1966
DOI: 10.1029/jz071i015p03729
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Gravity waves in a realistic atmosphere

Abstract: The atmospheric winds at ionospheric altitudes exhibit irregular short‐period wavelike components that have been observed through their distortion of meteor ionization trails and rocket vapor trails. An explanation for these components was proposed by Hines in his theory for internal atmospheric gravity waves in an isothermal medium. The isothermal theory is refined here to unify the treatment of acoustic, gravity, and evanescent waves in a gravitational atmosphere and to explain the physical processes behind … Show more

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Cited by 108 publications
(66 citation statements)
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“…The important aspects of these studies include: propagation characteristics of gravity waves in the realistic atmosphere (Midgley and Liemohn, 1966;Hines and Reddy, 1967;Lindzen, 1970), wave-mean flow interactions (Booker and Bretherton, 1967;Lindzen, 1973;Dunkerton, 1980;McIntyre, 1980), generation of turbulence and enhanced diffusion (Weinstock, 1976;Lindzen, 1981) and wave saturation and its effects (Fritts, 1984;Fritts and Rastogi, 1985). In recent years, the Rayleigh lidar technique has emerged as an effective means to study the gravity wave activity in the middle atmosphere over the height range of 30-70 km Hauchecorne, 1981, 1991;Wilson et al, 1990a, b;Gardner et al, 1989;Whiteway and Carswell, 1995;McDonald et al, 1998;Sivakumar et al, 2006;Ramkumar et al, 2006;Antonita et al, 2007).…”
Section: Introductionmentioning
confidence: 99%
“…The important aspects of these studies include: propagation characteristics of gravity waves in the realistic atmosphere (Midgley and Liemohn, 1966;Hines and Reddy, 1967;Lindzen, 1970), wave-mean flow interactions (Booker and Bretherton, 1967;Lindzen, 1973;Dunkerton, 1980;McIntyre, 1980), generation of turbulence and enhanced diffusion (Weinstock, 1976;Lindzen, 1981) and wave saturation and its effects (Fritts, 1984;Fritts and Rastogi, 1985). In recent years, the Rayleigh lidar technique has emerged as an effective means to study the gravity wave activity in the middle atmosphere over the height range of 30-70 km Hauchecorne, 1981, 1991;Wilson et al, 1990a, b;Gardner et al, 1989;Whiteway and Carswell, 1995;McDonald et al, 1998;Sivakumar et al, 2006;Ramkumar et al, 2006;Antonita et al, 2007).…”
Section: Introductionmentioning
confidence: 99%
“…1. Below 100km, we determine this value considering the results by JOHNSON and WILKINS (1965) and MIDGLEY and LIEMON (1966). Above 100km we choose the profile which rapidly decreases after KENESEA and ZIMMERMAN (1970).…”
Section: Co2mentioning
confidence: 99%
“…The flatearth and stratification assumptions limit the validity of our analysis to Al-waves. With these assumptions the hydrodynamical equations can be reduced to a set of six ordinary differential equations (Midgley and Liemohn 1966).…”
Section: Basic Equationsmentioning
confidence: 99%