RADIO WAVE PROPAGATION (Topics)
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Compact Bilateral Single Conductor Surface Wave Transmission Line
Compact bilateral single conductor Regarded as half mode CPW, a series of slotlines have been proposed whose characteristic impedance is easy to control [7]. The bilateral surface wave transmission line slotline with 50 ohm characteristic impedance is designed as shown in Fig. 2. The copper layers on both sides of the substrate are connected by Zhixia Xu, Shunli Li, Hongxin Zhao, Leilei Liu and the metalized via arrays, and the two via arrays can increase the perunit- Xiaoxing Yin length capacitance and decrease characteristic impedance to 50 ohm which is usually quite high for a conventional slotline. The height of via A compact bilateral single conductor surface wave transmission line h is 1.524 mm, the slot S is 0.3 mm; the space between via arrays d is (TL) is proposed, converting the quasi-transverse electromagnetic 0.4 mm; the space between neighbour vias a is 1 mm. (QTEM) mode of low characteristic impedance slotline into the As a single conductor TL, bilateral corrugated metallic strips are transverse magnetic (TM) mode of single-conductor TL. The propagation constant of the proposed TL is decided by geometric printed on both sides of the substrate and connected by via arrays the parameters of the periodic corrugated structure. Compared to configuration is shown in Fig. 3a. To excite the transverse magnetic conventional transitions between coplanar waveguide (CPW) and (TM) mode, the surface mode of the corrugated strip, from the quasi- single-conductor TLs, such as Goubau line (G-Line) and surface transverse electromagnetic (QTEM) mode, the mode of slotline, we plasmons TL, the proposed structure halves the size and this feature propose a compact bilateral transition structure, as shown in Fig. -
Long Earthquake'waves
~ LONG EARTHQUAKE'WAVES Seisllloloo-istsLl are tuning their instnlments to record earth 1l10tiollS with periods of one Jninute to an hour and mllplitudes of less than .01 inch. These,,~aycs tell llluch about the earth's crust and HHltltle by Jack Oliver "lhe hi-H enthusiast who hitS strug· per cycle. A reI.ltlvely shorr earthquake earth'luake waves tmvel at .9 to 1.S 1 gled to ImprO\'e tlIe re;pollse of wave has a duration of 10 seconds. At miles per second, they lange in length hI:; e'jlllpment In the bass range at present the most infornl.1tive long waves from 10 mile" up to the 8,OOO-mde length .11 oUlld 10 c~'d(-s per ;econd wIll ha VI" a h,\v€ periods of 15 to 75 seconds from of the earth's ,hamete... TheIr amplitude, fellow-feeling for the selsmologi;t \vho CfEst to crest. \Vith more advanced in however, is of an entirely di/lerent 01 de.. : IS ,attempting to tune hiS installments to ,,11 uments seismologists hope sooo to one of these waves displaces a point on the longest earth'luake \\".\\'es. But where study 450-second waves. The longest so the sudace of the eal th at some dislil1lce IIl-n deals in cITIes per second, seisll1OIo" f.tr detected had ., penod of :3,400 sec from the shock by no more than a hun· gy measures its fre<luencle; 111 seconds onds-·nearly an hour! Since these long dredth of an inch, even when eXCited by t/) ~ ~ SUBTERRANEAN TOPOGRAPHY of the North American con· at which the depth of the boundary was established. -
Surface Waves: What Are They? Why Are They Interesting?
