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標(biāo)題: Titlebook: Eddies in Marine Science; Allan R. Robinson (Gordon McKay Professor of Geoph Conference proceedings 1983 Springer-Verlag, Berlin Heidelber [打印本頁]

作者: 哪能仁慈    時(shí)間: 2025-3-21 19:25
書目名稱Eddies in Marine Science影響因子(影響力)




書目名稱Eddies in Marine Science影響因子(影響力)學(xué)科排名




書目名稱Eddies in Marine Science網(wǎng)絡(luò)公開度




書目名稱Eddies in Marine Science網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Eddies in Marine Science被引頻次




書目名稱Eddies in Marine Science被引頻次學(xué)科排名




書目名稱Eddies in Marine Science年度引用




書目名稱Eddies in Marine Science年度引用學(xué)科排名




書目名稱Eddies in Marine Science讀者反饋




書目名稱Eddies in Marine Science讀者反饋學(xué)科排名





作者: 肉體    時(shí)間: 2025-3-22 00:11

作者: 積習(xí)難改    時(shí)間: 2025-3-22 03:50
Arbeiten mit den Fallbeispielenective vortices extending throughout the entire water column, lens vortices, planetary waves, topographic waves and wakes, etc. All of these types of variable flow are commonly referred to by physical oceanographers by the generic term “eddies”.
作者: lambaste    時(shí)間: 2025-3-22 05:17

作者: Arb853    時(shí)間: 2025-3-22 08:51

作者: Cerebrovascular    時(shí)間: 2025-3-22 14:33
Conference proceedings 1983eter 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
作者: Cerebrovascular    時(shí)間: 2025-3-22 17:50
Overview and Summary of Eddy Scienceective vortices extending throughout the entire water column, lens vortices, planetary waves, topographic waves and wakes, etc. All of these types of variable flow are commonly referred to by physical oceanographers by the generic term “eddies”.
作者: 高度贊揚(yáng)    時(shí)間: 2025-3-22 21:47
Eddies in the Indian Oceanes in circulation. In doing this, some characteristic subsections of the region will be identified, and in the rest of the chapter the eddy properties of each of these subsections will be briefly described.
作者: osteoclasts    時(shí)間: 2025-3-23 04:37

作者: 堅(jiān)毅    時(shí)間: 2025-3-23 07:57

作者: 殘忍    時(shí)間: 2025-3-23 13:01

作者: tic-douloureux    時(shí)間: 2025-3-23 14:33

作者: 蛙鳴聲    時(shí)間: 2025-3-23 19:17
https://doi.org/10.1007/978-3-662-00474-6The oceanic region considered in this chapter is the subtropical South Pacific, bounded by latitudes 23°S and 45°S and by longitudes 150°E and 290°E. It borders the tropical South Pacific and the Southern Ocean, which are considered in Chapters 10 and 14 respectively.
作者: 心痛    時(shí)間: 2025-3-24 01:51

作者: Antagonist    時(shí)間: 2025-3-24 06:06

作者: 伴隨而來    時(shí)間: 2025-3-24 09:46
The South Pacific Including the East Australian CurrentThe oceanic region considered in this chapter is the subtropical South Pacific, bounded by latitudes 23°S and 45°S and by longitudes 150°E and 290°E. It borders the tropical South Pacific and the Southern Ocean, which are considered in Chapters 10 and 14 respectively.
作者: Epidural-Space    時(shí)間: 2025-3-24 10:50

作者: Cabinet    時(shí)間: 2025-3-24 16:22
Modelle und Modellvorstellungen,haps the major characteristic, of mesoscale variability in this ocean basin is its very strong qualitative dependence upon proximity to the Gulf Stream system (see Schmitz 1978). The focus of this chapter is upon studies made during the POLYMODE program of the character of mesoscale variability at g
作者: flourish    時(shí)間: 2025-3-24 20:11
Chemiefasern nach dem Viskoseverfahrenar floats. These instruments, like their progenitor the Swallow float, are in essence tagged water parcels which allow us to obtain an explicit description of fluid motion over a wide range of space and time scales. On time scales of months to years the wandering of floats from one region to another
作者: 含水層    時(shí)間: 2025-3-25 02:10

作者: 使成波狀    時(shí)間: 2025-3-25 07:18
https://doi.org/10.1007/978-3-662-62174-5nual changes found whenever an appropriate investigation has sought such variability. The Gulf Stream path meanders with a broad spectrum of variability, particularly downstream of Cape Hatteras. These lateral translations range from interannual and seasonal shifts to the north or south, through sub
作者: 吸氣    時(shí)間: 2025-3-25 11:25
Werner Baumann,Bettina Herberg-Liedtkee times that of the Atlantic. Yet both oceans are forced by roughly similar westerly winds in midlatitude, which separate the easterly trade winds to the south from the polar easterlies to the north. Both oceans respond in their wind-driven circulation by forming a set of basin-wide gyres with inten
作者: 靈敏    時(shí)間: 2025-3-25 13:51

