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| 1 | Arctic Sea Ice and Eurasian Climate:A Review显示文摘The Arctic plays a fundamental role in the climate system and has shown significant climate change in recent decades,including the Arctic warming and decline of Arctic sea-ice extent and thickness. In contrast to the Arctic warming and reduction of Arctic sea ice, Europe, East Asia and North America have experienced anomalously cold conditions, with record snowfall during recent years. In this paper, we review current understanding of the sea-ice impacts on the Eurasian climate.Paleo, observational and modelling studies are covered to summarize several major themes, including: the variability of Arctic sea ice and its controls; the likely causes and apparent impacts of the Arctic sea-ice decline during the satellite era,as well as past and projected future impacts and trends; the links and feedback mechanisms between the Arctic sea ice and the Arctic Oscillation/North Atlantic Oscillation, the recent Eurasian cooling, winter atmospheric circulation, summer precipitation in East Asia, spring snowfall over Eurasia, East Asian winter monsoon, and midlatitude extreme weather; and the remote climate response(e.g., atmospheric circulation, air temperature) to changes in Arctic sea ice. We conclude with a brief summary and suggestions for future research. | GAO Yongqi SUN Jianqi LI Fei HE Shengping Stein SANDVEN YAN Qing ZHANG Zhongshi Katja LOHMANN Noel KEENLYSIDE Tore FUREVIK SUO Lingling | 2015 | Advances in Atmospheric Sciences2015，32，1： | 21 |
| 2 | Paleoclimate Modeling in China: A Review显示文摘This paper provides a review of paleoclimate modeling activities in China. Rather than attempt to cover all topics, we have chosen a few climatic intervals and events judged to be particularly informative to the international community. In historical climate simulations, changes in solar radiation and volcanic activity explain most parts of reconstructions over the last millennium prior to the industrial era, while atmospheric greenhouse gas concentrations play the most important role in the20 th century warming over China. There is a considerable model–data mismatch in the annual and boreal winter temperature change over China during the mid-Holocene [6000 years before present(ka BP)], while coupled models with an interactive ocean generally perform better than atmospheric models. For the Last Glacial Maximum(21 ka BP), climate models successfully reproduce the surface cooling trend over China but fail to reproduce its magnitude, with a better performance for coupled models. At that time, reconstructed vegetation and western Pacific sea surface temperatures could have significantly affected the East Asian climate, and environmental conditions on the Qinghai–Tibetan Plateau were most likely very different to the present day. During the late Marine Isotope Stage 3(30–40 ka BP), orbital forcing and Northern Hemisphere glaciation, as well as vegetation change in China, were likely responsible for East Asian climate change. On the tectonic scale,the Qinghai–Tibetan Plateau uplift, the Tethys Sea retreat, and the South China Sea expansion played important roles in the formation of the East Asian monsoon-dominant environment pattern during the late Cenozoic. | JIANG Dabang YU Ge ZHAO Ping CHEN Xing LIU Jian LIU Xiaodong WANG Shaowu ZHANG Zhongshi YU Yongqiang LI Yuefeng JIN Liya XU Ying JU Lixia ZHOU Tianjun YAN Xiaodong | 2015 | Advances in Atmospheric Sciences2015，32，2： | 12 |
