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38篇 您的检索式:作者名="Ersi"
    题名 作者 年代 出处 被引量
1RIVER DISCHARGE CHANGES IN THE QINGHAI-TIBET PLATEAU显示文摘Annual mean discharge data of the five large rivers in the exorheic region of the Qing- hai-Tibet Plateau from 1956 to 2000 are analyzed for trends with the Mann-Kendall nonparametric trend test. The results reveal that though in general no in- creasing trends exist in the total river discharges, significant regional differences of river discharge ex- ist, reflecting the decreasing trends of discharge in the Yellow River and the Tongtian River (upper Changjiang River), an increasing trend in Yalong River, and inverted change in the Lancang River and Yarlung Zangbo River. Based on analyses of the seasonal discharge, it is found that climatic change had a significant effect on the seasonal variation of river discharge in the Qinghai-Tibet Plateau. In spring (from March to May) the discharge increased signifi- cantly, especially in the source area of the Yellow River. Together with the analyses on data of the mean temperature in the Northern Hemisphere and climatic data within the river basins, the relationship between discharges and mean temperature of the Northern Hemisphere is explored, which indicates that there is no increase in the stream discharge in the Qinghai-Tibet Plateau with global warming. It is probably the increasing evaporation, caused by rising temperature that offsets the hydrological effect of increasing precipitation.CAO Jianting QIN Dahe KANG Ersi LI Yuanyuan 2006Chinese Science Bulletin2006,51,5:9
2Estimation of tree transpiration and response of tree conductance to meteorological variables in desert-oasis system of Northwest China显示文摘Transpirations of three dominated tree species, namely Mongol Scotch Pine (Pinus sylvestris var. mongolica Litvin), White elm (Ulmus pumila) and Gansu Poplar (Populus gansuensis Wang et Yang) in oasis shelter forest (Linze site) and of two dominated tree species,namely Euphrates Poplar (Populus euphratica Oliv.) and Russia olive (Elaeagnus angustifolia Linn.) in lowland desert (Erjinaqi site) have been estimated using measured sapflow in summer,autumn and winter, 2002 and in spring, 2003. An ENVIS System was used for each site to measure microclimate variables, soil moisture and sapflow every half an hour, and the study time scale is one day. In the 104 days of observation during the growing season at the Linze site, the average daily sapflow of Gansu Poplar is 9.93L·d-1,and the average transpiration per unit leaf area is 1.99mm·d-1.For White elm tree,the daily average sapflow is 4.08L·d-1,while the daily average transpiration per unit leaf area is 0.49mm·d-1.The values for Mongol Scotch Pine are 3.91L·d-1 and 0.25mm·d-1,respectively.In the total 73 days of observation during the growing season at the Erjinaqi site, the daily average sapflows of Russia olive and Euphrates Poplar are 12.1 and 20.97L·d-1,respectively,and the average transpirations per unit leaf area are 0.22 amd 0.31mm·d-1,respectively.In the observation period of the growing season,tree conductances of Mongol Scotch Pine, White elm, Gansu Poplar or Russia olive show an exponential relationship with the daily average air temperature or vapour pressure deficit, but the relationship is not so obvious between tree conductance and global radiation. The transpiration process of each tree species is affected by all the observed four environmental variables. The response of tree conductance to different climatic factors changes with tree species. The effect of the same factor to the same tree species is also variable in different growing stages. The sapflow of every tree species is relatively large in later spring to early summer, and low in summer, and then reaches its largest value in later September. In the mid-November, the sapflow is relatively large, especially the deciduous tree species. This may be characteristic of the tree species in Arid Regions of Northwest China.CHEN Rensheng KANG Ersi ZHANG Zhihui ZHAO Wenzhi SONG Kechao ZHANG Jishi LAN Yongchao 2004Science China Earth Sciences2004,47,z1:5
