2) tropical Indian Ocean dipole
热带印度洋偶极子
1.
The third generation ocean model developed by the State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics (LASG) has been improved, and the integrated results of the improved model from January, 1959 to December, 1998 are analyzed to study the physical mechanism of occurrence, development and disappearance of the tropical Indian Ocean dipole.
分析了该模式1959年1月—1998年12月的40a积分结果,以此研究热带印度洋偶极子发生、发展和消亡的物理机制。
3) TIO monopole
热带印度洋单极
4) tropical Indian Ocean
热带印度洋
1.
Responses of East Asian winter and summer monsoons to autumn sea surface temperature anomalies in tropical Indian Ocean;
东亚冬夏季风对热带印度洋秋季海温异常的响应
2.
Connection Between Tropical Indian Ocean Dipole Event and Subtropical Indian Ocean Dipole Event;
热带印度洋偶极子事件和副热带印度洋偶极子事件的联系
3.
Study on the Heat Budget and Meridional Circulation in the Tropical Indian Ocean;
热带印度洋热收支与经向环流的研究
5) Indian Ocean Dipole
印度洋偶极子
1.
Influence of Eurasian Snow Cover in Spring on Indian Ocean Dipole;
欧亚春季雪盖对印度洋偶极子的影响
2.
Relationship between the Indian Ocean Dipole and Autumn Rainfall in China;
印度洋偶极子与中国秋季降水的关系
3.
Indian Ocean Dipole is able to influence occurrence of El Nino to some degree,but the occurrence and development of El .
结果表明:热带印度洋偶极子指数超前热带太平洋Nino3指数2月时相关最大,印度洋单极子指数滞后Nino3指数3~4月时相关最大。
6) Indian Ocean Dipole
印度洋偶极模
1.
The Meridian Pattern of Summer Rainfall in 2004 and Its Relationship with Indian Ocean Dipole;
2004年夏季经向型雨带及其与印度洋偶极模异常海温的关系
补充资料：“质子-电子偶极-偶极”质子弛豫增强
“质子-电子偶极-偶极”质子弛豫增强
物理学术语。原子核外层中不成对的电子质量小，但磁动性很强，可使局部磁场波动增强，促使氢质子弛豫加快，从而使T1和T2缩短，这种效应即为PEDDPRE。过渡元素和镧系元素大部分在d和f轨道有多个不成对电子，所以其离子往往具有PEDDPRE，可用来作顺磁性对比剂，如钆(Gd)。Gd在外层有7个不成对电子，具有很强的顺磁性。
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