安徽省潜山盆地发现恐龙蛋化石          下载免费PDF全文

陈忠良  何情  张蜀康  程小青 《中国地质》2022,49(4):1346-1347

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Comparison of Simulated and Reconstructed Temperature in China during the past 2000 years     

Wang Xiaoqing  Liu Jian  Wang Zhiyuan 《地球科学进展》2015,30(12):1318

Studying climate changes over the past 2 000 years has important scientific significance in exploring climate variability on decadal to centennial timescales, assessing the natural and anthropogenic contribution to the climate warming, and understanding the effects of human activities in the past and future climate changes. Due to the scarcity of observation and uncertainty of reconstruction in this period, climate model is developed as a useful tool for studying paleoclimate.The Community Earth System Model (CESM) is one of the state-of-the-art climate models, but its performance in simulating the temperature in China has not been examined.The temperature datasets of observation/reanalysis (GHCN_CAMS) and reconstructions during the past 2000 years in China were used to examine the performance of CESM. The comparison between the annual average temperatures of GHCN_CAMS reanalysis and simulation showed that the model well reproduced the spatial distributions and upward trend of the annual average temperature in China, and the comparison with reconstructions in five sub-regions of China indicated that the simulation were in good consistent with the average temperature changes of reconstructionson decadal time scales. On the centennial time scale, the average temperature fluctuations of simulation in the regions of China were in accord with reconstructions generally except for Central East and Tibet.There existed three warm periods of simulated temperature variation in China over the past 2000 years, including 0-540AD, 800-1250AD and 1901-2000AD, and two cold periods involving the 551-721AD and 1400-1850AD, which had some discrepancies with reconstructions. And the discrepancies between simulation and reconstructions might be related to uncertainties of the resolution, external forcing and parameterization of the subgrid-scale process in the model.  相似文献   

辉绿岩裂缝对其磁组构的影响          下载免费PDF全文

石林权  沈忠悦  潘小青  李明月  张志亮 《高校地质学报》2015,21(2):223

磁组构是由岩石中磁性矿物定向分布而产生的组构特征,因此磁组构分析是研究岩石组构常用的技术手段,它具有 见效快、灵敏度高、无损样品等特点,近年来得到广泛应用。然而在磁组构研究工作中钻取定向样品或定向手标本时,常 常会遇到天然样品含有裂缝且裂缝中充填大量近地表沉积物和自生矿物。本文针对辉绿岩裂缝充填物对其磁组构结果的影 响程度做了详细研究,选用160个含裂缝的辉绿岩岩芯定向样品,通过对比去除裂缝充填物前后的磁组构变化,发现实验 前后所有样品磁化率大小变化率平均值<1%,磁组构方向变化平均值<1°,因此认为辉绿岩裂缝物质对其磁组构影响甚微。 矿物学和岩石磁学分析表明裂隙充填物主要为石英、长石,以及少量赤铁矿、黄铁矿和绿泥石等表生矿物。而辉绿岩的携 磁矿物主要是亚铁磁性的磁铁矿,其磁化率强度约为同等质量裂缝填充物的30倍,致使辉绿岩中的裂隙充填物对磁组构的 影响很小。  相似文献   

军民测绘标准融合方法研究     

吕玉霞  史曙光  刘平芝  殷小庆  邓国庆 《测绘标准化》2015,(1):1-4

为了统筹军地资源,加强国防建设和经济建设,国家对军民融合的发展战略进行了统一部署。军民测绘标准融合是推动军民测绘事业发展的一项重要内容。通过梳理和对比分析现有军民测绘标准体系及其标准之间的相互关系,提出军民测绘标准融合的工作建议,从而为军民测绘标准融合工作的开展与实施提供参考。  相似文献   

Influence of flow velocity and spatial heterogeneity on DNAPL migration in porous media: insights from laboratory experiments and numerical modelling   总被引：1，自引：0，他引：1  

Fei Zheng  Yanwei Gao  Yuanyuan Sun  Xiaoqing Shi  Hongxia Xu  Jichun Wu 《Hydrogeology Journal》2015,23(8):1703-1718

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人工增雨防雹火箭弹道跟踪系统的研制及初步试验     

董晓波  王晓青  付娇  胡海涛  张权  杨洋  吕峰 《气象》2020,46(6):850-856

由于受到高空风场的影响,人工增雨防雹火箭真实的弹道轨迹和射程与理论弹道值具有不一致性。为增强实施增雨防雹作业的科学性、精准性及其作业效果评估准确性,研制了一套人工增雨防雹火箭播撒作业跟踪系统。该系统分为火箭定位系统和数据传输系统两部分,利用卫星定位模块加上数据传输电台模式将火箭飞行轨迹实时传输至地面。并开展了一次人工增雨防雹火箭弹道跟踪实弹发射试验,发射两发人工增雨防雹测试火箭,除初始阶段4～5 s卫星定位失锁而没有数据外,其余时间所有数据均接收完整。结合高空风场数据对人工增雨防雹测试火箭进行风偏修正后的实际弹道更接近于理论弹道,风偏修正意义明显,有利于增雨防雹火箭精准作业。  相似文献   

