Titlebook: Differential Equations Theory, Numerics and Applications; Proceedings of the I E. Groesen,E. Soewono Conference proceedings 1997 Springer S

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書目名稱Differential Equations Theory, Numerics and Applications影響因子(影響力)




書目名稱Differential Equations Theory, Numerics and Applications影響因子(影響力)學科排名




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書目名稱Differential Equations Theory, Numerics and Applications網(wǎng)絡公開度學科排名




書目名稱Differential Equations Theory, Numerics and Applications被引頻次




書目名稱Differential Equations Theory, Numerics and Applications被引頻次學科排名




書目名稱Differential Equations Theory, Numerics and Applications年度引用




書目名稱Differential Equations Theory, Numerics and Applications年度引用學科排名




書目名稱Differential Equations Theory, Numerics and Applications讀者反饋




書目名稱Differential Equations Theory, Numerics and Applications讀者反饋學科排名

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Stephanie Pinder-Amaker,Kimberlyn Leary a fixed number of solitary pulses separated by radiation-free flat substrates. Radiation is generated in a noise-free environment when excess mass drains out of a pulse in the form of a spreading shelf and the radiation grows rapidly by feeding on the active substrate. However, this growth can be s

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https://doi.org/10.1007/978-3-319-42893-2 for the behaviour of short waves. In ship hydrodynamics where the generation of short waves by a slowly sailing vessel and the diffraction of short surface waves by these vessels is of importance recently the ray method is applied successfully. In this presentation we present two cases, each with i

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The ‘New Racism’ and National-Populismns with weak transverse effects. Typical examples are the generalized Kadomtsev Petviashvili equation or the equation for Langmuir waves in a weakly magnetized plasma. Those solitary waves are not “classical” in the sense that (contrarily to the solitary waves of the Korteweg de Vries or the usual n

煩擾

The ‘New Racism’ and National-Populism(1984) for the solution of shallow water wave equations. The application of the numerical model to regional waters of Singapore is demonstrated for the case of Singapore Straits by comparing the results of numerical simulation with the field measurements of tidal water levels and currents..As a furt

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