| 3 | Late Paleozoic Fluid Systems and Their Ore-forming Effects in the Yuebei Basin,Northern Guangdong,China显示文摘Based on detailed and systematic researches of the geology of ore deposits, fluid inclusions and isotope geochemistry etc., and regarding the Late Paleozoic fluid system of the Yuebei Basin as an integrated object in this paper, we have revealed the temporo-spatial evolution law of the basin’s fluid system and discussed its ore-forming effects by simulating and analyzing the distribution of ore-forming elements, the fluid thermodynamics and dynamics of evolution processes of this basin. The results show that Late Paleozoic ore-forming fluid systems of the Yuebei Basin include four basic types as follows. (1) The sea floor volcanic-exhalation system developed during the rapid basin slip-extension stage in the Mid-Late Devonian, which affected the Dabaoshan region. It thus formed the Dabaoshan-type Cu-Pb-Zn-Fe sea floor volcanic-exhalation sedimentary deposits. (2) The compaction fluid system developed during the stable spreading and thermal subsidence-compression stage of the basin in the Mid-Late Devonian. The range of its effects extended all over the whole basin. It resulted in filling-metasomatic deposits, such as the Hongyan-type pyrite deposits and pyrite sheet within the Fankou-type Cu-Pb-Zn-S deposits. (3) The hot water circulation system of sea floor developed during the stage of basin uplifting and micro-aulacogen from the late Late Carboniferous to Middle Carboniferous. The range of its effects covered the Fankou region. It thus formed MVT deposits, such as the main orebody of the Fankou-type Pb-Zn-S deposits. (4) The gravity fluid system developed during the stage of fold uplifting and the basin closed from Middle Triassic to Jurassic, forming groundwater hydrothermal deposits, e.g. the veinlet Pb-Zn-calcite orebodies of the Fankou-type Pb-Zn-S deposits. Migration and concentration of the ore-forming fluids were constrained by the state of temporo-spatial distribution of its fluid potential. Growth faults not only converged the fluids and drove them to move upwards, but also the fluids often crossed the faults to the edges of the basin at the bottom of these faults and the lithologic interfaces, and even migrated to the basin’s edges from top to bottom along the faults, which may be one of the basic reasons for the stratabound deposits to cluster mainly along the contemporaneous faults on the inner border of the basin. The superposed mineralization resulting from the multi-stage activity of contemporaneous faults and ore-forming fluid systems in the basin may be one of the key factors for forming superlarge ore deposits. | DENG Jun YANG Liqiang SUN Zhongshi WANG Jianping WANG Qingfei CHENG Xueming ZHOU Yinghua | 2005 | Acta Geologica Sinica(English Edition)2005，79，5： | 6 |
| 4 | Greenland Ice Sheet Contribution to Future Global Sea Level Rise based on CMIP5 Models显示文摘Sea level rise(SLR) is one of the major socioeconomic risks associated with global warming. Mass losses from the Greenland ice sheet(GrIS) will be partially responsible for future SLR, although there are large uncertainties in modeled climate and ice sheet behavior. We used the ice sheet model SICOPOLIS(SImulation COde for POLythermal Ice Sheets) driven by climate projections from 20 models in the fifth phase of the Coupled Model Intercomparison Project(CMIP5) to estimate the GrIS contribution to global SLR. Based on the outputs of the 20 models, it is estimated that the GrIS will contribute 0–16(0–27) cm to global SLR by 2100 under the Representative Concentration Pathways(RCP) 4.5(RCP 8.5) scenarios. The projected SLR increases further to 7–22(7–33) cm with 2×basal sliding included. In response to the results of the multimodel ensemble mean, the ice sheet model projects a global SLR of 3 cm and 7 cm(10 cm and 13 cm with 2×basal sliding) under the RCP 4.5 and RCP 8.5 scenarios, respectively. In addition, our results suggest that the uncertainty in future sea level projection caused by the large spread in climate projections could be reduced with model-evaluation and the selective use of model outputs. | YAN Qing WANG Huijun Ola M.JOHANNESSEN ZHANG Zhongshi | 2014 | Advances in Atmospheric Sciences2014，31，1： | 5 |
