中高层大气环流模式的初步评估与敏感性分析          下载免费PDF全文

Zhaoyang Chai  Minghua Zhang  Qingcun Zeng  He Zhang  Jiangbo Jin  Jinbo Xie  Ting You 《大气和海洋科学快报》2021,14(2):35-41

提高大气环流模式的模式顶层高度对中高层大气(如平流层准两年振荡)的准确模拟至关重要.本研究将IAP大气环流模型(IAP-AGCM)延伸至中层大气顶(～0.01 hPa,～80 km)并提高垂直方向分辨率(91层),发展了一个中高层大气环流模型(IAP-AGCML91).结果表明,与低层模式相比,该中高层大气模式在整体上显著减小了平流层尤其是上平流层的冷偏差.研究发现这种改善与两种机制有关:与低层模式相比,高层模式模拟的短波加热更大,极区平流层附近的经向涡动热通量更大.上述结果表明,垂直分辨率和模式顶层高度对IAP-AGCML91的气候模拟有重要影响.  相似文献   

Field investigation of force and displacement within a strata slope using a real-time remote monitoring system     

Jiangbo Xu  Heng Li  Ke Du  Changgen Yan  Xu Zhao  Wu Li  Xinzhuang Xu 《Environmental Earth Sciences》2018,77(15):552

Research on monitoring and forecasting technology for slope stability is important for ensuring railway operation. This paper presents field investigation of force and displacement within a strata slope using a real-time remote monitoring system. Based on the interactions of the landslide body, the landslide bed and the monitoring anchor of slope, the mechanical principle of relative movement between the landslide body and the landslide bed can be found. This paper puts forward stress data obtained from a monitoring anchor as the main criterion for landslide stability. The stress will change continually inside the slope mass before the occurrence of a landslide. When the sliding force is larger than the anti-sliding force, deformation and landslides will occur; thus, the change in stress occurs before the change in displacement. In this study, the internal stress, deep displacement and surface strain of a railway slope were measured by a real-time remote-monitoring system, and a vibration metre was installed on the surface of the railway slope to study the influence of the train vibration load on the stability of the slope. The monitoring results are synthetically analysed temporally and spatially, then a railway slope forecasting model is proposed. According to the railway slope field application, the forecasting model makes successful predictions.  相似文献   

东太平洋克拉里昂-克里帕顿断裂带WPC1101沉积柱样磁性地层及沉积环境     

王海峰  韩玉林  朱克超  易亮  邓希光  刘广虎  任江波 《吉林大学学报(地球科学版)》2014,44(6):1892-1905

对采自东太平洋CC区西部的WPC1101重力活塞柱样进行了岩石磁学、古地磁极性地层及古生物地层年代学研究工作。等温剩余磁化强度（IRM）、磁滞回线和反向场退磁曲线测试结果表明,沉积物中的磁性矿物主要为磁铁矿,仅在柱状样底部存在少量赤铁矿/针铁矿。340~350 cm发育的埋藏结核层,标志着一处沉积间断的存在;60~336 cm发育上新世晚期的硅藻化石Cosinodiscus nodulifer,但古地磁极性地层缺失上新世-第四纪的2r反极性时;0~60 cm见第四纪标准化石Pseudoenuotia doliolus、Spongaster tetras,且顶部缺失1正极性时。综合对比古生物地层学、磁性地层学以及邻近区域地层学特征,认为该柱状样记录了从晚渐新世至第四纪的沉积历史,期间存在晚渐新世至早上新世、上新世晚期至第四纪早期及第四纪晚期3个时期的沉积间断,上述沉积间断的形成可能是南极底流的形成与增强、CCD界面抬升及海底侵蚀作用增强共同控制的结果。  相似文献   

华北板块北缘中段姚五沟岩体锆石U-Pb定年、地球化学特征及其与区域构造演化的关系          下载免费PDF全文

林智炜  吴堑虹  奚小双  夏艳菊  刘飚  蒋江波 《地质找矿论丛》2019,34(1):104-116

内蒙古太仆寺旗地区的姚五沟岩体位于华北板块北缘中段,主要岩石类型为花岗斑岩。岩体LA-ICP-MS锆石U-Pb测年结果为141.6 Ma±1.3 Ma(MSWD=0.78),形成于晚侏罗世。岩石化学特征显示岩体具高硅富碱的特征,A/CNK=0.93～1.07,为准铝质-弱过铝质,属高钾钙碱性系列。稀土配分模式呈右倾"V"字型,Eu负异常较显著(δEu=0.30～0.43),轻重稀土分异明显(w(La)N/w(Yb)N=34.04～48.59)。微量元素表现出富集Rb、Th、K等大离子亲石元素,亏损Ba、Sr和Nb、Ta、Ti、P等高场强元素,具有较高的10000×w(Ga)/w(Al)值(2.85～2.92)和w(Zr+Nb+Ce+Y)值(537.80×10~(-6)～584.10×10~(-6));表明其属A型花岗岩,由下地壳部分熔融而来,并伴随少量幔源组分参与,形成于非造山伸展环境。与研究区内的后淖S型花岗岩(255.8 Ma±1.6Ma,晚二叠世)和白旗A型花岗岩(134.6Ma±1.1Ma,晚侏罗世)的地球化学特征对比,发现由晚二叠世到晚侏罗世,岩浆源区由上地壳的泥质岩部分熔融转换为下地壳部分熔融,并伴随少量幔源组分参与,其大地构造背景由陆-陆碰撞环境转换为非造山伸展环境。  相似文献   

