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Atmospheric Dynamics II. Prof. Zhuo Wang 205 Atmospheric Science Building PH: 244-4270 e-mail: zhuowang@illinois.edu Time: Tues/Thurs, 12: 3 0 – 1: 45 p.m. . Why should we learn Dynamics?.
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Atmospheric Dynamics II Prof. Zhuo Wang 205 Atmospheric Science Building PH: 244-4270 e-mail: zhuowang@illinois.edu Time: Tues/Thurs, 12:30 – 1:45p.m.
Why should we learn Dynamics? Dynamic meteorology is the theoretical study of the atmospheric motions that are associated with weather and climate. It tells you why atmospheric motions take the forms/patterns they have and why they evolve and change in the way they do.
Why is a low-pressure system usually associated with cloudy or rainy weather? L V CF PGF friction
Why is a low-pressure system usually associated with cloudy or rainy weather? L V CF PGF friction
Why is a low-pressure system usually associated with cloudy or rainy weather? L V CF PGF friction
Why is a low-pressure system usually associated with cloudy or rainy weather? L V CF PGF friction
Why is a low-pressure system usually associated with cloudy or rainy weather?
200 hPaGeopotential Height Composite during El Nino Events: The Pacific-North American (PNA) Pattern How does a tropical forcing induce a stationary wave train pattern extending to the extratropics? Years: Nino 3.4 1958: 1.607 1966: 1.308 1973: 1.639 1983: 2.548 1987: 1.254 1992: 1.820 1995: 1.013 1998: 2.396 2003: 1.162
Textbooks and Course Materials • Mid-Latitude Atmospheric Dynamics: A First Course, by Jonathan E. Martin • An Introduction to Dynamic Meteorology, 4th Edition, by J. Holton, 2004, Academic Press Elsevier • Lecture notes
Topics • Fundamentals for understanding atmospheric motions • Planetary boundary layer • Circulation and Vorticity • Potential Vorticity • Simple Waves • Mid-latitude Synoptic-Scale Vertical Motions • Mid-latitude Cyclogenesis • Application of PV to Mid-latitude Weather Systems • Frontogenesis *March 5-8, April 16-20
Grading • Homework: 30% • Tests (5): 70% • No final or midterm