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024 7 _ |2 DOI
|a 10.1007/s00703-004-0087-6
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041 _ _ |a eng
082 _ _ |a 550
084 _ _ |2 WoS
|a Meteorology & Atmospheric Sciences
100 1 _ |a Müller, R.
|0 P:(DE-Juel1)129138
|b 0
|u FZJ
245 _ _ |a Polytropic atmospheres and the scaling of potential vorticity
260 _ _ |c 2005
|a Wien [u.a.]
|b Springer
300 _ _ |a
336 7 _ |a Journal Article
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440 _ 0 |a Meteorology and Atmospheric Physics
|x 0177-7971
|0 12865
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500 _ _ |a Record converted from VDB: 12.11.2012
520 _ _ |a Potential vorticity P is in widespread use as a diagnostic in atmospheric dynamics. Here, we employ the concepts of polytropic change of state and polytropic temperature for investigating the problem of scaling potential vorticity. For many applications, it has proven useful to scale P with a dimensionless scale factor to remove its exponential increase with altitude. This scale factor may be derived from the assumption of a polytropic reference atmosphere which includes the classical scaling using isothermal reference atmospheres as a special case.
536 _ _ |a Chemie und Dynamik der Geo-Biosphäre
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588 _ _ |a Dataset connected to Web of Science
650 _ 7 |a J
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700 1 _ |a Günther, G.
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773 _ _ |0 PERI:(DE-600)1462145-9
|a 10.1007/s00703-004-0087-6
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|t Meteorology and Atmospheric Physics
|v 90
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856 7 _ |u http://dx.doi.org/10.1007/s00703-004-0087-6
909 C O |o oai:juser.fz-juelich.de:35954
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914 1 _ |y 2005
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