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A new interpolation method for Antarctic surface temperature

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Progress in Natural Science:Materials International 2009年第12期19卷 1843-1849页

作者： Yetang Wang~(a,b),Shugui Hou~(b,c,*) a Monitoring Centre of Ocean Environment of Shandong Province,Yantai 2.4006,china b State key {2. of Cryospheric Science,Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences,Lanzhou 73000,china c moe,key laboratory for coast and island development,school of geographic and oceanographic Sciences,nanjing university,nanjing 2.0093,china [a]Monitoring Centre of Ocean Environment of Shandong Province Yantai 264006 China [b]State key laboratory of Cryospheric Science Cold and Arid Regions Environmental and Engineering Research Institute Chinese Academy of Sciences Lanzhou 73000 China [c]moe Key Laboratory for Coast and Island Development School of Geographic and Oceanographic Sciences Nanjing University Nanjing 210093 China

We propose a new methodology for the spatial interpolation of annual mean temperature into a regular grid with a geographic resolution of 0.01°for Antarctica by applying a recent compilation of the Antarctic temperature data.A multiple linear regression model of the dependence of temperature on some geographic parameters(i.e.,latitude,longitude,and elevation) is proposed empirically,and the kriging method is used to determine the spatial distribution of regional and local deviations from the temperature calculated from the multiple linear regression *** modeled value and residual grids are combined to derive a high-resolution map of surface air temperature. The performance of our new methodology is superior to a variety of benchmark methods(e.g.,inverse distance weighting,kriging, and spline methods) via cross-validation *** simulation resembles well with those distinct spatial features of surface temperature,such as the decrease in annual mean surface temperature with increasing latitude and the distance away from the {2. line; and it also reveals the complex topographic effects on the spatial distribution of surface temperature.

关键词： Surface temperature DEM Antarctica

Helium isotope investigation on magnetic reversal boundaries of loess-paleosol sequence at Luochuan, central Chinese Loess Plateau

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Chinese Science Bulletin 2007年第17期52卷 2407-2412页

作者： DU XueQing1,6, WANG YongHong2. REN JianGuo3, YE XianRen4 & LU HuaYu5,1 1 State key laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an 710075, {2. 2.College of Marine Geosciences, Ocean university of {2., Qingdao 2.6003, {2. 3 National Natural Science Foundation of {2., Beijing 100085, {2. 4 Lanzhou Research Center for Petroleum and Natural Gas Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences, Lanzhou 730000, {2. 5 key laboratory of coast and {12. development, school of geographic and oceanographic Sciences, nanjing university, nanjing 2.0093, {2. 6 Graduate university of Chinese Academy of Sciences, Beijing 100049, {2. State key laboratory of Loess and Quaternary Geology Institute of Earth Environment Chinese Academy of Sciences Xi''an 710075 China

Extraterrestrial particles have higher 3He/4He ratios than those of terrestrial sediments ( > 100 Ra versus < 0.03 Ra, where Ra is the 3He/4He ratio normalized to the atmospheric value of 1.4×10?6). The inter- planetary dust particles (IDPs), which are very rich in 3He, continuously bombard the Earth and can accumulate in deposits. IDPs sedimentation rate changes can significantly influence 3He concentration in the Earth surface sediments. Since IDPs are not easy to detect in terrestrial deposits, measuring helium isotopes is a helpful approach to examine changes in IDPs. Helium concentration and helium isotopic composition magnetic substances and the quartz particles were examined for helium concen- tration and helium isotopic ratio. Results show that the 3He/4He ratio and the 3He concentrations of the magnetic substances are clearly higher than those of the bulk samples and the quartz particles, and, the 3He/4He ratio of the extracted magnetic substances is also higher than that of the average level of the Earth’s crust. The higher helium content in the magnetic fractions can be explained by an influx of IDPs.

关键词：中国黄土高原古土壤氦同位素行星际尘埃颗粒反方向磁化

The application of geographic information technology to coastal geomorphology

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Acta Oceanologica Sinica 2009年第5期28卷 49-57页

作者： GUO Wei LI Shuheng ZHU Dakui school of Human Settlements and Civil Engineering Xi＇an Jiaotong University Xi＇an 710049 China Department of Computer Sciences Xi＇an Jiaotong University Xi＇an 710049 China Department of Urban and Resources Sciences Northwest University Xi＇an 710032 China Faculty of Environmental Sciences University of Waterloo Waterloo N2L3G1 Canada key laboratory of {2. ＆ island development of Ministry of Education Nanjing University Nanjing 210093 China

With the development of modern oceanic observation technologies, coastal survey data have been experiencing a substantial growth. The integration management of the data from different disciplines, different sources and different formats has become a major research field in coastal geomorphology by using geographic Information System （GIS）. This paper puts forward a new methodology framework of GIS techniques in coastal ocean geomorphology, including data acquisition, process, analysis, and representation. It focuses on some major GIS techniques to study the land-ocean interaction mechanism, such as spatial analysis, submarine topography model and three-dimension （3D） visualization, and apply its result to coastal urban planning, harbor site selection and geomorphology environment about coral reef and islands on the continental shelf. The case studies cover the whole coastal ocean to serve the social community, economical development and diplomatic rights for decision-making all round in the coastal zone. The research shows clearly that the application of coastal multi-source geospatial platform has changed the traditional coastal geomorphology science dramatically from its research scope, fields and methods, however, as made clear in this paper, extracting accurate information from remote sensing data and GIS databases for coastal geomorphological applications is a nontrivial challenge that requires the combined knowledge and skills of information scientists and geomorphologists.

