Abstract
Based upon temperature and salinity observations and upon the movements of three parachute drogues, the mean flow of water through Bay of Plenty is shown to be from west to east and to be part of the East Auckland Current. © Crown 1986.
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CITATION STYLE
APA
Ridgway, N. M., & Greig, M. J. N. (1986). Water movements in Bay of Plenty, New Zealand. New Zealand Journal of Marine and Freshwater Research, 20(3), 447–453. https://doi.org/10.1080/00288330.1986.9516164
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