全球海面简单高效实现技术研究

在数字地球上模拟海面,是数字地球可视化以及海洋仿真的重要需求之一。利用屏幕细分自适应算法对海面网格进行计算,并在GPU中处理其网格点相应的坐标转换和计算,大大减少了对CPU的占用率。在可视范围内,对海面网格进行实时的优化处理,提高了效率,满足数字地球相关仿真系统对海面仿真的需求。在解决海洋和陆地分离显示上,提出了一种简单的设置透明度的实现方法,既满足了现实需要,也大大提高了使用效率。     

钦州湾茅尾海周年环境因子及浮游植物群落特征

2010年1月、3月、6月及9月,共设14个调查站位对钦州湾茅尾海海域的环境因子及浮游植物的种类组成、优势种类、数量分布和群落多样性进行调查分析。结果茅尾海海区营养盐中POi—P值为0．01～0．07mg／dm^3,DIN值为0．16～O．78mg／dm^3,POi—P值和DIN值均有超4类海水水质标准现象。浮游植物共鉴定出82属,262种,优势种类16种,年平均丰度为6．29×10^4cells／L,生物多样性指数的年平均值为3．87。2010年茅尾海浮游植物种类和数量都比较丰富,种类的季节变化呈现由冬至秋减少的趋势,数量的季节变化比较明显,春季最低,平均密度仅为3．28×10^4cells／L,夏季最高,平均密度为9．25×10^4cells／L。     

阿根廷陆架坡海域的鱿鱼渔业现状及我国鱿钓业实践与发展

阿根廷陆架坡海域的鱿鱼资源是世界上最重要的国际性渔业对象之一。本文根据近年来有关国家机构和专家学者的研究和调查,对这一海域鱿鱼种群结构、洄游与分布和渔业状况进行综述,并结合舟山兴业公司鱿钓渔船的试生产实践,就今后我国鱿钓业在该海域的发展提出建议。     

拉布拉多海一年平整冰厚度SAR反演算法

在利用实测一年平整冰厚数据和同步全极化RADARSAT-2 SAR影像、全面分析不同SAR极化参数对海冰厚度敏感度的基础上,发现Alpha角最高;从理论上证实利用两者相关性反演冰厚的可行性,将所得经验方程用于冰厚反演,其结果与实测数据吻合较好;与现有常用方法的反演结果进行对比表明,新方法误差较小;Alpha角可以用于一年平整冰厚度反演,证明全极化SAR海冰信息反演冰厚确有优势。     

如何重构大传统——兼论《米诺王权与太阳女神》的方法论

当下文学人类学意义上的大传统指的是前文字时代的传统,服务于重构中国文化观这一现实诉求。如何利用非书写资料阐释中国版图内不同区域的文化在同一时段内的互动关系,继而重构该时期的文化传统,成为当前文学人类学大小传统理论建构的关键问题。《米诺王权与太阳女神》一书通过解读米诺时期金戒指上图像的意义,还原了米诺时期地中海文化共同体的本原面目,为中国文学人类学关于大传统关键问题的探讨提供了跨学科研究范式。     

基于ISCCP卫星资料的南中国海云量特征分析

为较准确地了解掌握可以反映南中国海天气和气候特征的云量分布演变特征,利用1999年1月至2009年12月的ISCCP卫星云量资料,通过物理量特征提取、对比分析等方法,研究了南中国海总云量及高、中、低云量的分布演变特征,以及其与其他海域各季节云量季节性变化特征。结果表明:南中国海低云量四季中均表现为由海区向沿岸递减,总云量和中、高云量夏秋季高于冬春季,低云量则相反。对于不同海域的云量细节特征要依据各季节大气和海洋环流变化来细致区分,这样有助于在掌握规律基础上有效制作海域上空云的预报。     

南海北部陆缘黏土矿物组合特征与地质意义

采用沉积矿物分析方法对南海北部九口探井渐新世—中新世沉积物进行系统的黏土矿物分析.结果表明:南海北部沉积物黏土矿物组成随时间及空间呈现规律性变化,黏土矿物伊/蒙转化深度具有自北向南逐步变浅的规律,与地温梯度升高变化趋势基本一致,这种黏土矿物伊/蒙转化的变化规律反映了南海北部洋陆过渡地壳减薄,莫霍面抬升,热流值升高的趋势.通过黏土矿物组合演变特征与热流变化趋势的相关关系,可以预测区域性温度场变化规律,加深对南海北部洋陆过渡地壳厚度变化的认识.     

东海风暴潮数值预报模式参数的敏感性分析

设计两个模拟台风,以北上型台风路径对东海风暴潮数值预报模式进行敏感性分析。采用高桥水文站的风暴潮计算结果,分析了台风引起的最大增水及出现时间对台风中心经度、纬度、中心气压和最大风圈半径的敏感程度。结果表明,最大风暴增水的数值对台风中心纬度并不敏感,对台风中心气压、最大风圈半径有一定的敏感,但也并不显著,而对台风中心经度最为敏感。最大增水出现的时间则对台风中心气压、最大风圈半径并不敏感,对台风中心经度和纬度较为敏感,尤其是纬度最为显著。在设计的两种模拟台风中,最大增水出现的时间表现出对台风中心纬度以及台风移速更为敏感.     

Magnetic characteristics and its environmental implications of core YSJD-86GC sediments from the southern South China Sea

Sediments of core YSJD-86GC （referred to as 86GC） collected from the southern South China Sea were selected for environmental magnetic studies. Combined with the published chronological framework, sediment magnetic properties were revealed for the study area since the MIS3 stage. The rock magnetic results indicate that low-coercivity magnetite is the main magnetic mineral within the sediments. Also, a certain amounts of hematite are present. The King plot and Day plot, which reflect the magnetic particle size, show that fine-grained pseudo-sin- gle-domain phase magnetic particles dominate the magnetic minerals in the sediments. Comparison of magnetic parameters and geochemical indicators show that magnetic properties of core 86GC sediments reflect a terrigenous input. Simultaneously, magnetic characteristics of the stud- ied sediment are influenced by the quantity of terrigenous sediment input, oxidation-reduction conditions of the provenance area, and the transportation environment and distance. Sea level fluctuation caused by global climate change was the main factor for variation in concentration of magnetic minerals and magnetic particle size of thestudied core sediments. Thus, variation of sediment magnetic properties in the study area can be used as an indirect indicator of sea level fluctuation.     

Millennial climate changes since MIS 3 revealed by element records in deep-sea sediments from northern South China Sea

High resolution elemental MD05-2903 from the northern South records in core China Sea were obtained from XRF scanning and grain size and mineral component analyses. The K/Ti curve reveals climate changes since MIS 3 on a millennial scale, representing one of the best such records so far from deep-sea sediments of the South China Sea. When compared our K/Ti record with other climate records from high latitude ice cores and from East Asia stalagmites, variations in the K/Ti record show some typical saw-shaped features of rapid climate changes in the Northern Hemisphere. Grain size analysis reveals a close relationship between variations in K/Ti and in the fine end-member grain size. XRD analysis confirms that high K/Ti layers were dominated by K-rich weathering minerals, especially illite, while low K/Ti layers contain low illite but high abundance of Ti-rich heavy minerals. Therefore, the K/Ti record reflects changes in the input and deposition of fine weathering minerals and heavy minerals in the northern South China Sea region during stadials and interstadials. These elemental changes were largely con- trolled by variations in rainfall, erosion, and fluvial trans- portation induced by East Asia Monsoon.