Abstract
A series of drogued floats was released at the entrance to Peel Inlet and the limit of their penetration into the inlet was found to be 1.75 � 0.15 km. We show that this compares favourably with a model based on the upstream propagation of a frictionless tide and use this model to discuss the exchange of the inlet waters due to barometric variations.
Subject
Ecology,Aquatic Science,Ecology, Evolution, Behavior and Systematics,Oceanography
Cited by
4 articles.
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