| 5 | Key gene and protein changes in the beta-amyloid pathway following Longyanshen polysaccharides treatment in a mouse model of Alzheimer's disease显示文摘BACKGROUND:During onset and development of Alzheimer's disease,β-amyloid(Aβ) precursor protein(APP),β-site amyloid precursor protein cleaving enzyme(BACE),andβ-amyloid are key genes and proteins in the Aβpathway,and over-expression of these genes can lead to Aβdeposition in the brain. OBJECTIVE:To observe the influence of Longyanshen polysaccharides on expression of BACE, APP,and Aβin the senescence-accelerated mouse prone/8(SAMP8) brain,and to compare these effects with huperzine A treatment. DESIGN,TIME AND SETTING:A randomized,controlled,neurobiochemical experiment was performed at the Department of Pharmacology and Scientific Experimental Center of Guangxi Medical University from September 2005 to January 2008. MATERIALS:Longyanshen polysaccharides powder was extracted from the dried slices of the medicinal plant Longyanshen.The active component,Longyanshen polysaccharides,was provided by the Department of Pharmacology,Guangxi Medical University;huperzine A was purchased from Yuzhong Drug Manufactory,China. METHODS:Healthy SAMP8 mice were used to establish a model of Alzheimer's disease.A total of 50 SAMP8 mice were randomly assigned to 5 groups(n = 10):SAMP8,huperzine A,low-,middle-, and high-dose polysaccharides.In addition,10 senescence-accelerated mouse resistant 1(SAMR1) mice were selected as normal controls.SAMP8 and SAMR1 mice were administered 30 mL/kg normal saline;the huperzine A group was administered 0.02 mg/kg huperzine A;the low-,middle-, and high-dose polysaccharides groups were respectively administered 45,90,and 180 mg/kg Longyanshen polysaccharides.Each group was treated by intragastric administration,once per day, for 50 consecutive days. MAIN OUTCOME MEASURES:One hour after the final administration,immunohistochemical analysis was used to determine Aβexpression in the cortex and hippocampus of SAMP8 mice. Reverse-transcription polymerase chain reaction was used to determine mRNA levels of BACE and APP in SAMP8 brain tissue. RESULTS:Compared with the SAMR1 group,Aβexpression in the cerebral cortex and hippocampus,as well as expression of BACE,APP mRNA in the brain was significantly increased in the SAMP8 group(P<0.05-0.01).Compared with the SAMP8 group,Aβexpression,as well as BACE and APP mRNA expression,were significantly decreased in the cerebral cortex and hippocampus of huperzine A and low-,middle-,and high-dose polysaccharides groups(P<0.05-0.01).In particular,the effect of high-dose polysaccharides was the most significant(P<0.05-0.01). CONCLUSION:Longyanshen polysaccharides reduced or inhibited over-expression of BACE,APP, and Aβin SAMP8 mice in a dose-dependent manner,and the effect was not worse than huperzine A. | Zhongshi Huang Shijun Zhang Haiyuan Xie Xing Lin Weizhe Jiang Renbin Huang | 2009 | Neural Regeneration Research2009，4，10： | 4 |
| 6 | Global Dynamics near the Resonance in the Sine-Gordon Equation显示文摘樱椋睿澹牵铮颍洌铮? EquationTX1IntroductionThenonlineardynamicsofthedampeddrivensine-Gordonequationut-uxx+sinu=-ε(αut+Γcosωt),(1.1)whe?.. | Huang Debin Liu Zengrong (Shanghai University) Cheng Zhongshi (Shanghai Administrative College for Trade Union Cadres) | 1998 | Advances in Manufacturing1998，，4： | 3 |
