Oxygen-carbon dioxide-nutrients relationships in the Southeastern Region of the Bering Sea     

Saúl Alvarez-Borrego  Louis I. Gordon  Lynn B. Jones  P. Kilho Park  Ricardo M. Pytkowicz 《Journal of Oceanography》1972,28(2):71-93

The vertical distribution of density, salinity, temperature, dissolved oxygen, apparent oxygen utilization, nutrients, preformed phosphate, pH, alkalinity, alkalinity: chlorinity ratio, in situ partial pressure of carbon dioxide, and percent saturation of calcite and aragonite, for the Southeastern Bering Sea, is studied and explained in terms of biological and physical processes. Some hydrological interactions between the Bering Sea and the North Pacific Ocean are explained. The horizontal distribution of dissolved oxygen at 2000 and 2500 m depths, throughout the Bering Sea, indicates that deep water is flowing from the Pacific, through the Kamchatka Strait, and then northward and eastward in the Bering Sea. Based on the dissolved oxygen distribution we estimate roughly that it takes 20 years for the deep waters to move from the Kamchatka Strait to the Southeastern part of the eastern basin. The surface concentration of nutrients is higher in the Bering Sea than in the North Pacific Ocean, probably because of upwelling and intense vertical mixing in the Bering Sea. A multivariable regression analysis of dissolved oxygen as a function of phosphate concentration and potential temperature was applied for the region where the potential temperature-salinity diagram is straight, and the confidence interval of the PO₄ coefficient, at the 95% probability level, was found consistent with theRedfield biochemical oxidation model. The calcium carbonate saturation calculations show that the Bering Sea is supersaturated with aragonite in the upper 100 m, and with calcite in the upper 200 m. Below these depths seawater is undersaturated with respect to these two minerals.  相似文献   

Solar rotation rate from stable sunspot tracings     

Atila Özgüç  Mualla Sağlamsaatçi 《Astrophysics and Space Science》1989,153(2):345-349

Positions of sunspots between 1966 and 1976 as observed at Kandilli Observatory were used to determine the differential rotation of the Sun. A total of 202 sunspot groups which were E, F, G, H, and J-types were chosen, and a least-squares solution was calculated with their daily rotations. A gradient difference was found between the two hemispheres of the Sun.  相似文献   

On the connection between terrestrial and riparian vegetation: the role of storage partitioning in water‐limited catchments          下载免费PDF全文

Saúl Arciniega‐Esparza  José Agustín Breña‐Naranjo  Peter A. Troch 《水文研究》2017,31(2):489-494

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珠江口盆地白云南洼珠海组陆架边缘三角洲沉积体系演化     

舒梁锋  张向涛  张忠涛  张丽丽  雷胜兰  高中亮  韩霄  于飒 《沉积学报》2022,40(3):825-837

珠江口盆地白云南洼珠海组发育陆架边缘三角洲,其不仅是深水区勘探重要的油气储层类型,也是沉积地质学和石油地质学研究的热点。根据高精度三维地震资料,应用三级层序格架内等时地层切片技术,对珠江口盆地白云南洼珠海组陆架边缘三角洲的沉积结构和平面演化开展了详细研究。研究表明,区内存在北部和西北部两个物源方向的陆架边缘三角洲物源供给体系,进而形成连续4期三角洲前积复合体,各期次通过解剖三角洲前积结构和叠置样式可细分为2~5套三角洲前积体,地震上表现为切线斜交型和S型反射结构。不同物源供给体系下的三角洲进积和加积速率差异明显,根据陆架边缘三角洲的演化阶段可划分为初始形成期、发展期和稳定期三个阶段。初始形成期为珠海组四段中晚期,三角洲垂向上均表现为进积,平面上北部物源供给的陆架边缘三角洲形成面积小,西北部物源供给的三角洲面积相对大;发展期为珠海组三段,三角洲垂向上进积和加积均存在,陆架边缘三角洲沉积厚度达到最大,平面上北部物源供给的陆架边缘三角洲—深水扇体系发育一定规模,西北部物源供给的陆架三角洲前缘发育陆架条带砂脊;稳定期为珠海组二段和一段,三角洲垂向结构表现为先进积后加积,三角洲前缘规模变大,陆坡水道和深水扇最为发育。珠海组时期陆架边缘三角洲形成演化受双物源差异供给、相对海平面的先升后降和构造活动的相对稳定共同控制。北部物源供给的珠海组陆架边缘三角洲—深水陆坡沉积体系可作为区内最有利的油气勘探目标。  相似文献   

苏尼特右旗1976—2006年沙尘天气的观测分析     

陈云峰  李丽儒  萨如拉 《内蒙古气象》2009,(3):10-12

基于苏尼特右旗1976—2006年的沙尘天气观测资料,对苏尼特右旗沙尘天气的年际变化、月际变化等进行了分析,结果表明,1976—2006年苏尼特右旗沙尘天气呈波动性减少趋势,月平均沙尘天气日数的波动性,与月平均最大风速和月平均大风日数成正相关。扬沙天气出现日数最多,沙尘暴天气次之,浮尘天气出现日数最少。造成沙尘天气除本地沙尘源外,上游沙尘的输送也是产生沙尘天气的重要原因。影响苏尼特右旗沙尘天气的主要天气形势为冷锋和蒙古气旋。  相似文献   

