The Combined Effect of Temperature and Humidity Fluctuations on Refractive IndexSource: Journal of Applied Meteorology:;1976:;volume( 015 ):;issue: 001::page 43Author:Wesely, Marvin L.
DOI: 10.1175/1520-0450(1976)015<0043:TCEOTA>2.0.CO;2Publisher: American Meteorological Society
Abstract: Depending on whether the radiation under consideration is acoustic, visible or microwave, either temperature or humidity fluctuations are ordinarily assumed to be an insignificant source of refractive index fluctuations. For applications in the atmospheric surface layer or in a free convection layer, the value of the local Bowen ratio ?, which is the ratio of sensible to latent heat flux densities, can be used to determine when variations in both temperature T and water vapor pressure e are important considerations. When |?| < 0.3 for applications involving visible radiation, |?| < 0.6 for acoustic radiation, and |?|>0.32 for microwave radiation, both T and e fluctuations have at least a 10% effect on the amplitudes of refractive index fluctuations, provided T and e are highly correlated. If T and e are uncorrelated, this 10% level is |?| < 0.067, |?| < 0.13 and |?| > 1.45 for acoustic, visible and microwave radiation, respectively. With knowledge of ? and the extent of the T and e correlation, refractive index ?fluxes? and structure function coefficients can be calculated from (or inversely, can be used to calculate) the corresponding parameters for temperature and humidity.
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| contributor author | Wesely, Marvin L. | |
| date accessioned | 2017-06-09T17:38:28Z | |
| date available | 2017-06-09T17:38:28Z | |
| date copyright | 1976/01/01 | |
| date issued | 1976 | |
| identifier issn | 0021-8952 | |
| identifier other | ams-9016.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4232458 | |
| description abstract | Depending on whether the radiation under consideration is acoustic, visible or microwave, either temperature or humidity fluctuations are ordinarily assumed to be an insignificant source of refractive index fluctuations. For applications in the atmospheric surface layer or in a free convection layer, the value of the local Bowen ratio ?, which is the ratio of sensible to latent heat flux densities, can be used to determine when variations in both temperature T and water vapor pressure e are important considerations. When |?| < 0.3 for applications involving visible radiation, |?| < 0.6 for acoustic radiation, and |?|>0.32 for microwave radiation, both T and e fluctuations have at least a 10% effect on the amplitudes of refractive index fluctuations, provided T and e are highly correlated. If T and e are uncorrelated, this 10% level is |?| < 0.067, |?| < 0.13 and |?| > 1.45 for acoustic, visible and microwave radiation, respectively. With knowledge of ? and the extent of the T and e correlation, refractive index ?fluxes? and structure function coefficients can be calculated from (or inversely, can be used to calculate) the corresponding parameters for temperature and humidity. | |
| publisher | American Meteorological Society | |
| title | The Combined Effect of Temperature and Humidity Fluctuations on Refractive Index | |
| type | Journal Paper | |
| journal volume | 15 | |
| journal issue | 1 | |
| journal title | Journal of Applied Meteorology | |
| identifier doi | 10.1175/1520-0450(1976)015<0043:TCEOTA>2.0.CO;2 | |
| journal fristpage | 43 | |
| journal lastpage | 49 | |
| tree | Journal of Applied Meteorology:;1976:;volume( 015 ):;issue: 001 | |
| contenttype | Fulltext |