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| 1 | Geochemical characteristics of natural gas from mud volcanoes in the southern Junggar Basin显示文摘A number of mud volcanoes exist in the southern Junggar Basin. To date few systematic studies on natural gas geochemistry of mud volcanoes have been conducted in China. In June 1991 and August 2010, the authors investigated the mud volcanoes in the southern Junggar Basin twice, and the mud volcanism weakened gradually as seen from the variations such as the decrease of gas pressure and output, the downthrow and dry up of the mud pool. The volcanic intensity was significantly weaker than that in Taiwan. The natural gas from the mud volcanoes in the southern Junggar Basin has similar geochemical characteristics, indicating the same source or origin. The main component of the mud volcano gas is alkane gas with contents of 91.15%-97.49%, and the gas is high-quality commercial gas since methane dominates in the alkane. The 13C1 values are 49.1‰--40.6‰, which are in accordance with the peak 13C1 frequency of mud volcano gas around the world, and the alkane gas displays positive carbon isotopic series, i.e., 13C1< 13C2< 13C3, suggesting typical thermogenic origin. The helium in the mud volcano gas is typically crust-derived due to the low R/Ra values of 0.011-0.054. The mud volcano gas is coal-derived since the 13C2 values are all greater than 28‰, and C1/C1-4 and 13C1 values are in accordance with those of natural gas derived from the Lower-Middle Jurassic coal-measures. Therefore, alkane gas from mud volcanoes in the southern Junggar Basin is mainly sourced from the Lower-Middle Jurassic coal-measures. | DAI JinXing WU XiaoQi NI YunYan WANG ZeCheng ZHAO ChangYi WANG ZhaoYun LIU GuiXia | 2012 | Science China Earth Sciences2012，55，3： | 13 |
| 2 | CAS FGOALS-f3-L Model Datasets for CMIP6 Historical Atmospheric Model Intercomparison Project Simulation显示文摘The outputs of the Chinese Academy of Sciences(CAS) Flexible Global Ocean–Atmosphere–Land System(FGOALS-f3-L) model for the baseline experiment of the Atmospheric Model Intercomparison Project simulation in the Diagnostic,Evaluation and Characterization of Klima common experiments of phase 6 of the Coupled Model Intercomparison Project(CMIP6) are described in this paper. The CAS FGOALS-f3-L model, experiment settings, and outputs are all given. In total,there are three ensemble experiments over the period 1979–2014, which are performed with different initial states. The model outputs contain a total of 37 variables and include the required three-hourly mean, six-hourly transient, daily and monthly mean datasets. The baseline performances of the model are validated at different time scales. The preliminary evaluation suggests that the CAS FGOALS-f3-L model can capture the basic patterns of atmospheric circulation and precipitation well, including the propagation of the Madden–Julian Oscillation, activities of tropical cyclones, and the characterization of extreme precipitation. These datasets contribute to the benchmark of current model behaviors for the desired continuity of CMIP. | Bian HE Qing BAO Xiaocong WANG Linjiong ZHOU Xiaofei WU Yimin LIU Guoxiong WU Kangjun CHEN Sicheng HE Wenting HU Jiandong LI Jinxiao LI Guokui NIAN Lei WANG Jing YANG Minghua ZHANG Xiaoqi ZHANG | 2019 | Advances in Atmospheric Sciences2019，36，8： | 12 |