| 7 | Simulation of Greenland ice sheet during the mid-Pliocene warm period显示文摘One of the key uncertainties in future sea-level projections is attributed to the Greenland ice sheet(GrIS).Studying the response of the GrIS to climate changes during the past warm periods is helpful for understanding future changes in the GrIS.In this study,using three global climate models(Community Atmosphere Model version3.1 and version 4.0 and Norwegian Earth System Model)and a three-dimensional ice sheet model,we investigate the climate and ice sheet changes over Greenland during the mid-Pliocene warm period(*3 Ma BP).The results show that the regionally averaged summer temperature over Greenland is 9.4–13.4°C higher during the mid-Pliocene period than during the pre-industrial era and the annual mean precipitation is 65.2–108.3 mm a-1greater.In response to this warm-wet climate,the GrIS shows a substantial decrease in size during the mid-Pliocene,with little ice existing along the eastern coast of Greenland.Compared to that simulated in the control run,the global sea level is approximately 7.8–8.1 m higher during the mid-Pliocene due to the decrease in the size of the GrIS.In addition,paleoclimate proxies also indicate that it is unlikely that a large-scale ice sheet exists over Greenland during the mid-Pliocene warm period. | Qing Yan Zhongshi Zhang Huijun Wang Ran Zhang | 2014 | Chinese Science Bulletin2014，59，2： | 3 |
| 8 | Simulation of sea surface temperature changes in the Middle Pliocene warm period and comparison with reconstructions显示文摘The Middle Pliocene (ca 3.12–2.97 Ma) is a recent warm period in the Earth’s history. In many respects, the warmth of the Middle Pliocene is similar to the probable warm situation of the late 21st century predicted by climate models. Understanding the Middle Pliocene climate is important in predicting the future climate with global warming. Here, we used the latest reconstructions for the Middle Pliocene—Pliocene Research Interpretation and Synoptic Mapping (PRISM) version 3—to simulate the Middle Pliocene climate with a fully coupled model Fast Ocean Atmosphere Model. From comparison of the results of simulations with reconstructions, we considered two important scientific topics of Middle Pliocene climate modeling: extreme warming in the subpolar North Atlantic and a permanent El Ni?o in the tropical Pacific. Our simulations illustrate that the global annual mean sea surface temperature (SST) in the Middle Pliocene was about 2.3°C higher than that in the pre-industrial era. The warming was stronger at midand high latitudes than at low latitudes. The simulated SST changes agree with SST reconstructions in PRISM3 data, especially for the North Atlantic, North Pacific and west coast of South America. However, there were still discrepancies between the simulation of the SST and reconstructions for the subpolar North Atlantic and tropical Pacific. In the case of the Atlantic, the weakened meridional overturning circulation in the simulation did not support the reconstruction of the extremely warm condition in the subpolar North Atlantic. In the case of the tropical Pacific, the whole ocean warmed, especially the eastern tropical Pacific, which did not support the permanent El Ni?o suggested by the reconstruction. From evaluation of the modeling and reconstruction, we suggest that the above discrepancies were due to uncertainties in reconstructions, difficulties in paleoclimate modeling and deficiencies of climate models. The discrepancies should be reduced through consideration of both the modeling and data. | YAN Qing ZHANG ZhongShi WANG HuiJun JIANG DaBang ZHENG WeiPeng | 2011 | Chinese Science Bulletin2011，56，9： | 2 |