富稀土磷酸盐及其在深海成矿作用中的贡献   总被引：1，自引：0，他引：1  

任江波  何高文  朱克超  邓希光  刘纪勇  傅飘儿  姚会强  杨胜雄  孙卫东 《地质学报》2017,91(6):1312-1325

中国最近几年对中北太平洋海域开展了系统调查,在中太平洋海盆新发现了稀土含量高达2000×10~(-6)的富稀土泥。深海泥样品稀土与各主要氧化物相关图解中,∑REY与P_2O_5含量始终保持良好的相关性。在太平洋各沉积物柱状样中,∑REY随着P2O5变化非常敏感。如果将P_2O_5含量高于0.25%的样品剔除,深海泥的∑REY不高于400×10~(-6),指示了磷对稀土元素的控制。海洋磷酸盐能够继承海水的负Ce异常及高Y/Ho比值特征,深海泥样品具有相似特征,且表现为稀土含量越高,其稀土配分模式越接近磷酸盐。酸淋滤实验显示,滤液中萃取出大部分的P及∑REY,且∑REY与P含量具有良好的正相关关系。无论∑REY高低,滤液稀土配分均呈现出显著的负Ce异常;而难溶残留物的∑REY普遍较低,且无负Ce异常特征。根据12组滤液中PO_4~(3-)与∑REY,估算出深海泥中的磷酸盐具有的∑REY含量范围为9495×10~(-6)~28287×10~(-6),这与深海泥中生物磷灰石的稀土含量和稀土模式均吻合。综上所述,我们认为深海泥中的磷酸盐主要以富稀土磷酸盐的形式存在,其稀土含量远高于深海泥中的铁锰氧化物和铝硅酸,因此磷含量的变化对于深海泥的稀土含量和模式影响至关重要。相较于碳酸盐沉积环境下容易形成贫稀土的磷块岩,深海环境下的化学沉积以及有机P的成岩作用容易形成富稀土磷酸盐。  相似文献   

Research on Dynamic of Terrestrial System of China: Academic Logic and Synthetic Scheme   总被引：2，自引：0，他引：2  

Wu Shaohong  Gao Jiangbo  Dai Erfu  Zhao Dongsheng  Yin Yunhe  Yang Lin  Zheng Jingyun  Pan Tao  Yang Qinye 《地球科学进展》2017,32(6):569-576

Land surface, the environment where human survive and develop, is a synthesis formed with multi-scaled and multi-process interactions between natural factors. The terrestrial system, which is the core study field of physical geography, can be defined as the land surface synthesis with spatially ordered distribution and temporally dynamic balance. In the past century, natural variations and human activities have had profound influences on land surface. How they drove the changed interactions between land surface factors, and further altered the land surface pattern, are the frontier and basis for global change and geography studies. Based on the brief review of research on terrestrial system at home and abroad, the paper summarized the existing difficulties and problems, and then proposed the academic logic for studies of dynamic of terrestrial system. The research should be conducted following the logic of elements, patterns and dynamic, with emphasis on themes of processes and feedback, variation in regions and terrestrial system. At last, the synthetic scheme was designed for research on dynamic of terrestrial system. Aimed at innovation of regionalization methodology and detection on driving mechanism of dynamic of terrestrial system, the following four aspects should be included: Changes and interaction mechanism of key factors (i.e. water, soil, climate and plant) and their spatial-temporal variation; Quantifying the influences of factor interactions on regionalization formation and conversion; Quantified assessment on changing tendency and magnitude of land surface pattern under global climate change; Accomplishment of dynamic land surface pattern at different past and future stages. Correspondingly, the technical route should combine bottom-up and top-down methodologies, with field survey, earth observation, station monitoring and mathematical simulation to build the comprehensive database. Conducting research on dynamic of terrestrial system can be helpful for developing theory of integrated physical geography, deepening cognition on dynamic land surface pattern, and providing scientific basis for regional sustainable resources utilization and countermeasure establishment of climate change adaptation.  相似文献   

A Study of Chromium Adsorption on Natural Goethite Biomineralized with Iron Bacteria   总被引：1，自引：0，他引：1  

SUN Zhenya ZHU Chunshui HUANG Jiangbo GONG Wenqi CHEN Hesheng MU Shanbin 《《地质学报》英文版》2006,80(4):597-603

