Development of the Subsurface Currents of the Northern Somali Current Gyre from March to July 1979
- 1 August 1980
- journal article
- other
- Published by American Association for the Advancement of Science (AAAS) in Science
- Vol. 209 (4456) , 593-595
- https://doi.org/10.1126/science.209.4456.593
Abstract
Measurements from March to July 1979 by current meters moored between the shelf and the deep sea from 5° to 8°N show that there was shallow ( < 150-meter) coastward and northward circulation between 6° and 8°N long before the onset of the southwest monsoon. After the onset, a powerful coastward flow developed offshore around 6°N, branching into northward and southward flows at the continental rise while the current deepened to more than 250 meters. There seemed to be a separate circulation on the shelf with some counterflow to offshore. All current records show that there were strong fluctuations with periods of 3 to 6 days.Keywords
This publication has 7 references indexed in Scilit:
- Evolution of Sea Surface Temperature in the Somali Basin During the Southwest Monsoon of 1979Science, 1980
- Subsurface Circulation in the Somali CurrentScience, 1980
- Somali Current: Evolution of Surface FlowScience, 1980
- Eddies off the Somali Coast during the southwest monsoonJournal of Geophysical Research: Oceans, 1979
- Measurements in the Source Region of the Somali Current during the Monsoon ReversalJournal of Physical Oceanography, 1978
- Evidence for baroclinic instability of the Norwegian CurrentJournal of Geophysical Research, 1977
- A Numerical Model of the Somali CurrentJournal of Physical Oceanography, 1976