SURFACE WAVES: WHAT ARE THEY? WHY ARE THEY INTERESTING? Janice Hendry Roke Manor Research Limited, Old Salisbury Lane, Romsey, SO51 0ZN, UK [email protected] ABSTRACT Surface waves have been known about for many decades and quite in-depth research took place up until ~1960s . Since then, little work has been done in this area. It is unclear why, however today we have more powerful modelling methods which may enable us to understand their use better. It is known that high frequency (HF) surface waves follow the terrain and this has been utilised in some cases such as Raytheon's HF surface wave radar (HFSWR) for detecting ships over-the-horizon. It is thought with some more insight and knowledge of this phenomenon, surface waves could be extremely useful for both military and civil use, from communications to agriculture. WHAT ARE SURFACE WAVES? Over the many decades that surface waves have been researched, some confusion has built up over exactly what constitutes a surface wave. This was discussed by James Wait in an IEE Transaction in 1965 1 and was even a matter of discussion at the General Assembly of International Union of Radio Science (URSI) held in London in 1960. It was concluded that “there is no neat definition which would encompass all forms of wave which could glide or be guided along an interface”. However, the definitions which have been settled upon for this paper are as follows: Surface Wave Region : The region of interest in which the surface wave propagates. Surface Wave : A surface wave is one that propagates along an interface between two different media without radiation; such radiation being construed to mean energy converted from the surface wave field to some other form. -
A Simplified Mathematical Model to Calculate the Maximum Usable Frequencies Over Iraqi Territory Khalid A
A Simplified Mathematical Model to Calculate the Maximum Usable Frequencies Over Iraqi Territory Khalid A. Hadi*, Loay E. Goerge** A Simplified Mathematical Model to Calculate the Maximum Usable Frequencies Over Iraqi Territory Khalid A. Hadi*, Loay E. Goerge** * Department of Astronomy & Space, College of Science, University of Baghdad ** Department of Computer Science, College of Science, University of Baghdad Receiving Date: 25-02-2011 - Accept Date: 13-06-2011 Abstract In this project, the spatial and temporal variation of maximum usable frequency (MUF) parameter is investigated and modeled. The values of MUF for Baghdad station links, with other stations distributed over Iraq territory, where determined using the international reference model (RECF533) for HF propagation. The determined MUF dataset reflected that the spatial distribution of this parameter for Baghdad station shows circular symmetry, which stimulated the possibility of using a two dimensional second order polynomial in order to describe MUF variation. The main feature of this adopted mathematical model is its low complexity. The results of conducted analysis indicated that the spatial variation of MUF is simple while its temporal variation is more complicated and needs more sophisticated mathematical description than the polynomial description. The test results showed that the accuracy of proposed simple model lies within the tolerance of REC533 reference model. Key words: Ionosphere, HF communication prediction, MUF Vol 7 No: 4, October 2011 1 20 ISSN: 2222-8373 A Simplified Mathematical Model to Calculate the Maximum Usable Frequencies Over Iraqi Territory 1. INTRODUCTION The Maximum Usable Frequency, denoted by MUF, is an important ionospheric parameter. It is defined as the highest frequency that allows reliable long-range high frequency (HF) radio communication between two points due to ion-ospheric refraction. -
Using High Frequency Propagation to Calculate Basic Maximum Usable Frequency
Using High Frequency Propagation to Calculate Basic Maximum Usable Frequency Israa Abdualqassim Mohammed Ali* * University of Baghdad, College of Science, Baghdad, Iraq Received: XX 20XX / Accepted: XX 20XX / Published online: ABSTRACT A comparison between observed (obs.) digital ionospheric sounding data and predicted (pre.) using International Reference Ionosphere (IRI) model for critical frequency (foF2) and Basic Maximum Usable Frequency (BMUF) of ionospheric F2-Layer has been made. A mid-latitude region selected for this research work by using data from station Wakkanai (45.38o N, 141.66o E). This study included 12 monthly median data from year (2001, R12=111) selected for high Sunspot number (SSN) and years for low SSN (2004, R12=44) and (2005, R12=29). Frequency parameters foF2 reveals that there is a good correlation between observed and predicted except for January of years 2001 and 2004, and BMUF revealed that there is a good correlation between observed and predicted for years of low SSN and all months except in month 1, 9 and 12 of year 2004, for year 2001 of high SSN there is a bad correlation. A correction factor as a function of time used from fitting technique to correct the predicted value with observed value of BMUF for year 2001. Keywords: Ionosphere; foF2; M3000F2; BMUF Author Correspondence, e-mail: [email protected] 1. INTRODUCTION The maximum usable frequency (MUF) is important ionospheric parameter for radio users because of its role in radio frequency management and for providing a good communication 1 link between two locations (Athieno et al., 2015; Suparta et al., 2018). -
Sky-Wave Propagation
