active monsoon period, resulting from the southwest monsoon (the summer phase of the Indian monsoon). However, during the break monsoon period (during the summer rainy season, when the monsoon circulation is disrupted), δ18O values in summer precipitation remain relatively high and local moisture recycling generally controls the moisture sources. Air temperature correlations with δ18O strengthen during the non-monsoon period (January―June, and October―December) due to continental air masses and the westerlies. In addition, evaporation also influences the δ18O variations in precipitation. The observed temporal and spatial variations of δ18O in precipitation on the western Tibetan Plateau and adjacent regions show that the late May and early June-the late August and early September time frame provides an important period for the transportation of moisture from various sources on the Tibetan Plateau, and that the region of the West Kunlun-Tanggula Ranges acts as a significant climatic divide on the Plateau, perhaps for all of western China. | YU WuSheng MA YaoMing SUN WeiZhen WANG Yu | 2009 | Chinese Science Bulletin2009，54，16： | 9 |
| 4 | Isotopic composition of atmospheric water vapor before and after the monsoon's end in the Nagqu River Basin显示文摘Atmospheric water vapor samples were col-lected in the Nagqu River Basin in the middle of Tibetan Plateau between August and October in 2004. Results show that there exist some fluctuations of the δ 18O of atmospheric water vapor, especially before and after the monsoon’s end. Moreover, the variety trend of the δ 18O of atmospheric water vapor inverse correlates with that of dew point. Precipitation events make an important effect upon the variation of δ 18O of atmospheric water vapor. During the whole sampling pe-riod, the δ 18O values of atmospheric water vapor are low while precipitation events occurred. The moisture origins also contribute to the variation of δ 18O of atmospheric water vapor. The oceanic moisture transported by the southwest monsoon results in lower δ18O of atmospheric water vapor in the Nagqu River Basin. Compared with the influence of the oceanic moisture, the δ 18O values, however, appear high re-sulting from the effect of the continental air mass in this re-gion. | YU Wusheng YAO Tandong TIAN Lide WANG Yu YIN Changliang | 2005 | Chinese Science Bulletin2005，50，23： | 7 |
| 5 | Temporal and spatial variations of δ^18O in precipitation of the Yarlung Zangbo River Basin显示文摘这份报纸在 2005 在四个车站(Lhaze, Nugesha, Yangcun 和 Nuxia ) 在降水基于未 1 8O 的变化在 Yarlung Zangbo 河盆的降水揭示稳定的同位素的时间、空间的变化。结果证明降水的未 1 8O 在 Yarlung Zangbo 河盆有不同季节的变化。未 1 8O 的更高的价值在季风降水以前在春天发生,并且更低的价值发生在季风降水期间。从空间变化,沿着 Yarlung Zangbo 河山谷在潮湿运输期间与高度效果和 rainout 处理,降水的 18O 逐渐地被弄空。因此,降水的未 1 8O 逐渐地减少从对下游在上游,并且在降水的未 1 8O 的差错率为二个原因是约 0.34 鈥 ? 100m 和 0.7 鈥 ? 100km。在季风降水期间,在降水的未 1 8O 的空间变化被数量效果在大规模统治摘要的状况。 | LIU Zhongfang TIAN Lide YAO Tandong GONG Tongliang YIN Changliang YU Wusheng | 2007 | Journal of Geographical Sciences2007，17，3： | 7 |
| 6 | What Determines China's Grain Imports and Self-sufficiency? The Role of Rising Domestic Costs and Varying World Market Prices显示文摘China s grain sectors have faced unprecedented challenges in recent years as the ever-increasing and historically high level of grain output has failed to reduce grain imports. On the contrary, high grain imports and high domestic stock have accompanied historically high domestic output, a situation dubbed the 'triple high' phenomenon in current policy discussion. This paper explores the role of widening domestic-world market price gaps in determining the triple high phenomenon.Unlike earlier studies that relied on production capacities, this paper argues that domestic production and demand (hence imports) are functions of domestic and world market prices and proposes an analytical framework to explicitly capture such price gaps under restricted trade linkages in general equilibrium. Following this approach, a set of price scenarios for the 2011-2020 period are constructed and simulated in a computable general equilibrium model. Results from the core scenarios, in which recent domestic and world market price trends are assumed to continue, suggest that further widening price gaps would substantially increase grain imports and reduce domestic output (by 60 million tons) and self-sufficiency ratios from base levels. In the alternative scenarios with larger (smaller) price gaps, we find higher (lower) imports and larger (smaller) decreases in domestic output and self-sufficiency ratios. Such results provide important policy implications as China's agricultural policy undergoes significant adjustment. | Wusheng Yu Tianxiang Li Jing Zhu | 2019 | China & World Economy2019，27，5： | 5 |
| 7 | Jensen, China's Agricultural Policy Transition: Impacts of Recent Reforms and Future Scenarios显示文摘 | Yu Wusheng Hans G | 2010 | Journal of Agricultural Economics2010，61，： | 1 |
