000 01948nam  2200373za 4500
0019.868889
003CaOODSP
00520221107162717
006m    go  d f      
007cr |||||||||||
008190226e19820108bcca|||fo|   f000 0 eng d
040 |aCaOODSP|beng|cCaOODSP|erda
043 |an-cn-bc
0861 |aEn57-44/82-001E-PDF
1001 |aHammond, Brian, |eauthor.
24510|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
4901 |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).
5200 |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?"
69207|2gccst|aWeather forecasts
69207|2gccst|aSatellite imagery
7101 |aCanada. |bEnvironment Canada.
7101 |aCanada. |bAtmospheric Environment Service. |bPacific Region.
7101 |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
85640|qPDF|s569 KB|uhttps://publications.gc.ca/collections/collection_2019/eccc/en57-44/En57-44-82-001-eng.pdf