ANTENNA AND WAVE PROPAGATION Introduction Electromagnetic Wave(Radio Waves) travel with a vel. of light. These waves comprises of both Electric and Magnetic Field. The two fields are at right-angles to each other and the direction of propagation is at right-angles to both fields. The Plane of the Electric Field defines the Polarisation of the wave. Field Strength Relationship Electric Field, E x y Magnetic Direction of Field, H z Propagation Electromagnetic Wave(Radio Waves) travel with a vel. of light. These waves comprises of both Electric and Magnetic Field. The two fields are at right-angles to each other and the direction of propagation is at right-angles to both fields. The Plane of the Electric Field defines the Polarisation of the wave. POLARIZATION The polarization of an antenna is the orientation of the electric field with respect to the Earth's surface. Polarization of e.m. Wave is determined by the physical structure of the antenna and by its orientation. Radio waves from a vertical antenna will usually be vertically polarized. Radio waves from a horizontal antenna are usually horizontally polarized. Classification of Radio Wave Propagation GROUND WAVE, SPACE WAVE, SKY WAVE Ground Waves or Surface Waves Ground Waves or Surface Waves ◦ Frequencies up to 2 MHz ◦ follows the curvature of the earth and can travel at distances beyond the horizon (upto some km) ◦ must have vertically polarized antennas ◦ strongest at the low- and medium-frequency ranges ◦ AM broadcast signals are propagated primarily by ground waves during the day and by sky waves at nightis a Surface Wave that propagates or travels close to the surface of the Earth. -
Interpretation and Utilization of the Echo
PROCEEDINGS OF THE IEEE, VOL. 62, NO. 6, JUNE 1974 673 Sea Backscatter at HF: Interpretation and Utilization of the Echo DONALD E. BARRICK, MEMBER, IEEE, JAMES M. HEADRICK, SENIOR MEMBER, IEEE, ROBERT W. BOGLE, DOUGLASS D. CROMBIE AND Abstract-Theories and concepts for utilization of HF sea echo are compared and tested against surface-wave measurements made from San Clemente Island in the Pacific in a joint NRL/ITS/NOAA Although the heights of ocean waves are generally small experiment. The use of first-order sea echo as a reference target for in terms of these radar wavelengths, the scattered echo is calibration of HF over-the-horizon radars is established. Features of the higher order Doppler spectrum can be employed to deduce the nonetheless surprisingly large and readily interpretable in principal parameters of the wave-height directional. spectrum (i.e., terms of its Doppler features. The fact that these heights are sea state); and it is shown that significant wave height can be read small facilitates the analysis of scatter using the perturbation from the spectral records. Finally, it is shown that surface currents approximation. This theory [2] produces an equation which and current (depth) gradients can be inferred from the same Doppler 1) agrees with the scattering mechanism deduced by Crombie sea-echo records. from experimental data; 2) properly predicts the positions of I. INTRODUCTION the dominant Doppler peaks; 3) shows how the dominant echo magnitude is related to the sea wave height; and 4) per mits an explanation of some of the less dominant, more com T WENTY YEARS ago Crombie [1] observed sea echo plex features of the sea echo through retention and use of the with an HF radar, and he correctly deduced the scatter higher order terms in the perturbation analysis. -
Radio Transmission and the Ionosphere
Ih S. DEPARTMENT OF COMMERCE NATIONAL BUREAU OF STANDARDS WASHINGTON / » ruT O v / Letter Circular LC-614 RADIO TRANSMISSION AND THE IONOSPHERE October 23, 19^0 6 . s TKD :ANK U. 3. DEPARTMENT OF COMMERCE Letter 1-6 NATIONAL BUREAU OF STANDARDS Circular Washington LC-6l4 ( Supersedes LC-E75) October 23 , 19^0 RADIO TRANSMISSION' AND THE IONOSPHERE Radio transmission over great distances is made possible by . reflection of the radio waves from ionized (electrically conduct- ing) layers in the ionosphere, the upper region of the earth* atmosphere. How far the radio waves go, and what frequencies may be used, are determined by the heights and the degree of ionization of the ionized layers, which are located between about BO kilometers (30 miles) and 400 kilometers (250 miles) above the earth's surface. Because of variations in the ionized layers, the conditions of radio wave transmission vary with time of day, with season, and from year to year. For the efficient maintenance of radio services it is important to have a constant supply of information on these changes. To this end an ionosphere observing, reporting, and predicting service is provided by the National Bureau of Standards. It is analogous to the weather reporting service, though quite independent of it-; the factors producing or affecting weather exist at much lower levels of the atmosphere than the ionosphere. The results of the Bureau * work on the ionosphere arid -radio transmission are made available to the public by a Science Service Urslgram and radio broadcast each week, and regular publication each month and each quarter, as well as through special papers (see References at end hereof) published from time to time on particular phases of the subject. -
Radio Communications
