IOD:印度洋偶极子
“印度洋偶极子”(Indian Ocean Dipole,简称IOD)是描述热带印度洋海温东西反相振荡现象的专业术语。这一概念在气候研究、海洋学和气象预测等综合领域被广泛使用,缩写形式“IOD”便于学术交流与日常书写,有助于提升相关讨论与文献撰写的效率。
Indian Ocean Dipole具体释义
Indian Ocean Dipole的英文发音
例句
- However, the pure IOD ( Indian Ocean Dipole(IOD) ) and pure ENSO are difficult to excite teleconnection wave train in the Southern Hemisphere, which further confirms the interaction between them.
- 而单纯IOD和单纯ENSO均难以在南半球对流层激发出遥相关波列,进一步证实了两者共同作用的影响。
- Influence of Eurasian Snow Cover in Spring on Indian Ocean Dipole(IOD)
- 欧亚春季雪盖对印度洋偶极子(IOD)的影响
- Teleconnection Pattern between Indian Ocean Dipole(IOD) Mode Events and Southern High Latitude Climate Anomalies with the Corresponding Dynamic View; The descent warms the air and its relative humidity accordingly drops.
- 印度洋海温偶极子型振荡和南半球高纬度气候异常之间的遥相关及动力机制解释这种下沉使空气变暖,其相对温度相应下降。
- Interdecadal change of the relationship between tropical Indian Ocean dipole and anomalous summer climate in China
- 热带印度洋偶极子(IOD)与中国夏季年际气候异常关系的年代际变化
- Simulated Structural Changes of Asian Summer Monsoon Circulation in Association with Indian Ocean Dipole(IOD) SSTAs
- 亚洲夏季风环流结构与热带印度洋偶极型海温异常
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