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Journal ArticleDOI

Obstacle gain in radio-wave propagation over inhomogeneous earth

K. Furutsu, +1 more
- Vol. 117, Iss: 5, pp 887-893
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TLDR
In this paper, the authors defined the obstacle gain as the gain caused by the earth's inhomogeneity and also the antenna height, or it can be the "terminal gain" in the sense that the inhomogeneous in the vicinity of the path terminal is particularly emphasised by the effect of the antenna length.
Abstract
The obstacle gains are numerically illustrated as functions of the distance between the obstacle and the path terminal for the typical examples of a ridge, a bluff on a homogeneous earth and a cliff at a coastline As the distance increases, these obstacle gains tend to become constants (ie the ridge gain, the bluff gain and the cliff gain that have been previously obtained), while, at short distances, they are directly affected by a diffraction loss, interference between the direct and reflected waves and other effects which are not optical in character A convenient formula for the obstacle gain is introduced for the poor convergence of the relevant residue series The obstacle gain defined here can be understood to be the gain caused by the earth's inhomogeneity and also the gain caused by the antenna height, or it can be the ‘terminal gain’, in the sense that the inhomogeneity in the vicinity of the path terminal is particularly emphasised by the effect of the antenna height It can be used in the same way as the ordinary antenna-height gain over a homogeneous earth

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Citations
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Journal ArticleDOI

Recent analytical investigations of electromagnetic ground wave propagation over inhomogeneous earth models

TL;DR: In this article, a consolidated review of recent analytical studies of electromagnetic waves propagating over inhomogeneous surfaces is presented, focusing on smooth boundaries that can be characterized by a local surface impedance.
Journal ArticleDOI

A systematic theory of wave propagation over irregular terrain

K. Furutsu
- 01 Sep 1982 - 
TL;DR: In this article, an explicit expression of the attenuation for a radio wave is obtained for a class of terrains consisting, along the wave path, of several sections of different heights and different electrical properties, taking into account the earth's curvature for every section.

Propagação de onda terrestre na faixa de frequências médias – aplicação ao planejamento da radiodifusão sonora digital

TL;DR: In this article, a trabalho discute o problema da propagacao da onda terrestre na faixa de ondasmedias visando aplicacao no planejamento da radiodifusao sonora digital.
References
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Journal ArticleDOI

The Calculation of Ground-Wave Field Intensity over a Finitely Conducting Spherical Earth

TL;DR: In this article, the authors simplify the calculation of ground-wave field intensity over a finitely conducting spherical earth for transmitting and receiving antennas of arbitrary heights and polarization for a single antenna.
Journal ArticleDOI

Diffraction and Scattering of the Electromagnetic Groundwave by Terrain Features

James R. Wait
- 01 Oct 1968 - 
TL;DR: In this paper, a class of two-dimensional diffraction and scattering problems is considered for evaluating the influence of idealized terrain features in groundwave propagation, making extensive use of the orthogonality properties of the Airy type wave functions which characterize the height dependence of the modes.
Journal ArticleDOI

Some numerical results based on the theory of radio wave propagation over inhomogeneous earth

TL;DR: In this paper, numerical examples are presented to show the dominant features of radio wave propagation over an inhomogeneous earth, based on the tllCories derived previously [Furutsu, 1957a, 1957b, 1959, 1963] in which the h eight and also the electrical properties of the earth's surface were assumed to change disco ntinuously several times along the wave path.
Journal ArticleDOI

Calculated curves for groundwave propagation over inhomogeneous earth with pronounced topographical features

TL;DR: In this article, numerical examples for radio propagation over a three-dimensional pa th are presented, where the path is assumed to be a land-sea-Iand path and a sea-land-sea path, and the attenuation is obtained both for the fl a t earth a nd the sp he rical earth and the val ues are compared to show th e asy mptoti c approach of these two value s at short distances.
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