1 edition of Eddy structure and the West and East Australian Currents found in the catalog.
Eddy structure and the West and East Australian Currents
John C. Andrews
by Flinders Institute for Atmospheric & Marine Sciences, Flinders University of South Australia in [Adelaide]
Written in English
Bibliography: p. 165-172.
|Statement||by John C. Andrews.|
|Series||Research report / the Flinders Institute for Atmospheric & Marine Sciences, the Flinders University of South Australia ;, no. 30, Research report (Flinders Institute for Atmospheric and Marine Sciences) ;, no. 30.|
|LC Classifications||GC283 .A53 1979|
|The Physical Object|
|Pagination||xvi, 172 p.,  p. of plates :|
|Number of Pages||172|
|LC Control Number||83225183|
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Eddy structure and the West Australian Current E 4- E3 I J, ~ '. 0 0 8 Fractionel volume trenspor'i- Fig. The volume transport between the surface and standard depths as a fraction of the total volume transport; all transports have a reference level of by: The West Australian Current (or the Western Australian Current), is a cool surface current of the Southern Ocean and Southern Indian Ocean.
It starts as the Southern Indian Ocean Current, a part of the larger Antarctic Circumpolar Current (also known as the West Wind Drift).As the current approaches Western Australia, it turns north, parallel to the western coast of Australia, and becomes the.
The analysis of an eddy census for the East Australian Current (EAC) region yielded a total of individual short-lived (7–28 days) cyclonic and anticyclonic eddies for the period to The East Australian Current (EAC) is a strong, warm, western boundary current that also influences cross-shelf patterns on the GBR and New South Wales (NSW) as it flows southwards along the.
The analysis of eddy currents. Richard L. Stoll. Clarendon Press, - Technology & Engineering - pages. 0 Reviews. From inside the book. What people are saying - Write a review. We haven't found any reviews in the usual places. Contents. INTRODUCTION. Albert J. Williams 3rd, in Measuring Ocean Currents, Western boundary currents like the Gulf Stream, Kuroshio, and Agulhas were first observed by ship drift but later by moorings, motivating the development of the VACM for capturing variability in the Gulf Stream.
An interesting experience that this instrument endured in the Agulhas (I learned from talks) was the nearly total. The strengthening East Australian Current, its eddies and biological effects — an introduction and overview article info The EAC’s eddy structure and formation by the EAC are examined.
A particular cold-core eddy is shown currents on both east and west coasts, and make speciﬁc comparisons between the EAC and the Leeuwin Current. Strong, persistent currents along the western boundaries of the world's major ocean basins are called "western boundary currents" (WBCs).
This chapter describes the structure and dynamics of WBCs, their roles in basin-scale circulation, regional variability, and their influence on atmosphere and by: You can write a book review and share your experiences. Other readers will always be interested in your opinion of the books you've read.
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The Antarctic Circumpolar Current (ACC) is an ocean current that flows clockwise from west to east around alternative name for the ACC is the West Wind ACC is the dominant circulation feature of the Southern Ocean and has a mean transport estimated at Sverdrups (Sv, million m³/s), or possibly even higher, making it the largest ocean current.
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The analysis of an eddy census for the East Australian Current (EAC) region yielded a total of individual short-lived ( days) cyclonic and anticyclonic eddies for the period to This was an average of about 23 eddies per year. 41% of the tracked individual cyclonic and anticyclonic eddies were detected off southeast Queensland between about 25 oS and 29 by: 6.
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