关键词： coastal geomorphology geographic information system (GIS) spatial analysis threedimensional visualization

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江苏海洋环境与沿海经济发展

水资源保护 2003年第6期19卷 19-21页

作者：朱大奎南京大学海岸与海岛开发教育部重点实验室江苏南京210093

根据多年对江苏省海岸研究,提出江苏淤泥质平原岸外古长江三角洲受潮流辐射改造,形成岸外海底沙脊群及沙脊之间的潮流通道,经多种方法研究测算,得出其中主要的潮流通道具有稳定性、良好的地质基础、古地理条件及强大的动力条件的结论,... 详细信息

根据多年对江苏省海岸研究,提出江苏淤泥质平原岸外古长江三角洲受潮流辐射改造,形成岸外海底沙脊群及沙脊之间的潮流通道,经多种方法研究测算,得出其中主要的潮流通道具有稳定性、良好的地质基础、古地理条件及强大的动力条件的结论,可建设为深水航道深水港。同时分析了洋口港将是江苏沿江开发的延伸,对江苏经济发展意义重大。

关键词：江苏海洋环境海岸线辐射沙洲洋口港深水航道

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用活有孔虫分布指示三亚汊道外港潮流格局

海洋学报 1999年第1期21卷 71-79页

作者：尤坤元朱晓东 SchaferCT ColeFE 南京大学海岸与海岛开发国家试点实验室南京210093 南京大学海岸与海岸开发国家试点实验室南京210093 GeologicalSurveyofCanada BedfordInstituteofOceanography

由因子分析得知，海南岛三亚湾汊道外港海底分布有四个主因子活有孔虫群，它们分别代表海湾内水体、湖冲出半盐水水体、湾外内陆架水体及内陆架与海湾水相混的过渡水体．这些水体在潮汐作用下的运动、相互混合，可由各水体的有孔虫指示... 详细信息

由因子分析得知，海南岛三亚湾汊道外港海底分布有四个主因子活有孔虫群，它们分别代表海湾内水体、湖冲出半盐水水体、湾外内陆架水体及内陆架与海湾水相混的过渡水体．这些水体在潮汐作用下的运动、相互混合，可由各水体的有孔虫指示．由每个主因子因子得分最高的三个属种百分含量之和等值线图所指示的外港潮流循环格局，与海洋学研究所得的结果相当一致．利用有孔虫指示潮汐汊道潮流格局尚属首次尝试，这方法对海岸开发分析泥沙运动、污染物排放等有实践意义．

关键词：活有孔虫群潮流循环格局主因子分析海南沉积

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东海北部底层冷水及双跃层初析

海洋与湖沼 1989年第1期20卷 75-86页

作者：苏育嵩李凤岐马鹤来钱清瑛青岛海洋大学

本文着重探讨东海北部区域底层冷水的形成和季节变化过程,指出北部冷水系冬季黄海沿岸水南下向东海输送低温水,并与外海高盐水混合变性形成的,它具有明显的移动规律。阐述了黄海沿岸水沿陆架下沉与黑潮次-中层水爬升的关系及其对北部冷... 详细信息

本文着重探讨东海北部区域底层冷水的形成和季节变化过程,指出北部冷水系冬季黄海沿岸水南下向东海输送低温水,并与外海高盐水混合变性形成的,它具有明显的移动规律。阐述了黄海沿岸水沿陆架下沉与黑潮次-中层水爬升的关系及其对北部冷水的影响。本文还分析了济州岛南部区域双跃层现象的类型及其波状结构的成因。发现上,下跃层之间存在着“跃层间环流”,它将导致双扩散的发生和有利于双跃层的维持。

关键词：冷却水双跃层

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1985年9月的吕宋海峡黑潮及其输送

热带海洋 1988年第2期 13-19页

作者：郭忠信方文东中国科学院南海海洋研究所

吕宋海峡黑潮的主流轴大致在12.°E附近,其西边界可达12.°E,东边界在12.°E之东。由于受吕宋冷涡之影响,在巴林搪海峡西口,黑潮流速达最高值(超过2.n)。在吕宋海峡的南部和北部,黑潮的体积输送分别为43×10~6m~3/s和32.10~6m~3/s。黑... 详细信息

吕宋海峡黑潮的主流轴大致在12.°E附近,其西边界可达12.°E,东边界在12.°E之东。由于受吕宋冷涡之影响,在巴林搪海峡西口,黑潮流速达最高值(超过2.n)。在吕宋海峡的南部和北部,黑潮的体积输送分别为43×10~6m~3/s和32.10~6m~3/s。黑潮有一个向西的11—12.10~6m~3/s的净体积输送,它贡献给进入南海的“黑潮南海分支”。黑潮的一个分支在2.°N与黑潮主流脱离,通过12.°E向西进入南海,流速达1.6kn,体积输送为11—12.10~6m~3/s。吕宋海峡右侧的暖涡较往常靠东北,其影响深度可达12.0m以深。

关键词：黑潮分支主流冷涡低涡吕宋海峡暖涡