| 書(shū)目名稱 | Eddies in Marine Science |
| 編輯 | Allan R. Robinson (Gordon McKay Professor of Geoph |
| 視頻video | http://file.papertrans.cn/303/302204/302204.mp4 |
| 叢書(shū)名稱 | Topics in Atmospheric and Oceanic Sciences |
| 圖書(shū)封面 |  |
| 描述 | 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 oce |
| 出版日期 | Conference proceedings 1983 |
| 關(guān)鍵詞 | Arctic Ocean; Atlantic Ocean; Coast; Indian Ocean; Meeresstr?mung; Pacific Ocean; Southern Ocean; Wirbel; ma |
| 版次 | 1 |
| doi | https://doi.org/10.1007/978-3-642-69003-7 |
| isbn_softcover | 978-3-642-69005-1 |
| isbn_ebook | 978-3-642-69003-7Series ISSN 1431-9314 |
| issn_series | 1431-9314 |
| copyright | Springer-Verlag, Berlin Heidelberg 1983 |
|Archiver|手機(jī)版|小黑屋|
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