The Numerical Solution of a Parabolic System of Differential Equations Arising in Shallow Water Theory

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"A finite difference approximation to a non-linear set of parabolic differential equations arising in shallow water theory is given. These difference equations were used to determine the shape and rate of propagation of a hum of fluid down a channel of constant depth. The hump of fluid was found to spread instead of steepen, as is the case in the usual shallow water theory."

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20 pages : illustrations

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Heller, Jack & Isaacson, Eugene October 15, 1960.

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"A finite difference approximation to a non-linear set of parabolic differential equations arising in shallow water theory is given. These difference equations were used to determine the shape and rate of propagation of a hum of fluid down a channel of constant depth. The hump of fluid was found to spread instead of steepen, as is the case in the usual shallow water theory."

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20 pages : illustrations

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Digitized from microopaque cards (1).

Includes bibliographical references (page 16)

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  • OCLC: #
  • SuDoc Number: Y 3.At 7:22/NYO-9372
  • Report No.: NYO-9372
  • Accession or Local Control No: metadc1463594
  • Archival Resource Key: ark:/67531/metadc1463594

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  • October 15, 1960

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  • Sept. 2, 2021, 4:30 p.m.

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  • July 24, 2023, 10:06 a.m.

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Heller, Jack & Isaacson, Eugene. The Numerical Solution of a Parabolic System of Differential Equations Arising in Shallow Water Theory, report, October 15, 1960; Washington D.C.. (https://digital.library.unt.edu/ark:/67531/metadc1463594/: accessed December 7, 2023), University of North Texas Libraries, UNT Digital Library, https://digital.library.unt.edu; crediting UNT Libraries Government Documents Department.

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