A Generalization of Bernoulli's TheoremSource: Journal of the Atmospheric Sciences:;1993:;Volume( 050 ):;issue: 010::page 1437Author:Schär, Christoph
DOI: 10.1175/1520-0469(1993)050<1437:AGOBT>2.0.CO;2Publisher: American Meteorological Society
Abstract: The conservation of potential vorticity Q can be expressed as ?(?Q/?t + ?·J = 0, where J denotes the total flux of potential vorticity. It is shown that J is related under statistically steady conditions to the Bernoulli function B by J = ?? ? ?B,where ? is the potential temperature. This relation is valid even in the nonhydrostatic limit and in the presence of arbitrary nonconservative forces (such as internal friction) and heating rates. In essence, it can be interpreted as a generalization of Bernoulli's theorem to the frictional and diabatic regime. The classical Bernoulli theorem?valid for inviscid adiabatic and steady flows?states that the intersections of surfaces of constant potential temperature and constant Bernoulli function yield streamlines. In the presence of frictional and diabatic effects, these intersections yield the flux lines along which potential vorticity is transported.
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| contributor author | Schär, Christoph | |
| date accessioned | 2017-06-09T14:31:27Z | |
| date available | 2017-06-09T14:31:27Z | |
| date copyright | 1993/05/01 | |
| date issued | 1993 | |
| identifier issn | 0022-4928 | |
| identifier other | ams-20916.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4157197 | |
| description abstract | The conservation of potential vorticity Q can be expressed as ?(?Q/?t + ?·J = 0, where J denotes the total flux of potential vorticity. It is shown that J is related under statistically steady conditions to the Bernoulli function B by J = ?? ? ?B,where ? is the potential temperature. This relation is valid even in the nonhydrostatic limit and in the presence of arbitrary nonconservative forces (such as internal friction) and heating rates. In essence, it can be interpreted as a generalization of Bernoulli's theorem to the frictional and diabatic regime. The classical Bernoulli theorem?valid for inviscid adiabatic and steady flows?states that the intersections of surfaces of constant potential temperature and constant Bernoulli function yield streamlines. In the presence of frictional and diabatic effects, these intersections yield the flux lines along which potential vorticity is transported. | |
| publisher | American Meteorological Society | |
| title | A Generalization of Bernoulli's Theorem | |
| type | Journal Paper | |
| journal volume | 50 | |
| journal issue | 10 | |
| journal title | Journal of the Atmospheric Sciences | |
| identifier doi | 10.1175/1520-0469(1993)050<1437:AGOBT>2.0.CO;2 | |
| journal fristpage | 1437 | |
| journal lastpage | 1443 | |
| tree | Journal of the Atmospheric Sciences:;1993:;Volume( 050 ):;issue: 010 | |
| contenttype | Fulltext |