AUTOSAL8400B型实验室盐度计及其应用

AUTOSAL 84 0 0 B型实验室盐度计是一种高精度的测量海水电导率 (换算盐度 )的仪器 ,其测量精度可达到± 0 .0 0 2 psu,被广泛应用于海洋环境测量以及现场和实验室仪器定标等领域。它的高精度测量特性在深海大洋中显得尤其重要。本文将详细介绍该盐度计的性能 ,以及操作步骤和使用技巧等 ,以便充分展示和发挥该盐度计的作用     

格罗夫山地无地面控制卫星影像数字制图和地貌、蓝冰及陨石分布分析

中国南极考察队第一次去东南极格罗夫山地进行考察之前 ,为了保证考察路线选择、导航和考察任务顺利进行 ,在无任何地面实地测量数据的情况下 ,采用星上参数处理并制成了1∶ 1 0万比例尺彩色卫星影像地图。通过对卫星影像的判读 ,对该地区的地形、地貌、蓝冰和陨石分布特点作了初步的分析和探讨 ,并勾画出可能有陨石分布的地区     

利用Argo剖面浮标分析上层海洋对台风“布拉万”的响应

In situ observations from Argo profiling floats combined with satellite retrieved SST and rain rate are used to investigate an upper ocean response to Typhoon Bolaven from 20 through 29 August 2012. After the passage of Typhoon Bolaven, the deepening of mixed layer depth(MLD), and the cooling of mixed layer temperature(MLT) were observed. The changes in mixed layer salinity(MLS) showed an equivalent number of increasing and decreasing because the typhoon-induced salinity changes in the mixed layer were influenced by precipitation, evaporation, turbulent mixing and upwelling of thermocline water. The deepening of the MLD and the cooling of the MLT indicated a significant rightward bias, whereas the MLS was freshened to the left side of the typhoon track and increased on the other side. Intensive temperature and salinity profiles observed by Iridium floats make it possible to view response processes in the upper ocean after the passage of a typhoon. The cooling in the near-surface and the warming in the subsurface were observed by two Iridium floats located to the left side of the cyclonic track during the development stage of the storm, beyond the radius of maximum winds relative to the typhoon center. Water salinity increases at the base of the mixed layer and the top of the thermocline were the most obvious change observed by those two floats. On the right side of the track and near the typhoon center when the typhoon was intensified, the significant cooling from sea surface to a depth of 200×104 Pa, with the exception of the water at the top of the thermocline, was observed by the other Iridium float. Owing to the enhanced upwelling near the typhoon center, the water salinity in the near-surface increased noticeably. The heat pumping from the mixed layer into the thermocline induced by downwelling and the upwelling induced by the positive wind stress curl are the main causes for the different temperature and salinity variations on the different sides of the track. It seems that more time is required for the anomalies in the subsurface to be restored to pretyphoon conditions than for the anomalies in the mixed layer.     

卓越工程师能力考核探讨与分析——以“GIS原理课程设计”为例

实践教学是理工科学生实践能力培养的关键一环。本文探讨了"GIS原理课程设计"实践课程的考核方式,对武汉大学遥感科学与技术专业的特色进行了分析,设计了一套面向卓越GIS工程师能力培养的考核模式,并对考核方式进行了分析。本文提出的考核模式改进了课程设计的考核形式,对相关专业的培养模式革新有一定的参考意义。     

利用Argo资料研究2001-2004年期间西北太平洋海洋上层对热带气旋的响应

利用Argo剖面浮标观测资料,对2001-2004年11月期间西北太平洋热带气旋经过后海洋上层的响应作了分析研究.结果显示,热带气旋经过后,55.6%的观测剖面其混合层深度会加深,范围在0-60m,并且在气旋过后5d内更为明显;由于混合加剧,大约有77.8%的观测剖面其混合层温度会下降,最多达5℃;61.1%的混合层盐度会下降,平均降盐约0.12;表层流速增大的占54%,平均增大30cm·s,表层流速的变化与风速的大小呈正相关,相关系数仅为0.06;混合层内温度变化与热带气旋风速呈负相关,相关系数为-0.15;混合层温度下降有明显的右偏现象,在气旋路径右侧50-150km处,温度下降尤为明显,而混合层盐度在气旋路径两侧的变化基本呈对称状分布;混合层深度在气旋路径右侧加深更为明显,在右侧100 150km范围内达到最大;混合层深度的变化与气旋经过前混合层的初始深度呈明显的负相关,相关系数达-0.42.     

全球Argo实时海洋观测网全面建成

文中较详尽地介绍了全球Argo实时海洋观测网建设现状,以及Argo资料在相关领域应用研究中所取得的成果,揭示了Argo资料广阔的应用研究前景。但要实现国际Argo计划的最终目标,尚需各参与国不遗余力。