Transverse banding in jet stream cirrus / Brian Hammond, supervising meteorologist.: En57-44/82-001E-PDF
"The jet stream downwind from a ridge is often hard to locate using satellite pictures because there is little or no cloud associated. However, in the following example the jet stream could be located using patches of cirrus cloud. This example is interesting in that transverse banding was evident in the cirrus jet stream cloud. The question arises - what causes this banding?"
Permanent link to this Catalogue record:
publications.gc.ca/pub?id=9.868889&sl=0
| Department/Agency | Canada. Environment Canada. Canada. Atmospheric Environment Service. Pacific Region. Canada. Atmospheric Environment Service. Pacific Weather Center. |
|---|---|
| Title | Transverse banding in jet stream cirrus / Brian Hammond, supervising meteorologist. |
| Series title | Pacific region technical notes ; no. 82-001 |
| Publication type | Series - View Master Record |
| Language | [English] |
| Format | Electronic |
| Electronic document | |
| Note(s) | Digitized edition from print [produced by Environment and Climate Change Canada]. Caption title. Includes bibliographical references (page 3). |
| Publishing information | Vancouver : Pacific Weather Centre, January 8, 1982. |
| Author / Contributor | Hammond, Brian, author. |
| Description | 1 online resource (3 pages, 2 unnumbered pages) : illustrations |
| Catalogue number |
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| Subject terms | Weather forecasts Satellite imagery |