Hemiplegia 发表于 2025-3-25 03:58:10
http://reply.papertrans.cn/17/1647/164651/164651_21.pngflammable 发表于 2025-3-25 11:04:12
http://reply.papertrans.cn/17/1647/164651/164651_22.pngInterlocking 发表于 2025-3-25 14:02:10
http://reply.papertrans.cn/17/1647/164651/164651_23.png音乐等 发表于 2025-3-25 17:38:37
http://reply.papertrans.cn/17/1647/164651/164651_24.png整体 发表于 2025-3-25 20:01:45
Fusarium Head Blight in Latin Americamore convenient, however, to separate the atmospheric wave motions from a hypothetical motionless or stationary background atmosphere. The wind can be divided into a source-free (no divergence) and a curl-free (no vorticity) component.Polydipsia 发表于 2025-3-26 02:14:32
https://doi.org/10.1007/978-94-007-7091-1 of the atmospheric gas is a complicated process that depends on the physical and chemical conditions of the atmosphere. Minor constituents like ozone or the ionospheric plasma play important roles in transferring solar energy into heat and momentum. Strictly speaking, one must solve a set of compli环形 发表于 2025-3-26 08:19:46
Martha Díaz de Ackermann,Man Mohan Kohlie to be taken into account. These indirect sources and sinks are a consequence of our limited ability to deal with the full complex system Earth-Ocean-Atmosphere on all scales of motion and to account for all physical and chemical processes in the multi-component atmospheric gas. Instead, we try to捕鲸鱼叉 发表于 2025-3-26 11:31:28
http://reply.papertrans.cn/17/1647/164651/164651_28.png玷污 发表于 2025-3-26 13:23:24
Erlei M. Reis,Marcelo A. Carmona this, we have to solve the system of Equations (5.8). In the presence of a realistic background temperature with height dependent scale height and variable Brunt-Väisälä frequency, this system can only be treated numerically. However, for an isothermal background atmosphere and constant dissipationlegitimate 发表于 2025-3-26 17:42:16
Erlei M. Reis,Marcelo A. Carmonanonlinear loss processes such as turbulence and eddy heat conduction by Rayleigh friction and Newtonian cooling. However, even without these loss processes, the waves interfere with each other via the nonlinear advection terms in the equations of motion. This nonlinear coupling gives rise to new wav