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Monday, February 3, 2020 | History

2 edition of Dynamics of nonlinear cross-equatorial flow in the deep ocean found in the catalog.

Dynamics of nonlinear cross-equatorial flow in the deep ocean

Christopher A. Edwards

Dynamics of nonlinear cross-equatorial flow in the deep ocean

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  • 24 Currently reading

Published by Massachusetts Institute of Technology, Woods Hole Oceanographic Institution, Joint Program in Oceanography/Applied Ocean Science and Engineering in Woods Hole, Mass .
Written in English

    Subjects:
  • Ocean currents.,
  • Ocean circulation.

  • Edition Notes

    Statementby Christopher A. Edwards.
    SeriesMIT/WHOI -- 97-10., MIT/WHOI (Series) -- 97-10.
    ContributionsMassachusetts Institute of Technology., Woods Hole Oceanographic Institution.
    The Physical Object
    Pagination180 p. :
    Number of Pages180
    ID Numbers
    Open LibraryOL15490796M

    Scott, Resistive Drift-Wave Turbulence. Mutter, Centered and staggered Fourier derivatives and Hilbert transforms. What needs to be done to ensure the poor and marginalise sections of our society do not lose out or not benefit from a sustainable blue economy? Atmosphere-Ocean, 27, — This symposium invites a wide range of data- and modeling-based presentations that aim to understand past behaviour of climate, ocean and ice.

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    Eddy-Zonal flow interactions and the persistence of the zonal index. Furthermore, in the Antarctic, sea ice change may affect ice shelf behaviour and hence could affect sea level change. Quarterly Journal of the Royal Meteorological Society, : Journal of Physical Oceanography, 31 3 : D'Odorico and T.


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Dynamics of nonlinear cross-equatorial flow in the deep ocean by Christopher A. Edwards Download PDF Ebook

Deep-Sea Research, 22 6 : Robinson1, G. Katz and J. It also illustrates the phenomena with numerical simulations and with stochastic models. Improving Nd isotope-based reconstructions of water masses Mechanisms and magnitudes of Nd supply to the oceans via particles, reactive sediments, or in dissolved form can vary as a function of climatically controlled parameters such as precipitation or ice and vegetation cover on the continents.

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Fairchild, B. Anchukaitis, K. The separate effects of the damping rates at low and high latitudes are somewhat more complex. Additional topics can consider extremes related to lake-effect or lake-modified systems and coastal extreme weather. Computing in Science and Engineering, 4 5 : Tsang, Y-K, and Vallis, G.

Chou, C. Journal of Physical Oceanography, 26 9 : Climate, 19, Nova University Press, Ft. However, the outlook for this proxy is, at present, mixed.

Comiso, J. Dynamics of nonlinear cross-equatorial flow in the deep ocean book, The North Atlantic Oscillation and regional phenology prediction over europe.

Response of the large-scale structure of the atmosphere to global warming. These effects are all demonstrated both by theoretical arguments and by numerical simulations with moist and dry general circulation models.

Baroclinic turbulence in the ocean: analysis with primitive equation and quasi-geostrophic simulations.The West African Sahel is well known for the severe droughts that ravaged the region in the s and s. Meteorological research on the region has flourished during the last decade as a result of several major field experiments.

This paper provides an overview of the results that have ensued. A major focus has been on the West African monsoon, a phenomenon that links all of West Africa Cited by: NOC Coastal Ocean Processes. Research interests Marine dynamics especially of the seas over the continental shelf and slope; waves over topography and their implications for residual circulation, sediment movement and ocean-shelf coupling and exchange.

Refereed Journal Articles (A pdf of the paper can be obtained by clicking the hyperlink attached to the image). 1. Swaters, G.

Current Trends in the Representation of Physical Processes in Weather and Climate Models

E., Ekman layer dissipation in an eastward-traveling modon. J. Phys. Oceanogr. 15,2. Swaters, G. E., Derivation and analysis of a McPhee-like damping term for inertially oscillating sea ice drift.The semiannual eastward winds of the tropical Indian Ocean drive the swift Yoshida–Wyrtki jets pdf, ) on the equator pdf the Indian monsoon transition months of April–May and October–galisend.com contrast to the Atlantic and Pacific, the eastward surface jet brings warm water to the eastern Indian Ocean and helps to maintain the Indo-Pacific warm galisend.com by: 1.Speaking as an educator, this is a useful and welcome resource for download pdf who plan on using this book as a class text I would recommend this book to anyone who wishes to gain an understanding of some of the fundamental ideas that underpin our current thinking about Author: R.

M. Samelson.The cross‐equatorial flow (Somali jet) is an essential component ebook the Asian monsoon system (Findlater, ).

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