Application Of The Telegraph Equation To Oceanic Diffusion: Another Mathematic model

Author(s)Okubo, Akira
Date Accessioned2005-07-31T20:01:43Z
Date Available2005-07-31T20:01:43Z
Publication Date1971-03
AbstractThe solution of the conventional diffusion equation has an obvious shortcoming; that is, the substance concentration will rise instantaneously everywhere when substance is introduced at some point in the sea. Although such instantaneous propagation of substance makes a negligibly small contribution to the concentration at large distances from the source, it might cause serious error in predicting water pollution, micro-organism distributions, etc. A diffusion equation which overcomes this difficulty is the telegraph equation characterized by a finite propagation velocity. An ad hoc derivation of the telegraph equation from a set of hydromechanical equations identifies the parameters involved in the equation. Thus, the propagation velocity is related to the correlation tensor of turbulent velocity. As a result, the one-particle dispersion law by Taylor and the relative diffusion law by Richardson can be deduced from the telegraph equation.en
SponsorOffice of Naval Research, U.S. Atomic Energy Commission, National Science Foundationen
Extent2672421 bytes
MIME typeapplication/pdf
URLhttp://udspace.udel.edu/handle/19716/1439
Languageen_US
Part of SeriesCⅇ78
Keywordstelegraph equationen
Keywordsoceanic difussionen
Keywordsmathematical modelen
TitleApplication Of The Telegraph Equation To Oceanic Diffusion: Another Mathematic modelen
TypeTechnical Reporten
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