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Last modified
7/28/2009 2:38:55 PM
Creation date
4/16/2008 11:11:42 AM
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Template:
Weather Modification
Title
Wintertime Cloud Systems Over the Rockies: Three Case Studies
Date
12/1/1980
Weather Modification - Doc Type
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<br />19 <br /> <br />The analysis procedure outlined above is the same method used by <br /> <br />}1anvitz, et al., (1976) to describe the convective cloud component pre- <br /> <br />sent in San Juan storms (see also }1arwitz, 1980). Therefore, the convec- <br /> <br />'" <br /> <br />tive cloud component will be defined as the layer that lies between the <br /> <br />convective instability base and convective instability top (see Figure <br /> <br />3 below). <br /> <br />KPa <br />40 L <br /> PIT PIT PIT <br /> cr <br /> w <br /> I- cr <br /> <! <br /> 3: w <br />50 I- <br /> "- <! <br /> cr ;: <br /> ~ w <br /> 0 I- ... <br /> W <t "- <br /> I- ;: ~ <br />4- <! 0 <br /> cr "- w <br />60 ::> l- <br /> I- 3 <t <br /> <t 0 cr <br /> (f) w ::> <br /> l- I- <br /> <t <! <br /> rr: (f) <br />70 PIB PIB ::> PIB CIS <br /> I- <br /> <t <br /> (f) <br />80 <br />90 <br /> e - a- e - <br /> e e e <br /> <br /> <br /> <br /> <br />Figure 3. Examples of convective cloud components. <br />
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