| 8 | Different region climate regimes and topography affect the changes in area and mass balance of glaciers on the north and south slopes of the same glacierized massif (the West Nyainqentanglha Range, Tibetan Plateau)显示文摘 | Wusheng Yu Tandong Yao Shichang Kang Jianchen Pu Wei Yang Tanguang Gao Huabiao Zhao Hang Zhou Shenghai Li Weicai Wang Linglong Ma | 2013 | Journal of Hydrology2013，，： | 1 |
| 9 | Trade policy responses to food price crisis and implications for existing domestic support measures: the case of China in 2008显示文摘 | Yu Wusheng Jensen Hans G | 2014 | Word Trade Review2014，13，4： | 1 |
| 10 | Relationships between δ^18O in precipitation and air temperature and moisture origin on a south-north transect of the Tibetan Plateau显示文摘 | YU Wusheng YAO Tandong TIAN Lide | 2008 | Atmospheric Research2008，87，2： | 1 |
| 11 | Seasonal deuterium excess in Nagqu precipitation: influence of moisture transport and recycling in the middle of Tibetan Plateau显示文摘 | Zhongfang Liu Lide Tian Tandong Yao Wusheng Yu | 2008 | Environmental Geology2008，，7： | 1 |
| 12 | China’s import duty drawback and VAT rebate policies: A general equilibrium analysis显示文摘 | Chi-Chur CHAO Eden S.H. YU Wusheng YU | 2006 | China Economic Review2006，，4： | 1 |
| 13 | Dif- ferent region climate regimes and topography affect the changes in area and mass balance of glaciers on the north and south slopes of the same glacierized massif (the West Nyainqentanglha Range, Tibetan Plateau ) 显示文摘 | Yu Wusheng Yao Tandong Kang Shichang | 2013 | Journal of Hydrology2013，495，2： | 1 |
| 14 | The Chinese Export Displacement Effect Revisited:The Case of the East African Community显示文摘China's increasing exports have prompted research to examine whether Chinese exports displace those that originate from elsewhere.In this paper we focus on the growth of China's exports to the East African Community(EAC)countries and show how they have afected exports from the European Union(EU).Our methodological contribution to the literature is a set of total and relative displacement estimates based on different specifications of the gravity model where we control for country-year fixed effects so as to avoid the error of not accounting for time-varying'multilateral resistance.'Our empirical findings do not support the hypothesis that Chinese exports have displaced exports from other countries including those from the EU.These results suggest that competition in the EAC market has not been a zero-sum game among different exporting countries. | Christian Elleby Wusheng Yu Qian Yu | 2023 | China & World Economy2023，31，6： | 0 |
| 15 | Study on ChemFET NO_2 Gas Sensor Array显示文摘Based on conventional metal-oxide-semiconductor field-effect transistor (MOSFET),a novel kind of chemical field-effect transistor (ChemFET) gas sensor array has been designed and fabricated.The obtained sensor consists of self-assembly polyaniline (PAN) composite film containing poly(acrylic acid) (PAA) which was used as gate material of MOSFET instead of conventional metallic gate.The UV-Vis absorption spectra of PAN/PAA films were characterized.The NO_2 gas sensitive property of the ChemFET sensor array was also investigated.Results show that the drain current of devices increases with increasing of back-side voltage,and decreases with the increase of NO_2 concentration when the NO_2 concentration is below 20μg/g.The temperature dependence of ChemFET sensor array shows that the drain current of ChemFET sensor decreases with increasing of temperature. | Guangzhong Xie Junsheng Yu Huilin Tai Wusheng Suo Yadong Jiang Bangchao Yang | 2006 | 稀有金属材料与工程2006，35，A03： | 0 |
| 16 | Stable isotopic compositions of precipitation events from Kathmandu, southern slope of the Himalayas显示文摘Investigation of temporal variations in the stable d18 O and d D isotopes from Kathmandu's precipitation events shows that the relatively enriched d18 O and d D values in the winter(the dry season, dominated by the westerlies) were positively correlated with temperature,indicating a temperature effect controlling the changes of d18 O and d D. However, the d18 O and d D values were depleted in the summer(the wet season, dominated by the Indian monsoon), which were negatively correlated with precipitation amount, indicating an amount effect. In addition, the comparison of stable isotopes in precipitation from Kathmandu and Mawlong(near the Bay of Bengal)shows that the overall trends of d18 O and d D values at Kathmandu generally approximate those at Mawlong.However, there remain many differences between the details of the isotopic changes at Kathmandu versus those at Mawlong. Compared with those at Mawlong, the further rainout effect and the more intense lift effect of the oceanic moisture by the high mountains resulted in the moredepleted d18 O and d D values in summer precipitation at Kathmandu. A deuterium excess and the local meteoric water lines reveal that evaporation at Kathmandu exceeds that at Mawlong. The data also show that the Indian monsoon activities at Mawlong are more intense than those at Kathmandu. | Tek Bahadur Chhetri Tandong Yao Wusheng Yu Li Ding Daniel Joswiak Lide Tian Lochan Prasad Devkota Dongmei Qu | 2014 | Chinese Science Bulletin2014，59，34： | 0 |
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