| 9 | Tectonic evolvement of metamorphic complexes at Jilin paleocontinental margin during the transition from late Archaean to early Proterozoic显示文摘The kinematics and dynamical process of tectonic evolvement of metamorphic complexes at the interim from late Archaean to early Proterozoic is one of the key problems in geosciences. For the disputation on the genesis of metamorphic complexes at the margin of Jilin palaeocontinent, this paper takes the example of Banshigou region, Jilin Province to discuss the dynamical evolution of palaeocontinent during the transition from late Archaean to early Pro- terozoic (2600—2000 Ma). On the time sequence, from center to palaeocontinental margin, it shows a series of dynamical movements including underplating, horizontal movement, subduc- tion, intraplate extension and separation. And its corresponding sequence of kinematical modes is as follows: vertical movement, horizontal movement, extension and shearing in contact zone, uplift-sliding movement in paleocontinental margin and interformational sliding, resulting in such tectonite sequence, tectonic gneiss, gneissic complex, gneissic complex-mylonite, mylonite and fracture cleavage-mylonite, which consist of the main body of metamorphic complexes. Their palaeostresses are: < 20, 20.40, 21.72, 28.80 and 30.8-69.8 MPa respectively. The deforma- tional metamorphic temperature is between hornblende and low-grade greenschist facies. The general deformational characters of Jilin palaeocontinent reflect a complete dynamic system of crust evolution, which indicates that the formation of the metamorphic complexes and the tec- tonic evolution are altered from vertical movement to compression to extension. It also indicates a continuous tectonic transformation from deep to shallow, and from ductile to brittle. The trans- formation between different dynamic mechanisms not only forms tectonic rocks, but also benefits the linking up, exchange and enrichment with rock-forming minerals and ore-forming elements. This research is helpful to classifying regional tectonic events and making further study on the evolution of palaeocontinental dynamics. | SUN Zhongshi1,DENG Jun2,JIANG Yanguo3,WANG Jianping2,WANG Qingfei2 & WEI Yanguang2 1.Department of Earth Sciences,Jilin University,Changchun 130061,China 2.Department of Geosciences and Mineral Resources,China University of Geosciences,Beijing 100083,China 3.Weihai Gold Institute,Shandong Weihai Gold Bureau,Weihai 264205,China Correspondence should be addressed to Sun Zhongshi(email: sunzs219@163.com) | 2004 | Science China Earth Sciences2004，47，11： | 2 |
| 10 | A Dynamic Distributed Spectrum Allocation Mechanism Based on Game Model in Fog Radio Access Networks显示文摘With the explosive growth of highspeed wireless data demand and the number of mobile devices, fog radio access networks(F-RAN) with multi-layer network structure becomes a hot topic in recent research. Meanwhile, due to the rapid growth of mobile communication traffic, high cost and the scarcity of wireless resources, it is especially important to develop an efficient radio resource management mechanism. In this paper, we focus on the shortcomings of resource waste, and we consider the actual situation of base station dynamic coverage and user requirements. We propose a spectrum pricing and allocation scheme based on Stackelberg game model under F-RAN framework, realizing the allocation of resource on demand. This scheme studies the double game between the users and the operators, as well as between the traditional operators and the virtual operators, maximizing the profits of the operators. At the same time, spectrum reuse technology is adopted to improve the utilization of network resource. By analyzing the simulation results, it is verified that our proposed scheme can not only avoid resource waste, but also effectively improve the operator's revenue efficiency and overall network resource utilization. | Yao Yu Shumei Liu Zhongshi Tian Siyu Wang | 2019 | China Communications2019，16，3： | 2 |
