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標(biāo)題: Titlebook: Nonlinear Physical Oceanography; A Dynamical Systems Henk A. Dijkstra Book 2000 Springer Science+Business Media Dordrecht 2000 Atlantic Oc [打印本頁(yè)]

作者: 脾氣好    時(shí)間: 2025-3-21 16:44
書(shū)目名稱Nonlinear Physical Oceanography影響因子(影響力)




書(shū)目名稱Nonlinear Physical Oceanography影響因子(影響力)學(xué)科排名




書(shū)目名稱Nonlinear Physical Oceanography網(wǎng)絡(luò)公開(kāi)度




書(shū)目名稱Nonlinear Physical Oceanography網(wǎng)絡(luò)公開(kāi)度學(xué)科排名




書(shū)目名稱Nonlinear Physical Oceanography被引頻次




書(shū)目名稱Nonlinear Physical Oceanography被引頻次學(xué)科排名




書(shū)目名稱Nonlinear Physical Oceanography年度引用




書(shū)目名稱Nonlinear Physical Oceanography年度引用學(xué)科排名




書(shū)目名稱Nonlinear Physical Oceanography讀者反饋




書(shū)目名稱Nonlinear Physical Oceanography讀者反饋學(xué)科排名





作者: 冷漠    時(shí)間: 2025-3-21 21:20

作者: 疏遠(yuǎn)天際    時(shí)間: 2025-3-22 00:40
Henk A. Dijkstrather these changes show the glass half empty or half full is difficult to discern. Whether it is under our power to fill—or empty—it is not all clear to me. The glass may be fuller now for one member of the marriage or family but emptier for another; fuller for women in some classes, emptier for those in other classes.
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作者: Ledger    時(shí)間: 2025-3-23 00:23
the last two decades. In addition, participants ana- lyzed the perceived and actual costs and benefits associated with chang- ing lifestyles, for women and men as individuals and for society as a whole. Finally, they considered the implications of their findings for the future and identified areas for further978-1-4613-3648-8978-1-4613-3646-4
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Nonlinear Physical Oceanography978-94-015-9450-9Series ISSN 1383-8601 Series E-ISSN 2215-162X
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作者: Albinism    時(shí)間: 2025-3-24 14:39
Henk A. Dijkstrae Patterns of an Era: Family, Work, and Education." A scholarly event saluting Radcliffe‘s centenary, the conference examined a range of indicators of social change, particularly as they relate to women in America in the last two decades. The program was interdisciplinary, bringing together scholars
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Background Material, through the chapters 5-7 more comfortable, some background material is included. First, the general equations of motion are presented in section 2.1 to introduce the notation used in the book. There are many textbooks available where these equations are derived and discussed (Pedlosky, 1987; Cushma
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作者: 貪婪地吃    時(shí)間: 2025-3-25 09:37
Numerical Techniques,cation points. As will become clear in this chapter, the detail of the dynamical behavior which can be analysed depends on the dimension, say TV, of the dynamical system. For systems of ordinary differential equations of small dimension (. < 10), the origin of very complex spatial/temporal dynamics
作者: Anthropoid    時(shí)間: 2025-3-25 14:51
The Wind-Driven Ocean Circulation,ion on time scales from several months to several years. Focus in this chapter is on the North Atlantic ocean circulation, and in particular the Gulf Stream region, since for this region relatively many observations are available. The midlatitude surface ocean circulation has also been extensively s
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作者: Lasting    時(shí)間: 2025-3-26 01:16
1383-8601 e the dynamics of the Gulf Stream in the Atlantic Ocean,the stability of the thermohaline circulation and the ElNi?o/Southern Oscillation phenomenon in the Tropical Pacific.On the other hand, the book also deals with the numerical methods forapplying bifurcation analysis on large dimensional dynamic
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作者: MEN    時(shí)間: 2025-3-26 22:26
Book 2000mics of the Gulf Stream in the Atlantic Ocean,the stability of the thermohaline circulation and the ElNi?o/Southern Oscillation phenomenon in the Tropical Pacific.On the other hand, the book also deals with the numerical methods forapplying bifurcation analysis on large dimensional dynamical systems
作者: Inclement    時(shí)間: 2025-3-27 03:26

作者: Indicative    時(shí)間: 2025-3-27 07:11
The Wind-Driven Ocean Circulation,Stream region, since for this region relatively many observations are available. The midlatitude surface ocean circulation has also been extensively studied theoretically using a wide range of ocean models. A description of the historical development of knowledge of the North Atlantic circulation has been given by Krauss (1996).
作者: 慎重    時(shí)間: 2025-3-27 10:44
The Thermohaline Ocean Circulation,icult to separate the three-dimensional ocean circulation in wind- and buoyancy driven parts. The motivation to study the buoyancy driven circulation in isolation is that the transitions in the flow which may have been responsible for rapid climate change in the past, strongly involved this component of the circulation.
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