Author: James Robert Barnum
Publisher:
ISBN:
Category : Electronic data processing
Languages : en
Pages : 124
Book Description
Twenty-four hour high-resolution FMCW soundings taken over an East-West 1900-km forward-propagation path show unexpectedly complex mode structure near sunset. Because of the presence of 1- and 2-hop sporadic-E modes, it was suggested that multiple reflections from sporadic-E and F-layers--such as 'M' and 'N' modes--accounted for much of the unexplained structure. This work represents an attempt to see how well these 'mixed' modes can be understood by employing computer ray-tracing procedures developed by Dr. T.A. Croft. A simple beta-Chapman layer, with its parameters adjusted to give synthetic ionograms that matched the experimental 1- and 2-hop F-layer modes, proved to be an adequate model for the F-layer profile over the path. Reference to the calibrated experimental ionograms yielded values for the sporadic-E reflection heights for each time of day. Assuming no horizontal tilts in layer density and ignoring the earth's magnetic field, synthetic ionograms involving multiple F-layer and sporadic-E reflections were then computed. The model-experiment comparisons show that surprisingly accurate estimations of both 1- and 2-hop and mixed modes are possible, using only relatively simple computational procedures. Although similar work has been done in this area, the present study is novel in its use of calibrated oblique ionograms for model derivation. The work should lead to a better understanding of both HF forward and backscatter propagation studies which are plagued with multiple, interlayer propagation modes. (Author).
Mixed-mode Oblique Ionograms: a Computer Ray-tracing Interpretation
Author: James Robert Barnum
Publisher:
ISBN:
Category : Electronic data processing
Languages : en
Pages : 124
Book Description
Twenty-four hour high-resolution FMCW soundings taken over an East-West 1900-km forward-propagation path show unexpectedly complex mode structure near sunset. Because of the presence of 1- and 2-hop sporadic-E modes, it was suggested that multiple reflections from sporadic-E and F-layers--such as 'M' and 'N' modes--accounted for much of the unexplained structure. This work represents an attempt to see how well these 'mixed' modes can be understood by employing computer ray-tracing procedures developed by Dr. T.A. Croft. A simple beta-Chapman layer, with its parameters adjusted to give synthetic ionograms that matched the experimental 1- and 2-hop F-layer modes, proved to be an adequate model for the F-layer profile over the path. Reference to the calibrated experimental ionograms yielded values for the sporadic-E reflection heights for each time of day. Assuming no horizontal tilts in layer density and ignoring the earth's magnetic field, synthetic ionograms involving multiple F-layer and sporadic-E reflections were then computed. The model-experiment comparisons show that surprisingly accurate estimations of both 1- and 2-hop and mixed modes are possible, using only relatively simple computational procedures. Although similar work has been done in this area, the present study is novel in its use of calibrated oblique ionograms for model derivation. The work should lead to a better understanding of both HF forward and backscatter propagation studies which are plagued with multiple, interlayer propagation modes. (Author).
Publisher:
ISBN:
Category : Electronic data processing
Languages : en
Pages : 124
Book Description
Twenty-four hour high-resolution FMCW soundings taken over an East-West 1900-km forward-propagation path show unexpectedly complex mode structure near sunset. Because of the presence of 1- and 2-hop sporadic-E modes, it was suggested that multiple reflections from sporadic-E and F-layers--such as 'M' and 'N' modes--accounted for much of the unexplained structure. This work represents an attempt to see how well these 'mixed' modes can be understood by employing computer ray-tracing procedures developed by Dr. T.A. Croft. A simple beta-Chapman layer, with its parameters adjusted to give synthetic ionograms that matched the experimental 1- and 2-hop F-layer modes, proved to be an adequate model for the F-layer profile over the path. Reference to the calibrated experimental ionograms yielded values for the sporadic-E reflection heights for each time of day. Assuming no horizontal tilts in layer density and ignoring the earth's magnetic field, synthetic ionograms involving multiple F-layer and sporadic-E reflections were then computed. The model-experiment comparisons show that surprisingly accurate estimations of both 1- and 2-hop and mixed modes are possible, using only relatively simple computational procedures. Although similar work has been done in this area, the present study is novel in its use of calibrated oblique ionograms for model derivation. The work should lead to a better understanding of both HF forward and backscatter propagation studies which are plagued with multiple, interlayer propagation modes. (Author).
Technical Abstract Bulletin
Quarterly Status Report No.112, October Through December 1968
Author: Stanford University. Stanford Electronics Laboratories
Publisher:
ISBN:
Category :
Languages : en
Pages : 114
Book Description
Publisher:
ISBN:
Category :
Languages : en
Pages : 114
Book Description
Masters Theses and Doctoral Dissertations in the Pure and Applied Sciences Accepted by Colleges and Universities of the United States
The Effect of Polarization Rotation on the Amplitude of Ionospherically-propagated Sea Backscatter
Author: Stanford University. Stanford Electronics Laboratories
Publisher:
ISBN:
Category : Ionospheric radio wave propagation
Languages : en
Pages : 234
Book Description
Previous experiments have shown that an ocean surface represents a strong source of high-frequency (HF) backscatter. The author has used a 2.5 km receiving antenna array--the world's largest--to study such backscatter both from the Gulf of Mexico and the Pacific Ocean. The narrow beamwidth of this antenna (1/3 deg average), together with SFCW sounding, confer unusually good azimuth and time-delay (range) resolution. The resulting detail and clarity has made possible more precise quantitative studies of sea backscatter. A particular goal of these studies is to develop a method of locating storms, or areas of unusual calm. (Author).
Publisher:
ISBN:
Category : Ionospheric radio wave propagation
Languages : en
Pages : 234
Book Description
Previous experiments have shown that an ocean surface represents a strong source of high-frequency (HF) backscatter. The author has used a 2.5 km receiving antenna array--the world's largest--to study such backscatter both from the Gulf of Mexico and the Pacific Ocean. The narrow beamwidth of this antenna (1/3 deg average), together with SFCW sounding, confer unusually good azimuth and time-delay (range) resolution. The resulting detail and clarity has made possible more precise quantitative studies of sea backscatter. A particular goal of these studies is to develop a method of locating storms, or areas of unusual calm. (Author).
Publications of Stanford University Radioscience Laboratory, 1968-1972
Master's Theses and Doctoral Dissertations in the Pure and Applied Sciences
Author:
Publisher:
ISBN:
Category : Dissertations, Academic
Languages : en
Pages : 172
Book Description
Publisher:
ISBN:
Category : Dissertations, Academic
Languages : en
Pages : 172
Book Description
Government Reports Announcements & Index
Author:
Publisher:
ISBN:
Category : Government publications
Languages : en
Pages : 1136
Book Description
Publisher:
ISBN:
Category : Government publications
Languages : en
Pages : 1136
Book Description