On the Existence of Benthic Storms
- https://doi.org/10.1080/14029251.2015.1113053How to use a DOI?
- equatorial flows, eddy viscosity, stratification
We study a model for the wind-induced current field of the Pacific ocean in order to demonstrate that currents in the surface layer are carried down to the deepest regions above the abyssal sea floor, which indicates the existence of the phenomenon of comparably strong currents in bottom regions as a result of wind-stress forces at the surface, also known as benthic storms.
- © 2015 The Authors. Published by Atlantis Press and Taylor & Francis
- Open Access
- This is an open access article distributed under the CC BY-NC 4.0 license (http://creativecommons.org/licenses/by-nc/4.0/).
Cite this article
TY - JOUR AU - Ronald Quirchmayr PY - 2021 DA - 2021/01 TI - On the Existence of Benthic Storms JO - Journal of Nonlinear Mathematical Physics SP - 540 EP - 544 VL - 22 IS - 4 SN - 1776-0852 UR - https://doi.org/10.1080/14029251.2015.1113053 DO - https://doi.org/10.1080/14029251.2015.1113053 ID - Quirchmayr2021 ER -