| 3 | Association of COVID-19 Vaccination and Clinical Severity of Patients Infected with Delta or Omicron Variants——China,May 21,2021-February 28,2022显示文摘Summary What is already known about this topic?Compared with the international mRNA and adenovirus-vectored coronavirus disease 2019(COVID-19)vaccines,there is less real-world research data about breakthrough cases in people vaccinated with China-made COVID-19 vaccines.Analyses of clinical outcomes of breakthrough cases will be an important supplement to the clinical trial efficacy and observational effectiveness data of China-made COVID-19 vaccines. | Mingshuang Li Qianqian Liu Dan Wu Lin Tang Xiaoqi Wang Tingting Yan Zhijie An Zundong Yin Geroge F.Gao Fuzhen Wang Hui Zheng | 2022 | China CDC weekly2022，4，14： | 10 |
| 4 | Geochemical Characteristics and Genetic Types of Natural Gas in the Xinchang Gas Field, Sichuan Basin, SW China显示文摘The molecular compositions and stable carbon and hydrogen isotopic compositions of natural gas from the Xinchang gas field in the Sichuan Basin were investigated to determine the genetic types. The natural gas is mainly composed of methane (88.99%–98.01%), and the dryness coefficient varies between 0.908 and 0.997. The gas generally displays positive alkane carbon and hydrogen isotopic series. The geochemical characteristics and gas-source correlation indicate that the gases stored in the 5^(th) member of the Upper Triassic Xujiahe Formation are coal-type gases which are derived from source rocks in the stratum itself. The gases reservoired in the 4^(th) member of the Xujiahe Formation and Jurassic strata in the Xinchang gas field are also coal-type gases that are derived from source rocks in the 3^(rd) and 4^(th) members of the Xujiahe Formation. The gases reservoired in the 2^(nd) member of the Upper Triassic Xujiahe Formation are mainly coal-type gases with small amounts of oil-type gas that is derived from source rocks in the stratum itself. This is accompanied by a small amount of contribution brought by source rocks in the Upper Triassic Ma'antang and Xiaotangzi formations. The gases reservoired in the 4^(th) member of the Middle Triassic Leikoupo Formation are oil-type gases and are believed to be derived from the secondary cracking of oil which is most likely to be generated from the Upper Permian source rocks. | WU Xiaoqi LIU Quanyou LIU Guangxiang WANG Ping LI Huaji MENG Qingqiang CHEN Yingbin ZENG Huasheng | 2017 | Acta Geologica Sinica(English Edition)2017，91，6： | 9 |
| 5 | The scientific connotation of oil and gas formations under deep fluids and organic-inorganic interaction显示文摘As a relatively stable craton block in the earth system, the petroliferous basin is influenced by the evolution of the earth system from the early development environment of source rocks, hydrocarbon formation, and reservoir dissolution to hydrocarbon accumulation or destruction. As a link between the internal and external factors of the basin, deep fluids run through the whole process of hydrocarbon formation and accumulation through organic-inorganic interaction. The nutrients carried by deep fluids promote the bloom of hydrocarbon-generating organisms and extra addition of carbon and hydrogen source, which are beneficial to the development of high-quality source rock and enhancement of the hydrocarbon generation potential. The energy carried by the deep fluid promotes the early maturation of the source rock and facilitates the hydrocarbon generation by activation and hydrogenation in high-mature hydrocarbon sources. The dissolution alteration of carbonate rocks and clastic reservoirs by CO_2-rich deep fluids improves the deep reservoir space, thus extending the oil and gas reservoir space into greater depth. The extraction of deeply retained crude oil by deep supercritical CO_2 and the displacement of CH_4 in shale have both improved the hydrocarbon fluidity in deep and tight reservoirs. Simultaneously, the energy and material carried by deep fluids(C, H, and catalytic substances) not only induce inorganic CH_4 formation by Fischer-Tropsch(F-T) synthesis