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John P. Boyd

    John P. Boyd es un distinguido científico y autor cuyo trabajo tiende un puente entre la rigurosa investigación científica y la narración imaginativa. Su carrera académica, profundamente arraigada en las ciencias atmosféricas, oceánicas y espaciales, también lo ha visto ser pionero en métodos computacionales y establecer programas de posgrado avanzados. Más allá de sus extensas contribuciones a la literatura científica, Boyd revela un espíritu creativo a través de su ciencia ficción, explorando ideas complejas con un estilo narrativo único.

    Dynamics of the Equatorial ocean
    Weakly Nonlocal Solitary Waves and Beyond-All-Orders Asymptotics
    • Weakly Nonlocal Solitary Waves and Beyond-All-Orders Asymptotics

      Generalized Solitons and Hyperasymptotic Perturbation Theory

      • 620 páginas
      • 22 horas de lectura

      Exploring the phenomenon of nonlocal solitary waves, the book delves into the mysterious origins of the "Morning Glory," a breathtaking cloud formation observed in northern Australia. These massive cylinders of cloud, rolling from the ocean inland, evoke a sense of wonder that has likely existed since ancient times. The text highlights the awe experienced by its early discoverer, who lived millennia before recorded history, and connects this natural spectacle to modern scientific understanding. The narrative intertwines history, science, and the beauty of nature.

      Weakly Nonlocal Solitary Waves and Beyond-All-Orders Asymptotics
    • Dynamics of the Equatorial ocean

      • 541 páginas
      • 19 horas de lectura

      This book is the first comprehensive introduction to the theory of equatorially-confined waves and currents in the ocean. Among the topics treated are inertial and shear instabilities, wave generation by coastal reflection, semiannual and annual cycles in the tropic sea, transient equatorial waves, vertically-propagating beams, equatorial Ekman layers, the Yoshida jet model, generation of coastal Kelvin waves from equatorial waves by reflection, Rossby solitary waves, and Kelvin frontogenesis. A series of appendices on midlatitude theories for waves, jets and wave reflections add further material to assist the reader in understanding the differences between the same phenomenon in the equatorial zone versus higher latitudes.

      Dynamics of the Equatorial ocean