Two-Point Wind Correlations on an Isobaric Surface in a Nonhomogeneous Non-Isotropic AtmosphereSource: Journal of Applied Meteorology:;1971:;volume( 010 ):;issue: 006::page 1266Author:Buell, C. Eugene
DOI: 10.1175/1520-0450(1971)010<1266:TPWCOA>2.0.CO;2Publisher: American Meteorological Society
Abstract: The approximate relations between the correlation coefficient for geopotential, the longitudinal wind component, and the transverse wind component on an isobaric surface in the case of an homogeneous isotropic atmosphere are discussed briefly. Corresponding approximate relations for a nonhomogeneous and non-isotropic atmosphere are presented. The mixed correlations for wind component (longitudinal with transverse, and vice versa) are no longer identically zero (as was the case for the homogeneous isotropic atmosphere). Approximate expressions for these mixed correlation coefficient functions are presented in terms of the correlation coefficient for geopotential. It is shown that the general configuration of values computed from observed winds are those expected from theoretical considerations.
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| contributor author | Buell, C. Eugene | |
| date accessioned | 2017-06-09T17:17:55Z | |
| date available | 2017-06-09T17:17:55Z | |
| date copyright | 1971/12/01 | |
| date issued | 1971 | |
| identifier issn | 0021-8952 | |
| identifier other | ams-8267.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4225811 | |
| description abstract | The approximate relations between the correlation coefficient for geopotential, the longitudinal wind component, and the transverse wind component on an isobaric surface in the case of an homogeneous isotropic atmosphere are discussed briefly. Corresponding approximate relations for a nonhomogeneous and non-isotropic atmosphere are presented. The mixed correlations for wind component (longitudinal with transverse, and vice versa) are no longer identically zero (as was the case for the homogeneous isotropic atmosphere). Approximate expressions for these mixed correlation coefficient functions are presented in terms of the correlation coefficient for geopotential. It is shown that the general configuration of values computed from observed winds are those expected from theoretical considerations. | |
| publisher | American Meteorological Society | |
| title | Two-Point Wind Correlations on an Isobaric Surface in a Nonhomogeneous Non-Isotropic Atmosphere | |
| type | Journal Paper | |
| journal volume | 10 | |
| journal issue | 6 | |
| journal title | Journal of Applied Meteorology | |
| identifier doi | 10.1175/1520-0450(1971)010<1266:TPWCOA>2.0.CO;2 | |
| journal fristpage | 1266 | |
| journal lastpage | 1274 | |
| tree | Journal of Applied Meteorology:;1971:;volume( 010 ):;issue: 006 | |
| contenttype | Fulltext |