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  • 1
    Publication Date: 2022-05-25
    Description: Author Posting. © The Authors, 2005. This is the author's version of the work. It is posted here by permission of Science in China Press for personal use, not for redistribution. The definitive version was published in Chinese Science Bulletin 51 (2006): 327-330, doi:10.1007/s11434-006-0327-x.
    Description: Mechanical energy input to the oceans is one of the most important factors controlling the oceanic general circulation. The atmosphere transports mechanical energy to the oceans primarily through wind stress, plus changes of the sea level pressure (the so-called atmospheric loading). The rate of mechanical energy transfer into the ocean due to atmospheric loading is calculated, based on TOPEX/POSEIDON data over ten-year period (1993-2002). The rate of total energy input for the world oceans is estimated at 0.04TW (1TW=1012W), and most of this energy input is concentrated in the Southern Oceans and the Storm Tracks in the Northern Hemisphere. This energy input varied greatly with time, and the amplitude of the interannual variability over the past ten years is about 15%.
    Description: WW and CCQ were supported by the National Nature Science Foundation of China through grant 40476010 and Research Fund for the Doctoral Program of Higher Education through grant 20030423011. RXH was supported by the National Aero-Space Administration through Contract No. 1229833 (NRA-00-OES-05).
    Keywords: Mechanical energy ; Atmospheric loading ; Ocean
    Repository Name: Woods Hole Open Access Server
    Type: Preprint
    Format: 157120 bytes
    Format: application/pdf
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  • 2
    Publication Date: 2022-05-25
    Description: Author Posting. © American Geophysical Union, 2013. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Geophysical Research Letters 40 (2013): 3677–3681, doi:10.1002/grl.50736.
    Description: Mesoscale eddies dominate oceanic kinetic energy at sub-inertial frequencies. Their three-dimensional structure has, however, remained obscure, hindering better understanding of eddy dynamics. Here by applying the composite analysis of satellite altimetry and Argo float data to the globe, we show that despite remarkable regional differences in amplitude, extent and polarity, etc., mesoscale eddies have a universal structure in normalized stretched coordinates. Horizontally, the associated pressure anomaly is well described by a function of the normalized radial distance from the eddy center R(rn)=(1−rn2/2)• exp(−rn2/2), whereas vertically it is sinusoidal in a stretched coordinate zs = ƒ z0 (N/f )dz, where N and f are the buoyancy frequency and the Coriolis parameter.
    Description: This research was supported by the National Natural Science Foundation of China under grant 41276014 and the National Basic Research Priorities Program of China through grant 2013CB430303.
    Description: 2014-01-30
    Keywords: Geostrophic eddy ; Three-dimensional structure ; Universal ; Ocean
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
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