Contourlet变换和Tsallis熵的多源遥感图像匹配   总被引：1，自引：0，他引：1  

吴一全  陈飒 《遥感学报》2010,14(5):899-910

提出了一种利用Contourlet变换、Tsallis熵和改进粒子群优化的多源遥感图像匹配算法。在分别对参考图像和目标图像进行Contourlet分解的基础上,以基于Tsallis熵的互信息量作为相似性度量准则,利用改进的带极值扰动的简化粒子群优化算法对低分辨率的遥感图像进行匹配操作,逐级上推,最终实现全分辨率情况下多源遥感图像的匹配。实验结果表明,与常用的遥感图像匹配算法相比,该算法匹配精度高,稳健性好,且运算量大幅减少。  相似文献   

地质图形处理系统设计   总被引：5，自引：0，他引：5  

萨贤春  门桂珍 《煤田地质与勘探》1997,25(2):21-24

介绍了地质图形计算机处理系统的系统功能、系统结构、图形数据库结构以及图形生成与编辑;讨论了在开发地质图形计算机辅助设计或绘图系统时,应如何体现专业特点,如何在数据中表达地质现象的地层和构造意义,如何在地质模型建立中融入专业人员的地质背景知识,以及怎样设计出实际有效的地质图形处理软件系统等问题。   相似文献   

Comparison of the QBO and F10.7 Solar Flux Effects on Total Mass Density     

Selçuk Sağır  Ramazan Atıcı 《Geomagnetism and Aeronomy》2018,58(7):841-845

Geomagnetism and Aeronomy - The comparison of the Quasi Biennial Oscillation (QBO) and F10.7 solar flux effects on Total Mass Density (TMD) obtained from NRLMSIS-00 model for 90 km altitude of...  相似文献   

The Relationship between Dst,IMF-Bz and Collision Parameters for O+ + N2 → NO+ + N Reactive Scattering in the Ionosphere     

Selçuk Sağir  Yaşar  Mehmet  Atici  Ramazan 《Geomagnetism and Aeronomy》2019,59(8):1003-1008

Geomagnetism and Aeronomy - The kinetic theory is particularly suitable and convenient to calculate the collision parameters in the ionospheric medium. In this study, the mean free path (λ)...  相似文献   

Review of Chinese atmospheric science research over the past 70 years: Synoptic meteorology     

Meng  Zhiyong  Zhang  Fuqing  Luo  Dehai  Tan  Zhemin  Fang  Juan  Sun  Jianhua  Shen  Xueshun  Zhang  Yunji  Wang  Shuguang  Han  Wei  Zhao  Kun  Zhu  Lei  Hu  Yongyun  Xue  Huiwen  Ma  Yaping  Zhang  Lijuan  Nie  Ji  Zhou  Ruilin  Li  Sa  Liu  Hongjun  Zhu  Yuning 《中国科学:地球科学(英文版)》2019,62(12):1946-1991

Synoptic meteorology is a branch of meteorology that uses synoptic weather observations and charts for the diagnosis,study,and forecasting of weather.Weather refers to the specific state of the atmosphere near the Earth's surface during a short period of time.The spatial distribution of meteorological elements in the atmosphere can be represented by a variety of transient weather phenomena,which are caused by weather systems of different spatial and temporal scales.Weather is closely related to people's life,and its development and evolution have always been the focus of atmospheric scientific research and operation.The development of synoptic meteorology is closely related to the development of observation systems,dynamical theories and numerical models.In China,observation networks have been built since the early 1950 s.Up to now,a comprehensive meteorological observation systembased on ground,air and space has been established.In particular,the development of a new generation of dense radar networks,the development of the Fengyun satellite series and the implementation of a series of large field experiments have brought our understanding of weather from large-scale environment to thermal dynamics,cloud microphysical structure and evolution characteristics of meso and micro-scale weather systems.The development of observation has also promoted the development of theory,numerical model and simulation.In the early days,China mainly used foreign numerical models.Lately,China has developed numerical model systems with independent intellectual property rights.Based on the results of high-resolution numerical simulations,in-depth understanding of the initiation and evolution mechanism and predictability of weather at different scales has been obtained.Synoptic meteorology has gradually changed from an initially independent development to a multidisciplinary approach,and the interaction between weather and the change of climate and environment has become a hot and frontier topic in atmospheric science.This paper reviews the important scientific and technological achievements made in China over the past 70 years in the fields of synoptic meteorology based on the literatures in China and abroad,from six aspects respectively including atmospheric dynamics,synoptic-scale weather,typhoon and tropical weather,severe convective weather,numerical weather prediction and data assimilation,weather and climate,atmospheric physics and atmospheric environment.  相似文献