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Rossby-gravity waves are equatorially trapped waves (much like Kelvin waves), meaning that they rapidly decay as their distance increases away from the equator (so long as the Brunt–Vaisala frequency does not remain constant). These waves have the same trapping scale as Kelvin waves, more commonly known as the equatorial Rossby deformation radius. They always carry energy eastward, but their 'crests' and 'troughs' may propagate westward if their periods are long enough.

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  • Ondas gravitacionales de Rossby (es)
  • Rossby-gravity waves (en)
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  • Las ondas gravitacionales de Rossby son ondas atrapadas ecuatorialmente (muy parecidas a las ondas Kelvin), lo que significa que decaen rápidamente a medida que aumenta su distancia lejos del ecuador (siempre que la no permanezca constante). Estas ondas tienen la misma escala de atrapamiento que las ondas Kelvin, más conocida como el Radio de deformación de Rossby ecuatorial.​ Siempre transportan energía hacia el este, pero sus "crestas" y "valles" pueden propagarse hacia el oeste si sus períodos son lo suficientemente largos. (es)
  • Rossby-gravity waves are equatorially trapped waves (much like Kelvin waves), meaning that they rapidly decay as their distance increases away from the equator (so long as the Brunt–Vaisala frequency does not remain constant). These waves have the same trapping scale as Kelvin waves, more commonly known as the equatorial Rossby deformation radius. They always carry energy eastward, but their 'crests' and 'troughs' may propagate westward if their periods are long enough. (en)
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  • Las ondas gravitacionales de Rossby son ondas atrapadas ecuatorialmente (muy parecidas a las ondas Kelvin), lo que significa que decaen rápidamente a medida que aumenta su distancia lejos del ecuador (siempre que la no permanezca constante). Estas ondas tienen la misma escala de atrapamiento que las ondas Kelvin, más conocida como el Radio de deformación de Rossby ecuatorial.​ Siempre transportan energía hacia el este, pero sus "crestas" y "valles" pueden propagarse hacia el oeste si sus períodos son lo suficientemente largos. (es)
  • Rossby-gravity waves are equatorially trapped waves (much like Kelvin waves), meaning that they rapidly decay as their distance increases away from the equator (so long as the Brunt–Vaisala frequency does not remain constant). These waves have the same trapping scale as Kelvin waves, more commonly known as the equatorial Rossby deformation radius. They always carry energy eastward, but their 'crests' and 'troughs' may propagate westward if their periods are long enough. (en)
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