Monin-Obukhov Similarity for Refractive Index RevisitedSource: Journal of the Atmospheric Sciences:;1993:;Volume( 050 ):;issue: 021::page 3677Author:Sorbjan, Zbigniew
DOI: 10.1175/1520-0469(1993)050<3677:MOSFRI>2.0.CO;2Publisher: American Meteorological Society
Abstract: Monin-Obukhov similarity applied to the real part of the refractive index variance n?2 is discussed. It is shown that, because the observed correlation coefficient rTQ between temperature and humidity is less than unity, scaling by n* = n?w?/u* (where u* is the friction velocity) makes the dimensionless variance n?2/n?*2 dependent on two dimensionless parameters, on dimensionless height z/L (where L is the Monin-Obukhov length), and on a parameter R, which is related to the Bowen ratio. As the Monin-Obukhov similarity framework is applied, a large scatter of the dimensionless refractive index variance is expected for certain values of the Bowen ratio. Such a scatter can be eliminated if a new scale N*, defined as a combination of temperature and humidity scales, is employed.
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| contributor author | Sorbjan, Zbigniew | |
| date accessioned | 2017-06-09T14:31:54Z | |
| date available | 2017-06-09T14:31:54Z | |
| date copyright | 1993/11/01 | |
| date issued | 1993 | |
| identifier issn | 0022-4928 | |
| identifier other | ams-21068.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4157366 | |
| description abstract | Monin-Obukhov similarity applied to the real part of the refractive index variance n?2 is discussed. It is shown that, because the observed correlation coefficient rTQ between temperature and humidity is less than unity, scaling by n* = n?w?/u* (where u* is the friction velocity) makes the dimensionless variance n?2/n?*2 dependent on two dimensionless parameters, on dimensionless height z/L (where L is the Monin-Obukhov length), and on a parameter R, which is related to the Bowen ratio. As the Monin-Obukhov similarity framework is applied, a large scatter of the dimensionless refractive index variance is expected for certain values of the Bowen ratio. Such a scatter can be eliminated if a new scale N*, defined as a combination of temperature and humidity scales, is employed. | |
| publisher | American Meteorological Society | |
| title | Monin-Obukhov Similarity for Refractive Index Revisited | |
| type | Journal Paper | |
| journal volume | 50 | |
| journal issue | 21 | |
| journal title | Journal of the Atmospheric Sciences | |
| identifier doi | 10.1175/1520-0469(1993)050<3677:MOSFRI>2.0.CO;2 | |
| journal fristpage | 3677 | |
| journal lastpage | 3679 | |
| tree | Journal of the Atmospheric Sciences:;1993:;Volume( 050 ):;issue: 021 | |
| contenttype | Fulltext |