摘要
A dominant role played by energy dispersion in the explosive development of extratropical marine cyclones over the Northwest Pacific has been revealed based on both the eddy energy equations and the energy flux vectors of nonlinear wave packet.At the initial and explosive time. the eddy energy from neighboring upstream systems beyond the radius of Rossby deformation is dispersed into the eddy energy center associated with the cyclone via ageostrophic geopotential fluxes,and results in the rapid increase of eddy kinetic energy and the occurrence of explosive cyclogenesis.When the cyclone begins to decay,its corresponding eddy energy is exported downstream and hence triggers the growth of new perturbation downstream.Through generalizing the energy flux vectors of quasigeostrophic wave packets to the nonlinear forms and making use of the relationship between the energy flux vectors and the total eddy energy,the approximation expressions of the total group velocity and relative group velocity are derived,and then they are used to compute an explosive case.The normalized ageostrophic geopotential fluxes by dividing the volume integral of ageostrophic geopotential fluxes by the integral of the total eddy energy determine the relative group velocity at which the eddy energy is spreading out,and they can be used to evaluate the position of next new disturbance.The nonlinear advective fluxes influence primarily the phase speed and translation of the cyclones.The results in this paper facilitate to expanding the mechanism research on explosive cyclones and have great significance for predicting the explosive intensification and downstream disturbance growth.
A dominant role played by energy dispersion in the explosive development of extratropical marine cyclones over the Northwest Pacific has been revealed based on both the eddy energy equations and the energy flux vectors of nonlinear wave packet.At the initial and explosive time. the eddy energy from neighboring upstream systems beyond the radius of Rossby deformation is dispersed into the eddy energy center associated with the cyclone via ageostrophic geopotential fluxes,and results in the rapid increase of eddy kinetic energy and the occurrence of explosive cyclogenesis.When the cyclone begins to decay,its corresponding eddy energy is exported downstream and hence triggers the growth of new perturbation downstream.Through generalizing the energy flux vectors of quasigeostrophic wave packets to the nonlinear forms and making use of the relationship between the energy flux vectors and the total eddy energy,the approximation expressions of the total group velocity and relative group velocity are derived,and then they are used to compute an explosive case.The normalized ageostrophic geopotential fluxes by dividing the volume integral of ageostrophic geopotential fluxes by the integral of the total eddy energy determine the relative group velocity at which the eddy energy is spreading out,and they can be used to evaluate the position of next new disturbance.The nonlinear advective fluxes influence primarily the phase speed and translation of the cyclones.The results in this paper facilitate to expanding the mechanism research on explosive cyclones and have great significance for predicting the explosive intensification and downstream disturbance growth.