and 'hydrothermal petroleum' generation from organic matter by thermal activity but also cause the hydrothermal alteration of crude oil from organic sources. Therefore, from the perspective of the interaction of the earth's sphere, deep fluids not only input a significant amount of exogenous C and H into sedimentary basins but also improve the reservoir space for oil and gas, as well as their enrichment and accumulation efficiencies. | Quanyou LIU Dongya ZHU Qingqiang MENG Jiayi LIU Xiaoqi WU Bing ZHOU Qi FU Zhijun JIN | 2019 | Science China Earth Sciences2019，62，3： | 8 |
| 6 | CAS FGOALS-f3-L Model Datasets for CMIP6 GMMIP Tier-1 and Tier-3 Experiments显示文摘The Chinese Academy of Sciences(CAS)Flexible Global Ocean Atmosphere Land System(FGOALS-f3-L)model datasets prepared for the sixth phase of the Coupled Model Intercomparison Project(CMIP6)Global Monsoons Model Intercomparison Project(GMMIP)Tier-1 and Tier-3 experiments are introduced in this paper,and the model descriptions,experimental design and model outputs are demonstrated.There are three simulations in Tier-1,with different initial states,and five simulations in Tier-3,with different topographies or surface thermal status.Specifically,Tier-3 contains four orographic perturbation experiments that remove the Tibetan Iranian Plateau,East African and Arabian Peninsula highlands,Sierra Madre,and Andes,and one thermal perturbation experiment that removes the surface sensible heating over the Tibetan Iranian Plateau and surrounding regions at altitudes above 500 m.These datasets will contribute to CMIP6’s value as a benchmark to evaluate the importance of long-term and short-term trends of the sea surface temperature in monsoon circulations and precipitation,and to a better understanding of the orographic impact on the global monsoon system over highlands. | Bian HE Yimin LIU Guoxiong WU Qing BAO Tianjun ZHOU Xiaofei WU Lei WANG Jiandong LI Xiaocong WANG Jinxiao LI Wenting HU Xiaoqi ZHANG Chen SHENG and Yiqiong TANG | 2020 | Advances in Atmospheric Sciences2020，37，1： | 4 |
| 7 | Epigenetic regulation of phosphodiesterase 4d in restrictive cardiomyopathy mice with cTnI mutations显示文摘Epigenetic regulations play an important role in disease development.In this study,we have investigated epigenetic regulations in restrictive cardiomyopathy mice with cTnI 193 His mutation.Our results demonstrated that phosphodiesterase(PDEs)4d was down-regulated in the heart of these mice.Further studies showed that the epigenetic modifications were associated with enhanced acetylation of histone 3 lysine 4 and lysines 9,whereas tri-methylation of histone 3 lysine 4,were decreased in histones near the PDE4d gene promoter regions.The binding levels of histone transmethylase SMYD1 and histone deacetylase HDAC1 were increased in the gene promoter regions in cTnI193 His transgenic hearts.Using immune-fluorescent labeling we found an evidence of cTnI existence in the nucleus of cardiomyocytes and Western blotting further confirmed that both wild type and mutated cTnI could be detected in the cell nucleus of the hearts.Furthermore,an interaction between cTnI and SMYD1,or cTnI and HDAC1 was observed.Overexpression of the mutated cTnI in cultured cardiomyocytes reduced the expression of PDE4d.Our data suggest that the decrease of PDE4d expression in RCM mice caused by cTnI mutations may be related to epigenetic regulation,i.e.,histone acetylation and methylation,and cTnI might be involved in this procedure via an interaction with HDAC1 and SMAD1 in the hearts. | Weian Zhao Xiaoqi Wu Zhiyuan Wang Bo Pan Lifei Liu Lingjuan Liu Xupei Huang Jie Tian | 2020 | Science China(Life Sciences)2020，63，4： | 4 |
