Spirals on the sea

Spiral eddies were first seen in the sun glitter on the Apollo Mission 30 years ago; they have since been recorded on SAR missions and in the infrared. The spirals are globally distributed, 10-25 km in size and overwhelmingly cyclonic. They have not been explained. Under light winds favorable to vis...

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Main Author: Walter Munk
Format: Article
Language:English
Published: Consejo Superior de Investigaciones Científicas 2001-12-01
Series:Scientia Marina
Subjects:
Online Access:http://scientiamarina.revistas.csic.es/index.php/scientiamarina/article/view/693
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author Walter Munk
author_facet Walter Munk
author_sort Walter Munk
collection DOAJ
description Spiral eddies were first seen in the sun glitter on the Apollo Mission 30 years ago; they have since been recorded on SAR missions and in the infrared. The spirals are globally distributed, 10-25 km in size and overwhelmingly cyclonic. They have not been explained. Under light winds favorable to visualization, linear surface features with high surfactant density and low surface roughness are of common occurrence. We have proposed that frontal formations concentrate the ambient shear and prevailing surfactants. Horizontal shear instabilities ensue when the shear becomes comparable to the coriolis frequency. The resulting vortices wind the liner features into spirals. The hypothesis needs to be tested by prolonged measurements and surface truth. Spiral eddies are a manifestation of a sub-mesoscale oceanography associated with upper ocean stirring; dimensional considerations suggest a horizontal diffusivity of order 103 m2 s-1.
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spelling doaj.art-e041be23ac864843845a432e89ff11592022-12-21T22:47:40ZengConsejo Superior de Investigaciones CientíficasScientia Marina0214-83581886-81342001-12-0165S219319810.3989/scimar.2001.65s2193687Spirals on the seaWalter Munk0University of California at San DiegoSpiral eddies were first seen in the sun glitter on the Apollo Mission 30 years ago; they have since been recorded on SAR missions and in the infrared. The spirals are globally distributed, 10-25 km in size and overwhelmingly cyclonic. They have not been explained. Under light winds favorable to visualization, linear surface features with high surfactant density and low surface roughness are of common occurrence. We have proposed that frontal formations concentrate the ambient shear and prevailing surfactants. Horizontal shear instabilities ensue when the shear becomes comparable to the coriolis frequency. The resulting vortices wind the liner features into spirals. The hypothesis needs to be tested by prolonged measurements and surface truth. Spiral eddies are a manifestation of a sub-mesoscale oceanography associated with upper ocean stirring; dimensional considerations suggest a horizontal diffusivity of order 103 m2 s-1.http://scientiamarina.revistas.csic.es/index.php/scientiamarina/article/view/693remote sensingair-sea boundaryfrontal formationmixing
spellingShingle Walter Munk
Spirals on the sea
Scientia Marina
remote sensing
air-sea boundary
frontal formation
mixing
title Spirals on the sea
title_full Spirals on the sea
title_fullStr Spirals on the sea
title_full_unstemmed Spirals on the sea
title_short Spirals on the sea
title_sort spirals on the sea
topic remote sensing
air-sea boundary
frontal formation
mixing
url http://scientiamarina.revistas.csic.es/index.php/scientiamarina/article/view/693
work_keys_str_mv AT waltermunk spiralsonthesea