1) South China Sea and its adjacent area
南海及邻域
1.
Based on the 18a 3h Tbb information during 1980 ~ 1997 provided by Japanese Meteorological Research Institute, the area statistics distribution characteristics of convection activity in South China Sea and its adjacent area is studied by way of statistic Tbb≤36℃ occurring frequency, providing reference basis for forecast.
利用日本气象研究厅提供的1980～1997年共18a3h一次的Tbb资料,采用统计Tbb≤-36℃出现频率的方法,研究了南海及邻域对流活动的区域统计分布特征,为预报提供参考依据。
2) South China and Adjacent Marginal Seas
华南及相邻边缘海域
3) South China Sea and its adjacent areas
南海及邻区
1.
Upper Triassic-Cretaceous sediment distribution and hydrocarbon potential in South China Sea and its adjacent areas;
南海及邻区中生代(晚三叠世—白垩纪)地层分布特征及含油气性对比
4) East China Sea
东海及邻域
1.
Inversion research for gravity and synthetical interpretation of two profiles in the area of East China Sea and its adjacency;
东海及邻域的两条剖面地球物理反演与综合解释
5) Shanghai and its adjacent offshore region
上海及邻近海域
1.
A database of earthquakes and neo-tenctonic activities in Shanghai and its adjacent offshore region is constructed on the GIS software platform MapGIS 6.
基于MapGIS构建上海及邻近海域地震和新构造活动数据库。
6) East China Sea and its vicinity
东海及邻近海域
补充资料：超导电性的局域和非局域理论（localizedandnon-localizedtheoriesofsuperconductivity）
超导电性的局域和非局域理论（localizedandnon-localizedtheoriesofsuperconductivity）
伦敦第二个方程（见“伦敦规范”）表明，在伦敦理论中实际上假定了js(r)是正比于同一位置r的矢势A(r)，而与其他位置的A无牵连；换言之，局域的A(r)可确定该局域的js(r)，反之亦然，即理论具有局域性，所以伦敦理论是一种超导电性的局域理论。若r周围r'位置的A(r')与j(r)有牵连而影响j(r)的改变，则A(r)就为非局域性质的。由于`\nabla\timesbb{A}=\mu_0bb{H}`，所以也可以说磁场强度H是非局域性的。为此，超导电性需由非局域性理论来描绘，称超导电性的非局域理论。皮帕德非局域理论就是典型的超导电性非局域唯象理论。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条