甘肃武威市一次局地大到暴雨天气成因分析

利用常规天气图、FY-2D卫星云图、单站地面资料、NCEP再分析物理量场资料,对2013年8月6日发生在甘肃武威市对流性强降雨天气成因进行了诊断分析。结果表明:强降雨是在一定的大尺度环流背景下高低层天气系统共同作用下发生的,地面气象要素的剧烈变化是强对流天气能量的释放过程;湿度条件和水汽在本地辐合为大到暴雨提供了充沛的水汽;高层辐散、低层辐合以及强烈的上升气流是大到暴雨发生的动力条件;强烈的不稳定能量和不稳定层结是对流增强、雨强较大的必要条件;对流云团的发展和加强是降雨强度较大的直接原因。     

吉林省敦化市团北区锡钼矿找矿远景浅析

吉林省敦化市团北区锡、钼矿体赋存于花岗斑岩体的西侧和东侧内接触带中,斑岩体西部以银、锡矿化为主,东部以钼矿化为主,矿化类型为斑岩型。矿体受北东向主断裂及其分支断裂所控制,区内北东向断裂为主要的控岩、控矿、导矿构造,北西向为主要的容矿构造。区内地球物理化学异常特征明显,深部及外围找矿潜力巨大。     

潞西团坡厂铁锌多金属矿成因

矿体产于印支期黑云角闪花岗闪长岩与寒武系(未分,∈?)变质岩接触带,F1压扭性断裂控制矿体的形态和展布。成因类型为热液接触交代一矽卡岩型铁锌矿。     

新疆哈图-包古图金铜矿集区锆石年龄及成矿特点

晚古生代,新疆西准噶尔地区发生了强烈的构造-岩浆活动和广泛的金、铜成矿作用,形成了哈图-包古图大型金铜矿集区。锆石SHRIMP U-Pb年龄测量表明,含矿闪长岩体形成于312.3±2.2Ma～332.0±2.8Ma,矿集区岩浆活动及其成矿作用发生在石炭纪。哈图-包古图矿集区成矿作用有4个显著特点:(1)地幔流体活动强烈;(2)构造应力转化快速;(3)拉斑系列和钙碱性系列岩浆成矿;(4)多种矿化类型集中发育等。哈图-包古图矿集区发育石英脉型-蚀变岩型金矿床、斑岩型铜矿床和同期的石英脉型-蚀变岩型金矿床以及热液脉型铜金矿床的成矿系列。     

基于Argo网格产品资料的台湾以东海域海温场结构与温跃层特征分析

基于2005年1月~2009年12月中国Argo实时数据中心发布的Argo网格化产品,对台湾以东海域的表层和深层海温进行了分析,证实了日本南部海域存在北太平洋副热带模态水,提出暖水团概念,分析了其成因和垂直结构,并利用SODA(Simple Ocean Data Assimilation)数据和WOA09(World Ocean Atlas 2005)数据对暖水团进行验证。揭示出台湾以东海域各层次温度大面分布大体呈3个模态特征,并依此将台湾以东海域分为热带、副热带和温带三个海区;对各海域截取断面图,对其温跃层进行分析,归纳出永久性温跃层和季节性温跃层在垂直方向上的分布和季节性变化,并对其成因进行了讨论。     

黄海冷水团海域微型异养鞭毛虫与细菌的弱耦合关系

A study was carried out to investigate the grazing pressure of heterotrophic nanoflagellates(HNF) on bacteria assemblages in the Yellow Sea Cold Water Mass(YSCWM) area in October, 2006. The results show that the HNF abundance ranges from 303 to 1 388 mL-1, with a mean of 884 mL-1. The HNF biomass is equivalent to 10.6%–115.6% of that of the bacteria. The maximum abundance of the HNF generally occurred in the upper 30 m water layer, with a vertical distribution pattern of surface layer abundance greater than middle layer abundance, then bottom layer abundance. The hydrological data show that the YSCWM is located in the northeastern part of the study area, typically 40 m beneath the surface. A weak correlation is found between the abundances of HNF and bacteria in both the YSCWM and its above water layer. One-way ANOVA analysis reveals that the abundance of HNF and bacteria differs between inside the YSCWM and in the above water mass. The ingestion rates of the HNF on bacteria was 8.02±3.43 h-1 in average. The grazing rate only represented 22.75%±6.91% of bacterial biomass or 6.55%+4.24% of bacterial production, implying that the HNF grazing was not the major factor contributing to the bacterial loss in the YSCWM areas.     