| 8 | Effect of 'Yang-warming and kidney essence-replenishing' herbal paste on cold-related asthma exacerbation显示文摘OBJECTIVE: To observe the effect of 'Yang-warming and kidney essence-replenishing' herbal paste on cold-related asthma exacerbation. METHODS: One hundred and fifty one patients with moderate to severe persistent asthma were randomly divided into a treatment group (n=74) and a control group (n=69). Both groups were given basic treatment according to the Global Initiative for Asthma scheme. The treatment group was also treated with herbal paste in the winter. The frequency of asthma exacerbation, cold and cold-re-lated asthma exacerbation, scores of the asthma control test (ACT), and kidney-deficiency syndrome during the one-year follow-up in each group were recorded. RESULTS: Compared with the control group, the onset frequencies of catching cold, asthma exacerbation, cold-related asthma exacerbation, and kidney-deficiency syndrome score were significantly reduced. There was no significant difference in scores of ACT between the two groups. CONCLUSION: 'Yang-warming and kidney essence-replenishing' herbal paste could reduce cold-related asthma exacerbation. | Binqing Tang Kehua Shi Xiaoqi Li Hongchang Wang Hong Fang Bidan Xiong Yingen Wu | 2013 | Journal of Traditional Chinese Medicine2013，33，4： | 3 |
| 9 | Origin and source of CO_2 in natural gas from the eastern Sichuan Basin显示文摘The CO2 contents of natural gas from the eastern Sichuan Basin were mainly less than 2%,and they were generally large when the H2S contents were over 5%.The natural gas in the eastern Sichuan Basin showed high δ13C1 values uncorrelated with H2S contents,and the oil-associated gas generally displayed carbon isotopic reversal between methane and ethane,whereas the coal-derived gas samples displayed positive series.The δ13C values of CO2 in the natural gas could be divided into two types,one with low values(-24‰--12‰)and the other with high values(-8‰-4‰).The natural gas had low R/Ra values and broad CO2/3He values distinct from the mantle-derived gas,and the CO2 was typical of crustal origin.Natural gas with high δ13CCO2 values is distributed in the north region of the eastern Sichuan Basin,and CO2 in H2S-poor and H2S-free reservoirs was mainly derived from the thermal decomposition of carbonate rocks under Permian magmatism and high heat flow,whereas CO2 in the gas reservoirs with high TSR extent was derived mainly from the dedolomitization of carbonate reservoirs under acidic formation water,and the CO2 of TSR origin generally entered into the secondary calcite.The CO2 in natural gas in the south-central region of the eastern Sichuan Basin,which had been rarely affected by the Emeishan mantle plume,displayed low δ13C values and was of organic origin.Though the natural gas in Wolonghe gas field had experienced TSR,the low reaction extent and weak acidity of formation water could hardly have resulted in the dedolomitization,and therefore CO2 in the natural gas was mainly of TSR origin with low δ13C values. | WU XiaoQi DAI JinXing LIAO FengRong HUANG ShiPeng | 2013 | Science China Earth Sciences2013，56，8： | 3 |
| 10 | InfiniumPurify: An R package for estimating and accounting for tumor purity in cancer methylation research显示文摘The proposition of cancer cells in a tumor sample,named as tumor purity,is an intrinsic factor of tumor samples and has potentially great influence in variety of analyses including differential methylation,subclonal deconvolution and subtype clustering.Infinium-Purify is an integrated R package for estimating and accounting for tumor purity based on DNA methylation Infinium 450 k array data.InfiniumPurify has three main functions getPurity,InfiniumDMC and InfiniumClust,which could infer tumor purity,differential methylation analysis and tumor sample cluster accounting for estimated or user-provided tumor purities,respectively.The InfiniumPurify package provides a comprehensive analysis of tumor purity in cancer methylation research. | Yufang Qin Hao Feng Ming Chen Hao Wu Xiaoqi Zheng | 2018 | Genes & Diseases2018，5，1： | 2 |