3The relationship between ENSO cycle and temperature,precipitation and runoff in the Qilian mountain area显示文摘El Nino and La Nina are the events concerned internationally. The corresponding relationship between El Nino events, temperature, precipitation and runoff in the Qilian mountain area are analyzed according to the date from the weather and the hydrometric stations in the area, the results show that effects of El Nino events to temperature, precipitation and runoff are different in the different time and zones. When El Nino occurs, temperature rises, but precipitation and runoff decrease in the whole Qilian mountain area, especially in the east and middle parts of the area. Temperature rises, precipitation and runoff still decrease in the eastern Qilian mountain area in the next year El Nino occurring, but decrease extent is fewer. There are not obvious relationship between temperature, precipitation and runoff with El Nino events in the western Qilian mountain area.LAN Yongchao,DING Yongjian,KANG Ersi,ZHANG Jishi(Cold and Arid Regions Environmental and Engineering Research Institute, CAS, Lanzhou 730000, China) 2003Journal of Geographical Sciences2003,13,3:2
4Cryospheric change in China显示文摘Xin Li Guodong Cheng Huijun Jin Ersi Kang Tao Che Rui Jin Lizong Wu Zhuotong Nan Jian Wang Yongping Shen 2008Global and Planetary Change2008,,3:1
5Recent and fu- ture climate change in Northwest China显示文摘Shi Yafeng Shen Yongping Kang Ersi etal 2007Climate Change2007,80,:1
6Trishear fault propagation folding显示文摘ERSI EV E A 1991Geology1991,19,:1
7Using Avenue显示文摘 USA:Environmental Systems Research0,,:1
8Observation and estimation of evaporateion from the ground surface of the cryosphere in estern Asia显示文摘 Kang Ersi Ohata T 2003Hydrological Processes2003,17,:1
9Effect of pH and polymer charge density on settling rate and turbidity of natural stone suspensions显示文摘ERSY B 2005International Journal of Mineral Processing2005,75,34:1
10Prospects for Household Borrowing in Greece and their Importance for Growth显示文摘Ersi Athanassiou 2007South-Eastern Europe Journal of Economics 2007 (1)2007,2007,1:1
11Observation and estimation of evaporation from the ground surface of the cryosphere in Eastern Asia 显示文摘ZHANG Yinsheng OHATA T ERSI K 2003Hydrology Process2003,17,:1
12Recent and future climate change in northwest China显示文摘SHI Y F SHEN Y P KANG ERSI 2007Climatic Change2007,80,34:1
13An hourly solar radiation model under actual weather and terrain conditions: A case study in Heihe river basin 显示文摘Chen Rensheng Lu Shihua Kang Ersi 2007Energy2007,32,:1
14Variance tendency in the 50-year annual meteorological and hydrological series of Hexi region of Gansu Province 显示文摘Chen Rensheng Kang Ersi Yang Jianping 2002Journal of Lanzhou University (Natural Sciences)2002,38,2:1
15Ineontience in the climacteric显示文摘Ersi E 2000Clinical Obstetrics and Gynecology2000,33,:1
16Validation of five global radiation models with measured daily data in China显示文摘Chen Rensheng Kang Ersi Yang Jianping 2004Energy Conversion and Management2004,45,:1
17Combination therapy of deferasirox and deferoxamine shows signifieant improvements in markers of iron overload in a patient with beta-thalassemia major and severe iron burden 显示文摘Ersi Voskaridou Veroniki Komninaka Antonis Karavas 2014Transfusion2014,54,3:1
18An hourly solar radiation model under actual weather and terrain conditions : A case study in Heihe river basin 显示文摘Chen Rensheng Lu Shihua Kang Ersi 2007Energy2007,32,:1
19Cold regions in China显示文摘Chen Rensheng Kang Ersi Ji Xibin 0,,02:1
20Recent and Future Climate Change in Northwest China显示文摘Yafeng Shi Yongping Shen Ersi Kang Dongliang Li Yongjian Ding Guowei Zhang Ruji Hu 2007Climatic Change (-)2007,,3:1
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