作者: Permanent    時(shí)間: 2025-3-25 17:31
,Praxis der beh?rdlichen Genehmigung,al regions. Experimental sites were chosen in the tropics at latitudes higher than 10° (Koshlyakov and Monin 1978) or at mid-latitudes (MODE Group, 1978; Robinson 1980). There exist, however, some XBT (Expendable Bathythermograph) sections through the equatorial belts that were obtained for studying
作者: glans-penis    時(shí)間: 2025-3-25 22:15
Internationale Atomgewichte 1968,nce of the monsoons and has a strongly variable seasonal circulation. As in most parts of the ocean, the only available overall view of eddy properties in this region is the one provided by Wyrtki, Magaard and Hager (1976). They calculated eddy kinetic energy per unit mass for each 5° square of the
作者: Highbrow    時(shí)間: 2025-3-26 03:57

作者: 任意    時(shí)間: 2025-3-26 07:42

作者: Carbon-Monoxide    時(shí)間: 2025-3-26 10:37

作者: Spangle    時(shí)間: 2025-3-26 15:54

作者: 不發(fā)音    時(shí)間: 2025-3-26 17:02

作者: 的染料    時(shí)間: 2025-3-26 22:18
https://doi.org/10.1007/978-3-642-69003-7Arctic Ocean; Atlantic Ocean; Coast; Indian Ocean; Meeresstr?mung; Pacific Ocean; Southern Ocean; Wirbel; ma
作者: Climate    時(shí)間: 2025-3-27 04:09

作者: 陰謀小團(tuán)體    時(shí)間: 2025-3-27 07:37
Eddies in Marine Science978-3-642-69003-7Series ISSN 1431-9314
作者: Ostrich    時(shí)間: 2025-3-27 13:30
Modelle und Modellvorstellungen,haps the major characteristic, of mesoscale variability in this ocean basin is its very strong qualitative dependence upon proximity to the Gulf Stream system (see Schmitz 1978). The focus of this chapter is upon studies made during the POLYMODE program of the character of mesoscale variability at great distances from the Gulf Stream system.
作者: Anecdote    時(shí)間: 2025-3-27 16:10
1431-9314 rly 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 wit
作者: Harrowing    時(shí)間: 2025-3-27 19:18

作者: macular-edema    時(shí)間: 2025-3-27 22:26

作者: Ischemic-Stroke    時(shí)間: 2025-3-28 04:49

作者: packet    時(shí)間: 2025-3-28 09:46

作者: Simulate    時(shí)間: 2025-3-28 12:38

作者: concubine    時(shí)間: 2025-3-28 16:17

作者: Decimate    時(shí)間: 2025-3-28 21:50
https://doi.org/10.1007/978-3-642-49796-4in terms of the areas where they are found. While the presentation is not intended to be exhaustive, it will be seen that enough is known to show that quasi-geostrophic motions play a variety of major roles in the dynamics of the northern oceans.
作者: Hemiplegia    時(shí)間: 2025-3-29 00:16
https://doi.org/10.1007/978-3-662-06237-1to the “mid-ocean” area (south of 20°S and between 50° and 100°E) so that the atlas compiled of the IIOE data (Wyrtki 1971) reveals a much lower station density in the central part of the Indian Ocean than elsewhere.
作者: 舊石器時(shí)代    時(shí)間: 2025-3-29 05:54

作者: 合適    時(shí)間: 2025-3-29 10:03
Vierstellige Mantissen der Logarithmen,s. The acute non-uniformity in the coverage of data, with adequate resolution, will often be mentioned and will be frequently invoked in qualifying any of the conclusions drawn. Most discussions will be concerned with the Northern and Equatorial Atlantic and Pacific Oceans.
作者: Ganglion-Cyst    時(shí)間: 2025-3-29 12:27

作者: 使熄滅    時(shí)間: 2025-3-29 18:39

作者: 無法解釋    時(shí)間: 2025-3-29 23:46

作者: 思想靈活    時(shí)間: 2025-3-30 02:52

作者: maverick    時(shí)間: 2025-3-30 05:07

作者: Nmda-Receptor    時(shí)間: 2025-3-30 09:38

作者: Matrimony    時(shí)間: 2025-3-30 12:28
Eddies in the Southern Indian Ocean and Agulhas Currentto the “mid-ocean” area (south of 20°S and between 50° and 100°E) so that the atlas compiled of the IIOE data (Wyrtki 1971) reveals a much lower station density in the central part of the Indian Ocean than elsewhere.
作者: 大包裹    時(shí)間: 2025-3-30 20:04
Global Summaries and Intercomparisons: Flow Statistics from Long-Term Current Meter Mooringsy one particular type of data - long-term current meter records - in order to provide a summary of kinetic energy statistics for as much of the world ocean as possible in the hope that meaningful regional characteristics will emerge.




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