| 11 | Recovery of thorium and rare earths from leachate of ion-absorbed rare earth radioactive residues with N1923 and Cyanex■572显示文摘Ion-absorbed rare earth ores radioactive residues(IREORR)are a class of waste residue from the production of rare earth elements(REEs).Because of its radioactive dose,IREORR are usually stored in waste warehouses.IREORR are difficult to be disposed of.However,it contains relatively high concentrations of REEs,which can be considered as a valuable secondary resource.In this paper,a novel process is developed for the separation of thorium(Th)and recovery of REEs from IREORR hydrochloric acid leachate with primary amine N1923 and Cyanex?572,respectively.The effects of sulfate concentration,extractant concentration and pH on N1923 extraction in hydrochloric acid solution were investigated in detail.The results show that the extraction capacity of N1923 can be improved by adding sulfate to the solution and increasing the concentration of N1923.Acidity has little effect on the extraction of Th when pH is higher than 1.As for the stripping,REEs are more easily stripped from loaded organic phase than Th,and nitric acid is a better stripping agent than hydrochloric acid.Combined with the extraction of Cyanex■572 for REEs,a fractional extraction experiment for separating Th and enriching of REEs was performed.The yield of Th is higher than 99.9%and the concentration of REEs is enriched to 183.84 g/L. | Jia Su Xiangguang Guo Yun Gao Shan Wu Ruigao Xu Xiaoqi Sun | 2021 | Journal of Rare Earths2021，39，10： | 2 |
| 12 | Significance of gypsum-salt rock series for marine hydrocarbon accumulation显示文摘With further exploration and research,the gypsum-salts rock series as good caprocks attracted a lot of attention.The gypsum-salt rock series played an important role during migration,preservation and trapping of hydrocarbons.Recently,major breakthroughs have been continuously made in marine petroleum exploration of gypsum-salt rock series in the eastern Ordos Basin,the central Tarim Basin and the western Sichuan Basin in China,and the high-evolution and low-abundance gypsum-salt rock series as hydrocarbon source rocks become possible.Besides research advances in the reservoirecaprock assemblage of gypsum-salt rock series,development and hydrocarbon-generation potential of source rocks in the gypsum-salt rock series were well studied in terms of source-rock development environment and hydrocarbon generation mechanism.Results showed that the gypsum-salt rock series,including high-evolution and low-TOC gypsum-salt rock series in China,could be regarded as good source rocks.This understanding was a breakthrough to previous traditional viewpoint that low-TOC gypsum-salt rock series could not act as effective hydrocarbon sources.The key to understand hydrocarbon-generation mechanism was that abundant and high-quality hydrocarbon-generation materials,large amount of hydrocarbon generation and conversion in geological history,and hydrocarbongeneration materials occurred in the form of carboxylates,were developed in the high-evolution and low-TOC gypsum-salt rock series. | Wenhui Liu Heng Zhao Quanyou Liu Bing Zhou Dianwei Zhang Jie Wang Longfei Lu Houyong Luo Qingqiang Meng Xiaoqi Wu | 2017 | Petroleum Research2017，2，3： | 2 |
