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  • 1
    Publication Date: 2015-06-19
    Description: Pacific Ocean western boundary currents and the interlinked equatorial Pacific circulation system were among the first currents of these types to be explored by pioneering oceanographers. The widely accepted but poorly quantified importance of these currents-in processes such as the El Nino/Southern Oscillation, the Pacific Decadal Oscillation and the Indonesian Throughflow-has triggered renewed interest. Ongoing efforts are seeking to understand the heat and mass balances of the equatorial Pacific, and possible changes associated with greenhouse-gas-induced climate change. Only a concerted international effort will close the observational, theoretical and technical gaps currently limiting a robust answer to these elusive questions.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Hu, Dunxin -- Wu, Lixin -- Cai, Wenju -- Gupta, Alex Sen -- Ganachaud, Alexandre -- Qiu, Bo -- Gordon, Arnold L -- Lin, Xiaopei -- Chen, Zhaohui -- Hu, Shijian -- Wang, Guojian -- Wang, Qingye -- Sprintall, Janet -- Qu, Tangdong -- Kashino, Yuji -- Wang, Fan -- Kessler, William S -- England -- Nature. 2015 Jun 18;522(7556):299-308. doi: 10.1038/nature14504.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Key Laboratory of Ocean Circulation and Waves, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China. ; Physical Oceanography Laboratory, Qingdao Collaborative Innovation Center of Marine Science and Technology, Ocean University of China, Qingdao 266003, China. ; 1] Physical Oceanography Laboratory, Qingdao Collaborative Innovation Center of Marine Science and Technology, Ocean University of China, Qingdao 266003, China [2] CSIRO Oceans and Atmosphere Flagship, Aspendale, Victoria 3195, Australia. ; Australian Research Council (ARC) Centre of Excellence for Climate System Science, Mathews Building, The University of New South Wales, Sydney 2052, Australia. ; Institut de Recherche pour le Developpement (IRD), UMR5566-LEGOS, UPS (OMP-PCA), 31400 Toulouse, France. ; Department of Oceanography, University of Hawaii at Manoa, 1000 Pope Road, Honolulu, Hawaii 96822, USA. ; Lamont-Doherty Earth Observatory, Earth Institute at Columbia University, Palisades, New York 10964, USA. ; CSIRO Oceans and Atmosphere Flagship, Aspendale, Victoria 3195, Australia. ; Scripps Institution of Oceanography, 9500 Gilman Drive, La Jolla, California 92037, USA. ; IPRC, Department of Oceanography, SOEST, University of Hawaii, Honolulu, Hawaii 96822, USA. ; Center for Earth Information Science and Technology, Japan Agency for Marine-Earth Science and Technology (JAMSTEC) 3173-25 Showa-machi Kanazawa-ku, Yokohama 236-0001, Japan. ; NOAA/Pacific Marine Environmental Laboratory, Seattle, Washington 98115, USA.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/26085269" target="_blank"〉PubMed〈/a〉
    Keywords: *Climate ; *Climate Change ; El Nino-Southern Oscillation ; Hot Temperature ; Pacific Ocean ; Uncertainty ; *Water Movements
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    Archive of applied mechanics 66 (1996), S. 336-342 
    ISSN: 1432-0681
    Keywords: boundary layer ; semi-similarity ; singular parabolicity ; finite difference ; upwind scheme
    Source: Springer Online Journal Archives 1860-2000
    Topics: Mechanical Engineering, Materials Science, Production Engineering, Mining and Metallurgy, Traffic Engineering, Precision Mechanics
    Notes: Summary The development of a compressible boundary layer over a wedge impulsively set into motion is studied in this paper. The initial motion is independent of the leading edge effect and the solutions are those of a Rayleigh-type problem. The motion tends to an ultimate steady state of Falkner-Skan type. The equations governing the transient boundary layer from the initial steady state to the terminal steady-state change their character after certain time due to the leading edge effect and thereafter solution depends on both the end conditions. Numerical solutions are obtained through the second-order accuracy upwind scheme. The effects of the Falkner-Skan parameter and the surface temperature on the transient flow and heat transfer are also studied. It has been found that the flow separation does not occur form≧−0.0707 when θ w = 1.5 (hot wall), andm≧−0.118 when θ 0.5 (cold wall).
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    Springer
    Archive of applied mechanics 66 (1996), S. 336-342 
    ISSN: 1432-0681
    Keywords: Key words boundary layer ; semi-similarity ; singular parabolicity ; finite difference ; upwind scheme
    Source: Springer Online Journal Archives 1860-2000
    Topics: Mechanical Engineering, Materials Science, Production Engineering, Mining and Metallurgy, Traffic Engineering, Precision Mechanics
    Notes: Summary  The development of a compressible boundary layer over a wedge impulsively set into motion is studied in this paper. The initial motion is independent of the leading edge effect and the solutions are those of a Rayleigh-type problem. The motion tends to an ultimate steady state of Falkner-Skan type. The equations governing the transient boundary layer from the initial steady state to the terminal steady-state change their character after certain time due to the leading edge effect and thereafter solution depends on both the end conditions. Numerical solutions are obtained through the second-order accuracy upwind scheme. The effects of the Falkner-Skan parameter and the surface temperature on the transient flow and heat transfer are also studied. It has been found that the flow separation does not occur for .
    Type of Medium: Electronic Resource
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