A Half Century of Progress in Meteorology: A Tribute to by Richard H. Johnson, Robert A. Houze Jr. PDF

By Richard H. Johnson, Robert A. Houze Jr.

ISBN-10: 1878220691

ISBN-13: 9781878220691

Through a chain of reports by way of invited specialists, this monograph will pay tribute to Richard Reed's extraordinary contributions to meteorology and his management within the technological know-how neighborhood over the last 50 years.

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Extra resources for A Half Century of Progress in Meteorology: A Tribute to Richard Reed

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16 from Schultz and Doswell (1999). e the base of the trough near peak intensity as amplification of the synoptic-scale baroclinic wave ceases as the thermal and geopotential height troughs come into phase. Finally, the jet-front system migrates downstream into the southwesterly flow where confluence in the presence of warmair advection contributes to frontogenesis. A possible difficulty with the Shapiro (1982) schematic representation in Fig. 20, however, is that individual upper-level fronts are seldom observed to migrate around the base of the baroclinic wave trough from the northwesterly to the southwesterly flow [the Bosart (1970) case is atypical].

Based on the previous discussion, the use of PV thinking and a DT perspective are likely to be helpful in this endeavor. 7. An example of upper-level frontogenesis in southwesterly flow a. Conceptual models offrontal life cycles Although case studies of upper-level fronts over North America since the pioneering investigations by Reed and CHAPTER 2 35 BOSART Sanders (1953) and Reed (1955) have uncovered many important aspects of the structure of these fronts, attempts to document complete frontal life cycles have been more difficult.

0 .. . : :. ~·<·"~l"; :"'~"'l"':' ~\ '4 \ 21 B OSART 2 -1t,........ .. ~... " • .. --....... - .... I ... \ .... \ .. \ "I . ,. FIG. 8. (left) Semigeostrophic solution for an upper-level jet streak exit region overlying a surface frontal zone (refer to Figs. 2. 7a,b). Values of Ji2, :f, and N2 coincide with those for the control case (see Hakim and Keyser 2001). Streamfunction is given by thick lines (negative values dashed) every 2 x 103 m2 S-I; positive values of vertical motion OJ are shaded every 2 cm S-1 starting at I cm S-I, and absolute momentum is given by thin dashed lines every 30 m s-1.

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A Half Century of Progress in Meteorology: A Tribute to Richard Reed by Richard H. Johnson, Robert A. Houze Jr.

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