RADIO COMMUNICATIONS An Amateur Radio Technician and General Class License Study Guide Prepared by John Nordlund – AD5FU and Edited by Lynette Dowdy - KD5QMD Based on the Element 2 Technician Exam Question Pool Valid from 7/1/06 until 7/1/2010 and the Element 3 General Exam Question Pool Valid 7/1/2007 until 7/1/2011 Page 1 of 78 Acknowledgment: My greatest thanks to Lynette – KD5QMD, for her understanding and assistance, without which this book would be filled with countless typographical and grammatical errors and an overload of confusing jargon and bewildering techno-babble. | | This publication is the intellectual property of the author, and may not be reproduced for commercial gain for any purpose without the express permission of the author. | | However, Share the Fun. | | This publication may be freely distributed for the educational benefit of any who would care to obtain or upgrade their amateur radio license. | | | If you love the hobby you have a duty of honor to pass it along to the next generation. | | | 73 de AD5FU Page 2 of 78 How to use this study guide. Contained within the next 73 pages is a text derived from the official exam question pools for Element 2 Technician and Element 3 General class exams. It is the expressed opinion of the author and editor of this study guide that studying the full question pool text is counterproductive in attempting to obtain your Amateur Radio License. We therefore do not recommend downloading the actual exam question pool texts. This study guide is divided into sections of related information. -
HF Radio Propagation
Introduction to HF Radio Propagation 1. The Ionosphere 1.1 The Regions of the Ionosphere In a region extending from a height of about 50 km to over 500 km, most of the molecules of the atmosphere are ionised by radiation from the Sun. This region is called the ionosphere (see Figure 1.1). Ionisation is the process in which electrons, which are negatively charged, are removed from neutral atoms or molecules to leave positively charged ions and free electrons. It is the ions that give their name to the ionosphere, but it is the much lighter and more freely moving electrons which are important in terms of HF (high frequency) radio propagation. The free electrons in the ionosphere cause HF radio waves to be refracted (bent) and eventually reflected back to earth. The greater the density of electrons, the higher the frequencies that can be reflected. During the day there may be four regions present called the D, E, F1 and F2 regions. Their approximate height ranges are: • D region 50 to 90 km; • E region 90 to 140 km; • F1 region 140 to 210 km; • F2 region over 210 km. At certain times during the solar cycle the F1 region may not be distinct from the F2 region with the two merging to form an F region. At night the D, E and F1 regions become very much depleted of free electrons, leaving only the F2 region available for communications. Only the E, F1 and F2 regions refract HF waves. The D region is very important though, because while it does not refract HF radio waves, it does absorb or attenuate them (see Section 1.5). -
Comparison of Maximum Usable Frequency (MUF) Variability Over Peninsular Malaysia with IRI Model During the Rise of Solar Cycle 24
Journal of Atmospheric and Solar-Terrestrial Physics 138-139 (2016) 87–92 Contents lists available at ScienceDirect Journal of Atmospheric and Solar-Terrestrial Physics journal homepage: www.elsevier.com/locate/jastp Research paper Comparison of maximum usable frequency (MUF) variability over Peninsular Malaysia with IRI model during the rise of solar cycle 24 R.A. Malik a,b,n, M. Abdullah a,c, S. Abdullah c, M.J. Homam d a Department of Electrical, Electronic and Systems Engineering, Universiti Kebangsaan Malaysia, Malaysia b Science & Technology Research Institute for Defence (STRIDE), Malaysia c Space Science Centre (ANGKASA), Universiti Kebangsaan Malaysia, Malaysia d Universiti Tun Hussein Onn Malaysia, Malaysia article info abstract Article history: The aim of this paper is to study maximum usable frequency (MUF) variability over Peninsular Malaysia Received 27 July 2015 (112.5°E, 2.5°N) which is located in the equatorial region during the rise of Solar Cycle 24 (2009–2011). Received in revised form The MUF Test data was obtained from high frequency (HF) transmission tests that were conducted from 16 December 2015 April 2009 to September 2011. Relative variability VR was used to compute the relative variability of MUF. Accepted 26 December 2015 Variability of diurnal, seasonal and sunspot effect on MUF of test was compared to International Re- Available online 29 December 2015 ference Ionosphere (IRI) version of 2012. The results show that: (a) MUF from the IRI model is higher Keywords: than the MUF Test but the magnitude for the -
SDSU Template, Version 11.1
AN HF MULTITONE MODEM _______________ A Thesis Presented to the Faculty of San Diego State University _______________ In Partial Fulfillment of the Requirements for the Degree Master of Science in Electrical Engineering _______________ by Louis A. Rey Summer 2017 iii Copyright © 2017 by Louis A. Rey All Rights Reserved iv DEDICATION This thesis is dedicated to my wife, two daughters and all who have loved and supported me throughout this journey. v ABSTRACT OF THE THESIS An HF Multitone Modem by Louis A. Rey Master of Science in Electrical Engineering San Diego State University, 2017 In today’s world, we can find signals being transmitted on every portion of the frequency spectrum from a few Hertz up to several Giga Hertz. Frequencies of upwards of 60GHz are common today. Although it is now common to operate in ever higher frequencies, High Frequency (HF) frequencies (3 to 30 MHz) enjoyed huge popularity during the advent of early long-range communication work. Before satellites were invented, it was the only means of transmitting information at long distances wirelessly. Initial work in the defense industry gave fruit to Multitone modems which were then superseded by single tone modems for both data and voice communications at 2400bps, 9600bps and 19400bps. With the growing popularity of digital signal processing and software radio, these modems are now easily implemented. This thesis revisits Multitone modems, also known as parallel tone modems, which use 16 and 39 tones for data and voice respectively. A comparison with modern communication systems will be explored. A description of the Modem sections will be created using MATLAB.