成都信息工程学院：《动力气象学》课程教学资源（电子教案）授课计划（林蟒、李国平）

一、大气边界层 二、大气能量学 三、大气波动 四、地转适应过程 五、大气波动的不稳定理论 六、低纬大气动力学基础

§1 大气能量的主要形式 §2 铅直气柱中各种能量的比较 §3 能量方程与能量守恒 §4 大气中的能量转换事实 §5 大尺度大气运动的能量循环过程

§4 重力外波和重力内波 §5 惯性振荡与惯性波 §6 水平无辐散的 Rossby 波 §7 有水平辐合辐散的 Rossby 波 §8 大气混合波—惯性重力外波 §9 群速度，波的频散效应

Can be continuous Trajectory of a space shuttle Mass density in a cross-section of a brain · Can be discrete dNa base sequence Digital image pixels Can be 1-D,2-D,·N-D For this course: Focus on a single(1-D) independent variable which we call“time

1Some examples of systems 2 System properties and examples CAusality

Representation of ct signals Approximate any input x(t) as a sum of shifted, scaled

Fouriers derivation of the ct fourier transform x(t)-an aperiodic signal view it as the limit of a periodic signal as t→∞ For a periodic signal the harmonic components are spaced Oo=2π/ T apart. AsT→∞,Obo→>0, and harmonic components are space

Fourier series: Periodic signals and lti Systems ()=∑H(k k= ak一→H(ko)ak “g Soak-→|H(jkco)lkl H(7k)=1H(k0e∠B(ko) or powers of signals get modified through filter/system ncludes both amplitude phase akeJhwon

1. DTFT Properties and Examples 2. Duality in fs& ft 3. Magnitude/Phase of Transforms and Frequency Responses