100 Years of the Ocean General Circulation

The central change in understanding of the ocean circulation during the past 100 years has been its emergence as an intensely time-dependent, effectively turbulent and wave-dominated, flow. Early technologies for making the difficult observations were adequate only to depict large-scale, quasi-stead...

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Main Authors: Wunsch, Carl Isaac, Ferrari, Raffaele
Other Authors: Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
Format: Article
Language:English
Published: American Meteorological Society 2021
Online Access:https://hdl.handle.net/1721.1/129466
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author Wunsch, Carl Isaac
Ferrari, Raffaele
author2 Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
author_facet Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
Wunsch, Carl Isaac
Ferrari, Raffaele
author_sort Wunsch, Carl Isaac
collection MIT
description The central change in understanding of the ocean circulation during the past 100 years has been its emergence as an intensely time-dependent, effectively turbulent and wave-dominated, flow. Early technologies for making the difficult observations were adequate only to depict large-scale, quasi-steady flows. With the electronic revolution of the past 50+ years, the emergence of geophysical fluid dynamics, the strongly inhomogeneous time-dependent nature of oceanic circulation physics finally emerged. Mesoscale (balanced), submesoscale oceanic eddies at 100-km horizontal scales and shorter, and internal waves are now known to be central to much of the behavior of the system. Ocean circulation is now recognized to involve both eddies and larger-scale flows with dominant elements and their interactions varying among the classical gyres, the boundary current regions, the Southern Ocean, and the tropics.
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spelling mit-1721.1/1294662022-09-29T11:01:13Z 100 Years of the Ocean General Circulation Wunsch, Carl Isaac Ferrari, Raffaele Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences The central change in understanding of the ocean circulation during the past 100 years has been its emergence as an intensely time-dependent, effectively turbulent and wave-dominated, flow. Early technologies for making the difficult observations were adequate only to depict large-scale, quasi-steady flows. With the electronic revolution of the past 50+ years, the emergence of geophysical fluid dynamics, the strongly inhomogeneous time-dependent nature of oceanic circulation physics finally emerged. Mesoscale (balanced), submesoscale oceanic eddies at 100-km horizontal scales and shorter, and internal waves are now known to be central to much of the behavior of the system. Ocean circulation is now recognized to involve both eddies and larger-scale flows with dominant elements and their interactions varying among the classical gyres, the boundary current regions, the Southern Ocean, and the tropics. 2021-01-20T16:09:06Z 2021-01-20T16:09:06Z 2018-01 2020-04-17T13:45:28Z Article http://purl.org/eprint/type/JournalArticle 0065-9401 https://hdl.handle.net/1721.1/129466 Wunsch, Carl and Raffaele Ferrari. "100 Years of the Ocean General Circulation." Meteorological Monographs, 59, American Meteorological Society, 2018, 7.1-7.32. © 2018 American Meteorological Society en http://dx.doi.org/10.1175/amsmonographs-d-18-0002.1 Meteorological Monographs Article is made available in accordance with the publisher's policy and may be subject to US copyright law. Please refer to the publisher's site for terms of use. application/pdf American Meteorological Society American Meteorological Society
spellingShingle Wunsch, Carl Isaac
Ferrari, Raffaele
100 Years of the Ocean General Circulation
title 100 Years of the Ocean General Circulation
title_full 100 Years of the Ocean General Circulation
title_fullStr 100 Years of the Ocean General Circulation
title_full_unstemmed 100 Years of the Ocean General Circulation
title_short 100 Years of the Ocean General Circulation
title_sort 100 years of the ocean general circulation
url https://hdl.handle.net/1721.1/129466
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