2011～2012年冬季欧亚大陆低温严寒事件与平流层北极涛动异常下传的影响   总被引：4，自引：1，他引：3  

兰晓青  陈文 《大气科学》2013,37(4):863-872

利用NCEP-NCAR 再分析资料分析了2011～2012 年冬季发生在欧亚大陆的一次异常低温严寒事件的大气环流演变过程以及可能的成因。这次低温事件,主要出现在2012 年1 月下旬至2 月上旬,持续大约3 周左右,非常强的低温异常覆盖了几乎整个欧洲以及东亚的西伯利亚、蒙古国和我国东北、华北等地。这次低温事件的演变与对流层北极涛动(AO)由正位相转变为负位相的时间相匹配,意味着AO 可能发挥重要作用。进一步分析表明,前期行星波的异常上传导致平流层发生爆发性增温现象,极夜急流减弱,AO 位相首先在平流层由正变负;在2～3 周左右的时间内,平流层AO 异常信号逐渐下传,使得对流层AO 也转为负位相;随后,乌拉尔山阻塞高压异常发展,极区的冷空气不断向南爆发,先后在东亚和欧洲造成剧烈的降温,导致低温严寒事件。因此,考虑平流层环流的异常可能有助于提高欧亚大陆冬季低温严寒事件的预测能力。  相似文献   

Influence of the Kuroshio on hydrography and hydrometeorology in the East China Sea near-shore region     

Shi Maochong  Wang Xiaoqing  Jing Zhenhua 《中国海洋湖沼学报》1989,7(4):312-317

The aim of the study was 1)to determine the relation between the Kuroshio meander and the intensity of the subtropic high pressure over the Pacific Ocean, and then to obtain statistical validity for the observational conclusion that the occurrence time of the Kuroshio meander leads the time of strengthened C-circulation of Europe by one or more years; 2) to develop a method to predict the occurrence time of flood or drought periods in the Changjiang River Valley from the occurrence time of the Kuroshio meander, since there is a close relation between the occurrence time of the drought or flood periods in the Changjiang River Valley and the occurrence time of the strong or weak periods of C-circulation of Europe; and 3) to develop a logical explanation verifiable by remote sensing technique and other means that the warm species phytoplanktons collected recently in the Jiaozhou Bay of Shandong Peninsula in China were carried there by a new warm current branch of the Kuroshio in the East China Sea. This paper was presented at the Conference on Western Pacific Circulation Influence on the China Seas in Qingdao, 1987, and approved for publishing as a monograph.  相似文献   

帕隆藏布流域然乌-培龙段冰湖溃决危险性评估     

柳金峰  程尊兰  陈晓清 《山地学报》2012,(3):369-377

西藏帕隆藏布流域内发育了我国境内最大的海洋性冰川群,冰湖星罗棋布,是遭受冰湖溃决危害的典型区域。以帕隆藏布流域然乌-培龙段的冰湖为研究对象,在分析其环境背景的原则上,通过遥感解译,分析研究区冰湖的分布现状;在基于指标容易获取的基础上,从冰川特征、冰湖特征和下游沟道特征3个类别选取了8个冰湖溃决危险性评估指标,并利用模糊物元可拓性理论对研究区的冰湖溃决危险性进行综合评估。通过评估,研究区130个冰湖中,高度危险的有18个,占总数的13.85%;中度危险的有36个,占总数的27.69%;低度危险的有76个,占总数的58.46%;高度危险的冰湖主要集中分布在然乌-松宗区段内。  相似文献   

面向山地灾害动态过程仿真的地形三维建模与可视化     

叶健  陶和平  陈锦雄  陈晓清 《山地学报》2012,(2):195-200

基于山地灾害动态过程仿真需要的考虑,并针对该动态过程仿真时渲染数据量过大所造成的实时性较差的问题,提出了利用改进的三角形二叉树LOD算法实现地形三维建模与可视化的方法。算法对山地地形数据进行了分层和分块的预处理,用三角形二叉树表示地形网格,并结合视点和局部地形的粗糙程度,动态的载入所需的地形块和释放无用的地形块,使得内存中的地形数据维持在一定范围内。实验结果表明;在对地形渲染不失真的前提下,本方法能够有效地提高地形绘制的效率,可应用到大规模山地地形的三维建模与可视化中去,为整个山地灾害的动态过程仿真奠定了良好的基础。  相似文献