| 13 | The first extra-large helium-rich gas field identified in a tight sandstone of the Dongsheng Gas Field,Ordos Basin,China显示文摘Helium gas is a scarce but important strategic resource,which is usually associated with natural gas.Presently,only one extra-large helium-rich gas field has been found in China:the Hetianhe Gas Field in the Tarim Basin.This paper reports a new example,the Dongsheng Gas Field(DGF)in the Ordos Basin.In this study,92 natural gas samples from the DGF were analyzed for helium content and isotope composition using isotope mass spectrometry.The natural gas samples were found to have an average helium content of 0.133%,with 65(70.7%)of the samples having a helium content of 0.1%or more.Based on the proven natural gas reserves of the DGF,the proven geological helium reserves were calculated to be 1.96×10^(8)m^(3),suggesting that it represents the first extra-large helium-rich natural gas reservoir to be hosted in tight sandstone in China.The ^(3)He/^(4)He ratios of 5 natural gas samples from the DGF are within the range of 3.03×10^(−8)–3.44×10^(−8).Therefore,the helium in the gas field is thought to be of typical crustal origin and to have formed in the granitic basement that is rich in uranium and thorium.The accumulation of helium-rich natural gas was controlled by regional tectonic activities.Activity along the fault connecting the reservoir with the basement caused release of the helium gas,which entered the overlying strata along the fault and accumulated with conventional hydrocarbon gas.Based on the structural background and the distribution of helium source rocks in the Ordos Basin,the main helium source rocks with high exploration potential are located in deep strata within the north and middle parts of the basin. | Weilong PENG Quanyou LIU Ying ZHANG Huichong JIA Dongya ZHU Qingqiang MENG Xiaoqi WU Shang DENG Yongsheng MA | 2022 | Science China Earth Sciences2022，65，5： | 2 |
| 14 | Is depression a discon-nection syndrome? Meta - analysis of diffusion tensor imagingstudies in patients with MDD显示文摘 | Yi Liao Xiaoqi Huang Qizhu Wu | 2013 | J Psychiatry Neurosci2013，38，1： | 1 |
| 15 | Disrupted Brain Connectivity Networks in Drug-Naive, First-Episode Major Depressive Disorder显示文摘 | Junran Zhang Jinhui Wang Qizhu Wu Weihong Kuang Xiaoqi Huang Yong He Qiyong Gong | 2011 | Biological Psychiatry2011，，4： | 1 |
| 16 | Comparative study of Co_(3)O_(4)-ZSM-5 catalysts synthesized by different hydrothermal methods for the catalytic oxidation of dichloromethane显示文摘In this work,various Co_(3)O_(4)-ZSM-5 catalysts were prepared by the microwave hydrothermal method(MH-Co_(3)O_(4)@ZSM-5),dynamic hydrothermal method(DH-Co_(3)O_(4)@ZSM-5),and conventio nal hydrothermal method(CH-Co_(3)O_(4)/ZSM-5).Their catalytic oxidation of dichloromethane(DCM)was analyzed.Detailed characterizations such as X-ray diffractometer(XRD),scanning microscopy(SEM),X-ray photoelectron spectroscopy(XPS),Brunauer-Emmett-Teller(BET),H2 temperature-programmed reduction(H2-TPR),temperature-programmed desorption of O_(2)(O_(2)-TPD),temperature-programmed desorption of NH_(3)(NH_(3)-TPD),diffuse reflectance infrared Fourier-transform spectra with NH_(3)molecules(NH_(3)-DRIFT),and temperature-programmed surface reaction(TPSR)were performed.Results showed that with the assistance of microwave,MH-Co_(3)O_(4)@ZSM-5 formed a uniform core-shell structure,while the other two samples did not.MH-Co_(3)O_(4)@ZSM-5 possessed rich surface adsorbed oxygen species,higher ratio of Co^(3+)/Co^(2+),strong acidity,high reducibility,and oxygen mobility among the three Co_(3)O_(4)-ZSM-5 catalysts,which was beneficial for the improvement of DCM oxidation.In the oxidation of dichloromethane,MH-Co_(3)O_(4)@ZSM-5 presented the best activity and mineralization,which was consistent with the characterizations results.Meanwhile,according to the TPSR test,HCl or Cl_(2)removal from the catalyst surface was also promoted in MH-Co_(3)O_(4)@ZSM-5 by their abundant Bronsted acid sites and the promotion of Deacon reaction by Co_(3)O_(4)or the synergistic effect of Co_(3)O_(4)and ZSM-5.According to the results of in situ DRIFT studies,a possible reaction pathway of DCM oxidation was proposed over the MH-Co_(3)O_(4)@ZSM-5 catalysts. | Xiaoqi Fei Shuang Cao Weilong Ouyang Haiqiang Wang Zhongbiao Wu | 2021 | Chinese Chemical Letters2021，32，3： | 1 |
