|
000
| 01948cam 2200373za 4500 |
|---|
| 001 | 9.868889 |
|---|
| 003 | CaOODSP |
|---|
| 005 | 20221107162717 |
|---|
| 006 | m go d f |
|---|
| 007 | cr ||||||||||| |
|---|
| 008 | 190226e19820108bcca|||fo| f000 0 eng d |
|---|
| 040 | |aCaOODSP|beng|cCaOODSP|erda |
|---|
| 043 | |an-cn-bc |
|---|
| 086 | 1 |aEn57-44/82-001E-PDF |
|---|
| 100 | 1 |aHammond, Brian, |eauthor. |
|---|
| 245 | 10|aTransverse banding in jet stream cirrus / |cBrian Hammond, supervising meteorologist. |
|---|
| 264 | 1|aVancouver : |bPacific Weather Centre, |cJanuary 8, 1982. |
|---|
| 300 | |a1 online resource (3 pages, 2 unnumbered pages) : |billustrations |
|---|
| 336 | |atext|btxt|2rdacontent |
|---|
| 337 | |acomputer|bc|2rdamedia |
|---|
| 338 | |aonline resource|bcr|2rdacarrier |
|---|
| 490 | 1 |aPacific region technical notes ; |vno. 82-001 |
|---|
| 500 | |aDigitized edition from print [produced by Environment and Climate Change Canada]. |
|---|
| 500 | |aCaption title. |
|---|
| 504 | |aIncludes bibliographical references (page 3). |
|---|
| 520 | 0 |a"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?" |
|---|
| 692 | 07|2gccst|aWeather forecasts |
|---|
| 692 | 07|2gccst|aSatellite imagery |
|---|
| 710 | 1 |aCanada. |bEnvironment Canada. |
|---|
| 710 | 1 |aCanada. |bAtmospheric Environment Service. |bPacific Region. |
|---|
| 710 | 1 |aCanada. |bAtmospheric Environment Service. |bPacific Weather Center. |
|---|
| 830 | #0|aPacific region technical notes (Canada. Atmospheric Environment Service. Pacific Region)|vno. 82-001|w(CaOODSP)9.865532 |
|---|
| 856 | 40|qPDF|s569 KB|uhttps://publications.gc.ca/collections/collection_2019/eccc/en57-44/En57-44-82-001-eng.pdf |
|---|