Author: V. S. Whitehead
Publisher:
ISBN:
Category :
Languages : en
Pages : 86
Book Description
Synoptic charts of pressure, temperature, and density as determined by the wind field were prepared to 56 km altitude. These charts indicate that synoptic scale perturbations similar in extent to those found in the troposphere and lower stratosphere exist to at least up to that height. Mean monthly meridional cross-sections of density distribution as determined by the wind field are given to 80 km altitude. These cross sections depict well the known lower level features of the density distribution and suggest an orderly change in the mesospheric density pattern as the seasons progress. Diurnal and semidiurnal oscillations of isopycnic surfaces at 20N, 30N, and 40N for summer and for winter are given to 80 km. The amplitude of the diurnal wave appears to increase rapidly above 50 km with the phase shifting eastward with height to 80 km. Three atmospheric models are presented in which absorption of solar radiant energy and the downward conduction of heat are the only heat transfer processes. These models were intended to simulate, to some extent, the atmosphere between 90 and 200 km. Discrepancies between the three models, however, discourage their use for their intended purpose, but do suggest methods for developing improved models. (Author).
Atmospheric Structure and Circulation to 200 Km in Terms of Density
Author: V. S. Whitehead
Publisher:
ISBN:
Category :
Languages : en
Pages : 86
Book Description
Synoptic charts of pressure, temperature, and density as determined by the wind field were prepared to 56 km altitude. These charts indicate that synoptic scale perturbations similar in extent to those found in the troposphere and lower stratosphere exist to at least up to that height. Mean monthly meridional cross-sections of density distribution as determined by the wind field are given to 80 km altitude. These cross sections depict well the known lower level features of the density distribution and suggest an orderly change in the mesospheric density pattern as the seasons progress. Diurnal and semidiurnal oscillations of isopycnic surfaces at 20N, 30N, and 40N for summer and for winter are given to 80 km. The amplitude of the diurnal wave appears to increase rapidly above 50 km with the phase shifting eastward with height to 80 km. Three atmospheric models are presented in which absorption of solar radiant energy and the downward conduction of heat are the only heat transfer processes. These models were intended to simulate, to some extent, the atmosphere between 90 and 200 km. Discrepancies between the three models, however, discourage their use for their intended purpose, but do suggest methods for developing improved models. (Author).
Publisher:
ISBN:
Category :
Languages : en
Pages : 86
Book Description
Synoptic charts of pressure, temperature, and density as determined by the wind field were prepared to 56 km altitude. These charts indicate that synoptic scale perturbations similar in extent to those found in the troposphere and lower stratosphere exist to at least up to that height. Mean monthly meridional cross-sections of density distribution as determined by the wind field are given to 80 km altitude. These cross sections depict well the known lower level features of the density distribution and suggest an orderly change in the mesospheric density pattern as the seasons progress. Diurnal and semidiurnal oscillations of isopycnic surfaces at 20N, 30N, and 40N for summer and for winter are given to 80 km. The amplitude of the diurnal wave appears to increase rapidly above 50 km with the phase shifting eastward with height to 80 km. Three atmospheric models are presented in which absorption of solar radiant energy and the downward conduction of heat are the only heat transfer processes. These models were intended to simulate, to some extent, the atmosphere between 90 and 200 km. Discrepancies between the three models, however, discourage their use for their intended purpose, but do suggest methods for developing improved models. (Author).
Progress on a Study of Atmospheric Circulation to 200 Kilometers in Terms of Density
Author: V. S. Whitehead
Publisher:
ISBN:
Category :
Languages : en
Pages : 51
Book Description
This report presents a summary of the results to date of a study of circulation to 200 km altitude in terms of density. Equations are developed which describe the behavior of density in hydrostatic atmospheres in general. The effects of vetical motion on the density departure from standard is shown for three hypothetical atmospheres. A method is developed for determination of the slopes of constant density surfaces from the wind field. The results of applying this method to the wind data taken from the Meteoralogical Rocket Network are given. A simple two-dimensional model for the atmosphere between 90 and 220 km is constructed. This model is based on assumed equilibrium between absorption of solar electromagnetic radiation and downward conduction of thermal energy. (Author).
Publisher:
ISBN:
Category :
Languages : en
Pages : 51
Book Description
This report presents a summary of the results to date of a study of circulation to 200 km altitude in terms of density. Equations are developed which describe the behavior of density in hydrostatic atmospheres in general. The effects of vetical motion on the density departure from standard is shown for three hypothetical atmospheres. A method is developed for determination of the slopes of constant density surfaces from the wind field. The results of applying this method to the wind data taken from the Meteoralogical Rocket Network are given. A simple two-dimensional model for the atmosphere between 90 and 220 km is constructed. This model is based on assumed equilibrium between absorption of solar electromagnetic radiation and downward conduction of thermal energy. (Author).
Technical Abstract Bulletin
Author:
Publisher:
ISBN:
Category : Science
Languages : en
Pages : 684
Book Description
Publisher:
ISBN:
Category : Science
Languages : en
Pages : 684
Book Description
Scientific and Technical Aerospace Reports
Author:
Publisher:
ISBN:
Category : Aeronautics
Languages : en
Pages : 240
Book Description
Publisher:
ISBN:
Category : Aeronautics
Languages : en
Pages : 240
Book Description
U. S. Government Research and Development Reports
Author:
Publisher:
ISBN:
Category : Science
Languages : en
Pages : 1776
Book Description
Publisher:
ISBN:
Category : Science
Languages : en
Pages : 1776
Book Description
Atmospheric Pressure, Density, Temperature and Wind Variations Between 50 and 200 Km
Author: Carl Gerald Justus
Publisher:
ISBN:
Category : Meteorology
Languages : en
Pages : 92
Book Description
Publisher:
ISBN:
Category : Meteorology
Languages : en
Pages : 92
Book Description
Government-wide Index to Federal Research & Development Reports
Author:
Publisher:
ISBN:
Category : Government publications
Languages : en
Pages : 760
Book Description
Publisher:
ISBN:
Category : Government publications
Languages : en
Pages : 760
Book Description
Atmospheric Structure and Its Variations in the Lower Thermosphere
Author: K. S. W. Champion
Publisher:
ISBN:
Category : Atmosphere, Upper
Languages : en
Pages : 36
Book Description
Publisher:
ISBN:
Category : Atmosphere, Upper
Languages : en
Pages : 36
Book Description
Air Force Research Resumés
Author:
Publisher:
ISBN:
Category : Military research
Languages : en
Pages : 592
Book Description
Publisher:
ISBN:
Category : Military research
Languages : en
Pages : 592
Book Description
OAR Cumulative Index of Research Results
Author:
Publisher:
ISBN:
Category : Aeronautics
Languages : en
Pages : 576
Book Description
Publisher:
ISBN:
Category : Aeronautics
Languages : en
Pages : 576
Book Description