| 17 | Super-ferric Dipole Prototype for Super-FRS of FAIR显示文摘 | Yuan Ping Ma Lizhen H. Leibrock Zhang Xiaoqi Zhang Bin Yao Qinggao Wu Weiyue Wang Qiuliang Wu Wei Wu xi Yang Tongjun Cuo Beilei Han Shaofei He Yuan Zhang Siling | 2009 | 近代物理研究所和兰州重离子加速器实验室年报:英文版2009，，1： | 1 |
| 18 | 大气所全球25 km气候模式CAS FGOALS-f3-H参加CMIP6 HighResMIP数据介绍显示文摘高分辨率模式比较计划(HighResMIP)是CMIP6中新增的模式间比较计划,旨在关注水平分辨率对气候模拟的影响。本文介绍了中国科学院大气物理研究所全球25km FGOALS-f3-H和100km FGOALS-f3-L模式的基本信息,以及参与HighResMIP的试验设计,强迫数据,数据后处理方法等信息。水平分辨率25km的FGOALS-f3-H模式和100km FGOALS-f3-L模式由标准外强迫场驱动,且分别在1950-2014和2015-50时段进行两组协同试验,试验编号分别为'highresSST-present'及'highresSST-future'。模拟和预估数据集包含多种输出频率:1小时平均,3小时平均,6小时瞬时,日平均和月平均等。评估结果表明:水平分辨率的提高能够显著改进模式在热带气旋、日变化和极端降水的模拟性能。相较于全球100km低分辨率的FGOALS-f3-L,全球25km的FGOALS-f3-H能够更好的刻画热带气旋的生命周期和全球降水的日变化主要特征,特别是能够准确再现亚洲夏季风的降水日变化峰值时间。该数据集的发布将大大促进水平分辨率对气候模拟和预估影响的相关研究。 | BAO Qing LIU Yimin WU Guoxiong HE Bian LI Jinxiao WANG Lei WU Xiaofei CHEN Kangjun WANG Xiaocong YANG Jing ZHANG Xiaoqi | 2020 | Atmospheric and Oceanic Science Letters2020，13，6： | 1 |
| 19 | CAS FGOALS-f3-L Large-ensemble Simulations for the CMIP6 Polar Amplification Model Intercomparison Project显示文摘Large-ensemble simulations of the atmosphere-only time-slice experiments for the Polar Amplification Model Intercomparison Project(PAMIP)were carried out by the model group of the Chinese Academy of Sciences(CAS)Flexible Global Ocean-Atmosphere-Land System(FGOALS-f3-L).Eight groups of experiments forced by different combinations of the sea surface temperature(SST)and sea ice concentration(SIC)for pre-industrial,present-day,and future conditions were performed and published.The time-lag method was used to generate the 100 ensemble members,with each member integrating from 1 April 2000 to 30 June 2001 and the first two months as the spin-up period.The basic model responses of the surface air temperature(SAT)and precipitation were documented.The results indicate that Arctic amplification is mainly caused by Arctic SIC forcing changes.The SAT responses to the Arctic SIC decrease alone show an obvious increase over high latitudes,which is similar to the results from the combined forcing of SST and SIC.However,the change in global precipitation is dominated by the changes in the global SST rather than SIC,partly because tropical precipitation is mainly driven by local SST changes.The uncertainty of the model responses was also investigated through the analysis of the large-ensemble members.The relative roles of SST and SIC,together with their combined influence on Arctic amplification,are also discussed.All of these model datasets will contribute to PAMIP multi-model analysis and improve the understanding of polar amplification. | Bian HE Xiaoqi ZHANG Anmin DUAN Qing BAO Yimin LIU Wenting HU Jinxiao LI Guoxiong WU | 2021 | Advances in Atmospheric Sciences2021，38，6： | 1 |
| 20 | Simultaneous determination of chloramphenicol, florfenicol and florfenicol amine in ham sausage with a hybrid chemiluminescent immunoassay显示文摘 | Xiaoqi Tao Haiyang Jiang Xuezhi Yu Jinghui Zhu Xia Wang Zhanhui Wang Lanlan Niu Xiaoping Wu Jianzhong Shen | 2013 | Food Additives & Contaminants: Part A2013，，5： | 1 |
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