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portada eddies in marine science (in English)
Type
Physical Book
Illustrated by
Publisher
Year
2011
Language
English
Pages
612
Format
Paperback
Dimensions
24.4 x 17.0 x 3.3 cm
Weight
1.01 kg.
ISBN
364269005x
ISBN13
9783642690051

eddies in marine science (in English)

A. R. Robinson (Illustrated by) · Springer · Paperback

eddies in marine science (in English) - Robinson, A. R.

Physical Book

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Synopsis "eddies in marine science (in English)"

It is now well known that the mid-ocean flow is almost everywhere domi- nated by so-called synoptic or meso-scale eddies, rotating about nearly vertical axes and extending throughout the water column. A typical mid- ocean horizontal scale is 100 km and a time scale is 100 days: these meso- scale eddies have swirl speeds of order 10 cm s -1 which are usually con- siderably greater than the long-term average flow. Many types of eddies with somewhat different scales and characteristics have been identified. The existence of such eddies was suspected by navigators more than a century ago and confirmed by the world of C. O'D. Iselin and V. B. Stock- man in the 1930's. Measurements from RIV Aries in 1959/60, using the then newly developed neutrally buoyant floats, indicated the main char- acteristics of the eddies in the deep ocean of the NW Atlantic while a se- ries of Soviet moored current-meter arrays culminated, in POLYGON- 1970, in the explicit mapping of an energetic anticyclonic eddy in the tropical NE Atlantic. In 1973 a large collaborative (mainly U. S., U. K. ) program, MODE-I, produced synoptic charts for an area of the NW At- lantic and confirmed the existence of an open ocean eddy field and es- tablished its characteristics. Meso-scale eddies are now known to be of interest and importance to marine chemists and biologists as well as to physical oceanographers and meteorologists.

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The book is written in English.
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