Goethite, especially biogenic goethite, has high specific surface area and great capacity for the adsorption of many contaminants including metal ions and organic chelates. Chromium is a redox actively toxic metal ion that exists as either Cr^Ⅲ or Cr^Ⅵ in nature, and as such it is essential to understand its behavior of adsorption on natural goethite mineralized by iron bacteria, as Gallionella and Leptothrix in water body. The adsorption of Cr^3＋ and Cr^Ⅵ on naturally biomineralized goethite is studied in this paper. The results show that both Langmuir and Freundlich adsorption isothermal models are able to accurately describe the adsorption of these two ions. Investigation of SEM/EDS, TEM/EDS indicates that the two ions do not adsorb homogeneously on goethite owing to the different microstructures of goethite, and that the microspherical goethite has a greater adsorption capacity for chromium ions than the helical one. XPS data show that redox reaction of chromium on the surface of biomineralized goethite takes place in the adsorption of both Cr^3＋ and Cr^Ⅵ. The CrvI adsorbed on biogoethite is much easier to transform into CrIII than the oxidization of Cr^Ⅲ on the bio-goethite.  相似文献   

湖南锡田钨锡多金属矿田燕山期NE向断层演化历史及其成矿意义          下载免费PDF全文

刘飚  吴堑虹  李欢  奚小双  孔华  曹荆亚  蒋江波  林智炜  吴经华  梁伟 《地球科学》2021,46(1):43-58

为了确定湖南锡田矿田燕山期NE向断层演化历史、蚀变特征及与钨锡成矿关系本文调查了矿田内燕山期断层野外宏观特征,对断层中充填石英脉进行了显微鉴定、阴极发光、含矿元素分析,结果显示:(1)断层以NE60°～70°平行分布于茶汉盆地南北两侧,均倾向茶汉盆地,断层的陡倾、棱角状角砾及梳状石英等指示了断层的张性性质;(2)断层经...  相似文献   

CAS-ESM2.0 Model Datasets for the CMIP6 Flux-Anomaly-Forced Model Intercomparison Project(FAFMIP)   总被引：3，自引：3，他引：0  

Jiangbo JIN  He ZHANG  Xiao DONG  Hailong LIU  Minghua ZHANG  Xin GAO  Juanxiong HE  Zhaoyang CHAI  Qingcun ZENG  Guangqing ZHOU  Zhaohui LIN  Yi YU  Pengfei LIN  Ruxu LIAN  Yongqiang YU  Mirong SONG  Dongling ZHANG 《大气科学进展》2021,38(2):296-306

The second version of the Chinese Academy of Sciences Earth System Model(CAS-ESM2.0)is participating in the Flux-Anomaly-Forced Model Intercomparison Project(FAFMIP)experiments in phase 6 of the Coupled Model Intercomparison Project(CMIP6).The purpose of FAFMIP is to understand and reduce the uncertainty of ocean climate changes in response to increased CO2 forcing in atmosphere-ocean general circulation models(AOGCMs),including the simulations of ocean heat content(OHC)change,ocean circulation change,and sea level rise due to thermal expansion.FAFMIP experiments(including faf-heat,faf-stress,faf-water,faf-all,faf-passiveheat,faf-heat-NA50pct and faf-heat-NA0pct)have been conducted.All of the experiments were integrated over a 70-year period and the corresponding data have been uploaded to the Earth System Grid Federation data server for CMIP6 users to download.This paper describes the experimental design and model datasets and evaluates the preliminary results of CAS-ESM2.0 simulations of ocean climate changes in the FAFMIP experiments.The simulations of the changes in global ocean temperature,Atlantic Meridional Overturning Circulation(AMOC),OHC,and dynamic sea level(DSL),are all reasonably reproduced.  相似文献   

CAS-ESM2.0 Model Datasets for the CMIP6 Ocean Model Intercomparison Project Phase 1(OMIP1)   总被引：2，自引：2，他引：0  

Xiao DONG  Jiangbo JIN  Hailong LIU  He ZHANG  Minghua ZHANG  Pengfei LIN  Qingcun ZENG  Guangqing ZHOU  Yongqiang YU  Mirong SONG  Zhaohui LIN  Ruxu LIAN  Xin GAO  Juanxiong HE  Dongling ZHANG  Kangjun CHEN 《大气科学进展》2021,38(2):307-316

As a member of the Chinese modeling groups,the coupled ocean-ice component of the Chinese Academy of Sciences’Earth System Model,version 2.0(CAS-ESM2.0),is taking part in the Ocean Model Intercomparison Project Phase 1(OMIP1)experiment of phase 6 of the Coupled Model Intercomparison Project(CMIP6).The simulation was conducted,and monthly outputs have been published on the ESGF(Earth System Grid Federation)data server.In this paper,the experimental dataset is introduced,and the preliminary performances of the ocean model in simulating the global ocean temperature,salinity,sea surface temperature,sea surface salinity,sea surface height,sea ice,and Atlantic Meridional Overturning Circulation(AMOC)are evaluated.The results show that the model is at quasi-equilibrium during the integration of 372 years,and performances of the model are reasonable compared with observations.This dataset is ready to be downloaded and used by the community in related research,e.g.,multi-ocean-sea-ice model performance evaluation and interannual variation in oceans driven by prescribed atmospheric forcing.  相似文献