| 11 | Effects of low-pressure O^-2 and Zn atmosphere on the green emission of ZnO phosphor显示文摘 | Liu Z S Author Reprint Author Liu Zhongshi Liu Zhongshi Jing XP | 2006 | J Electrochem Soc2006，153，12： | 1 |
| 12 | Current Status of Research on Optimum Sizing of Stand-a- lone Hybrid Solar-wind Power Generation Systems 显示文摘 | Zhou Wei Lou Chengzhi Li Zhongshi | 2010 | Applied Energy2010，87，2： | 1 |
| 13 | Emission proper- ties of Eu2+, Mn2+ in MAl2Si2O8 (M= Sr, Ba) 显示文摘 | Ye Shi Liu Zhongshi Wang Xiuteng | 2009 | Journal of Luminescence2009，129，： | 1 |
| 14 | Enhanced Sensitivity and Selectivity of Chemosensor for Malonate by Anchoring on Gold Nanoparticles显示文摘有 bis-thiourea 的 4 functionalized 武装的新奇器官无机的 nanohybrided 受体然后集合在金 nanoparticles 上被综合。preorganized 系统为 dicarboxylates 察觉到的 spectrophotometric 拥有 phenylthiourea 单位,特别 malonate,基于在金 nanoparticles (GNP ) 的表面电浆子吸收的变化。吸收度乐队的紧张与 dicarboxylates 增加的集中逐渐地增加。但是在电浆子乐队的如此的一个离子选择的变化没在测试由 mono-thiourea-modified GNP 执行了的控制被观察,受体第 3a 免费 receptor2。当它从协会常数被显示出,源于量的滴定,受体 4 能有选择地认出更短的碳链的 dicarboxylate 阴离子,并且有最高的亲密关系到 malonate。为受体 4 的阴离子的相互作用性质被 1H NMR 和紫外力的分光镜的方法评估。 | Liu, Yanyun Liu, Yun Liang, Zhongshi Li, Xiangyang Liu, Shunying Yu, Jiahui | 2011 | Chinese Journal of Chemistry2011，29，3： | 1 |
| 15 | Diagnostic value of carcinoembryonic antigen in malignant pleural effusion: A meta‐analysis显示文摘 | Huan‐ZhongSHI Qiu‐LiLIANG JingJIANG Xue‐JunQIN Hai‐BoYANG | 2008 | Respirology2008，，4： | 1 |
| 16 | Composite Metallogenic Systems in the Weihai Area of Shandong and Evolution of Continental Dynamic Regimes显示文摘摘要:把地区性的地质的调查基于9张l:50,000规模并且由 metallogenic 系统的理论和综合分析指导了结构并且 metallogenic 特征,这份报纸在此提出 Weihai 区域的合成 metallogenic 系统,山东省,瞄准在区域在起源和众多的存款的控制矿石的结构上解决这些问题。它的科学意义在下列三个方面被反映:(1 ) 合成 metallogenic 系统的基本特征能被认出,它由二种类型组成:原生地变形热水的 metallogenic 系统和中生代 magmatic 热水的 metallogenic 系统(即 Indosinian 早 Yanshanian 接触交代矿床 metallogenic 系列和中间迟了的 Yanshanian magmatic 热水的 metallogenic 系列) 。二个系列分别地显示弓形、 NW 正确的侧面的安排和 N-S 平行带的分布,与相应矿物质集合是 Au+Ag+Pb+Zn,等等;并且 Cu+Mo+Fe, Au+Ag+Cu+Pb-Zn+Mo+Co-Ni+suIfides+silicides+K-feldspar,等等(2 ) 合成 metallogenic 系统可以被用来解释沉积物的复杂基因关系。通过在三主要 metallogenic 之间的关系的分析,间隔和他们的相应来源摇系列(Jingshan 和 Rongcheng 组;超级单位的 Wendong 和早中间的 Yanshanian Weideshan 超级单位;并且中间迟了的 Yanshanian Weideshan 和 Laoshan 超级单位) 象 Fanjiabu 金沉积物的案例研究一样,我们区分了在接触交代矿床(skarn类型)之间的同宗象 noncognate 重叠在之间一样的 metallogenic 系列和magmatic热水的 metallogenic 系列二并且变形热水的 metallogenic 系统。(3 ) 合成 metallogenic 系统是容易与大陆人的进化有关动态政体。变形热水的 metallogenic 系统的形成从扩展经历了 tectono 动态的政体的三种不同类型的转变 ? 压缩 ? 砍接触交代矿床(skarn 类型) 的从压缩的 metallogenic 系统 ? 扩展 ? 压缩;并且从扩展的 magmatic 热水的 metallogenic 系统的 ? 和平的板的 subductive 压缩。三种类型的进化都被归因于洞关上或 paleocontinent 的分叉集中,和所有他们的矿化作用从集中的结束对应于转变的间隔到 Weihai paleocontinent 的早集成。都,这些将有益于我们大陆人 metallogenic 过程的动力学的更深的学习。 | SUN Zhongshi WANG Peifu DENG Jun WANG Qingfei WANG Jianping MU Taisheng SUN Li FAN Siqi YE Songqing LIU Zhenghong CUI Shuxue | 2007 | Acta Geologica Sinica(English Edition)2007，81，2： | 1 |
| 17 | Multisource image fusion method using support value transform 显示文摘 | Sheng Zheng Wen Zhongshi Liu Jian | 2007 | IEEE Transactions on Image Processing2007，16，7： | 1 |
| 18 | Organic modification on TiO2 nanoparticles by grafting polymer显示文摘 | Ling Zan Zhongshi Liu Jiacheng Zhong Zhenghe Peng | 2004 | Journal of Materials Science2004，，9： | 1 |
| 19 | First case of Edwardsiella ictaluri infection in China farmed yellow catfish Pelteobagrus fulvidraco显示文摘 | Shigen Ye Hua Li Guo Qiao Zhongshi Li | 2009 | Aquaculture2009，，1： | 1 |
| 20 | First case of Edwardsiella ictaluri infection in China farmed yellow catfish Pelteobagrus fulvidraco显示文摘 | Shigen Ye Hua Li Guo Qiao Zhongshi Li | 2009 | Aquaculture2009，，1： | 1 |
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