The roles of different mechanisms related to the tide-induced fronts in the Yellow Sea in summer

In summer, the Yellow Sea Cold Water Mass （YSCWM） is a stable water mass of low temperature lying at the bottom of the central Yellow Sea （YS）. It is fringed by some typical tidal fronts, which separate deep, stratified water on the offshore side from the well-mixed, shallow water on the inshore side. Three striking fronts--Subei Bank Front （SBF）, Shandong Peninsula Front （SPF）, and Mokpo Front （MKF; a front off the southwestern tip of the Korean Peninsula）--have been iden- tified by various studies from both satellite observations and model results. Tide plays an important role in the formation and maintenance of these fronts. However, it is still a matter of debate as to the roles these two kinds of mechanisms of upwelling and tidal mixing play, and how importance they are in the maintenance processes of the above three fronts. Basing a nested high-resolution model HYCOM （the Hybrid Coordinate Ocean Model）, this study focuses on the different mechanisms of tidal effects on the thermal fronts in the YS in summertime. Through comparative experiments with and without tidal forcing, the results indicate that the MKF is mainly driven by tide-induced upwelling. For the SPF, tidal mixing is the dominant factor, when lower cold water is stirred upwards along the sloping topography of the western YS. Meanwhile, the combined effect of upwelling and tidal mixing is the main cause of the formation of the SBF. Diagnostic analysis of thermal balance shows that horizontal nonlinear advection induced by strong tidal currents also contributes to the thermal balance of frontal areas.     

大数据环境下道路场景高时空分辨率众包感知方法EI北大核心CSCD

道路场景作为人类发展演变中最重要、最复杂、最典型的载体之一,是道路基础设施与活动行为共同构成的综合体,链接和构建“人地关系”。道路场景感知从二维抽象简略到三维精细丰富、从静态过去式向动态现在时发展,成为智慧城市、智能交通、无人驾驶的关键技术支撑,是我国新型城镇化战略、交通强国战略的核心技术保障。本文立足于时空交通大数据,提出基于道路场景静态基础设施“形”和动态活动行为“流”的高时空分辨率道路场景感知方法。该方法从静态路网“形”角度,以“点-线-面-体”等要素为研究脉络,构建高精度道路地图众包感知的理论体系;在活动行为“流”感知上,突破传统的点模式分析局限,发展了道路网络空间活动流的时空建模与多尺度分析方法。本文揭示了静态基础设施“形”结构与动态活动行为“流”模式交互作用下的道路场景演化规律,形成以“形”控“流”、借“流”定“形”、“形”“流”叠置的高时空精度道路场景众包感知理论体系,为智慧城市、智能交通的发展提供核心技术与数据支撑。     

河南省庙咀钒矿地质特征及成矿浅析

庙咀钒矿是近年查明的一个中型钒矿床。钒矿床地处荆紫关—师岗复向斜南翼,矿体赋存于下寒武统水沟口组底部硅质岩和泥岩中,严格受控于地层及岩性。矿石类型主要为黏土岩型及条带状硅质岩型两种,钒主要以离子吸附和类质同象赋存于黏土矿物中。矿床成因为滨海-浅海沉积型层控矿床。     

夏季黄海冷水团海域的丙烯酸分布与海洋环境因子和叶绿素a变化之间的关系

海水中主要含硫化合物β-二甲基巯基丙酸内盐(DMSP)降解可产生丙烯酸(AA)和活性气体二甲基硫(DMS)。2011年8月对黄海冷水团海域的AA及相关参量的分布特征进行了研究。结果表明,该海域表层海水中AA的浓度为0~0.208μmol/L,平均值为(0.081±0.075)μmol/L。AA的高值区出现在海域的东南部,可能是受到长江冲淡水的影响。AA的浓度总体上呈现出由南到北递增的趋势,与Chl-a较为一致,表明该海域的AA主要是由DMSP裂解产生的。表层海水中AA与温度表现出明显的负相关性。AA的垂直分布表现为:中层底层表层,这可能是产生AA的浮游植物与消耗AA的细菌共同作用的结果。海域中AA浓度与DMSP或DMS无明显的相关性。AA浓度远高于DMS,AA/DMS平均为106∶1,初步估算出DMSP降解产生的AA约为66.5%。AA/Chl-a平均为126.6 mmol/g,比DMSP/Chl-a高1个数量级,比DMS/Chl-a高2个数量级。