Response of the Equatorial Countercurrent to the Subtropical Atmosphere
- 28 September 1973
- journal article
- other
- Published by American Association for the Advancement of Science (AAAS) in Science
- Vol. 181 (4106), 1244-1245
- https://doi.org/10.1126/science.181.4106.1244
Abstract
The strength of the equatorial countercurrent of the North Pacific and associated variations in sea surface temperatures at its eastern extremity off Central America are related to the zonal wind flow in the remote subtropical atmosphere with lags of as much as 8 months between wind and temperature.Keywords
This publication has 1 reference indexed in Scilit:
- Teleconnections in the Equatorial Pacific OceanScience, 1973