<?xml version="1.0" encoding="UTF-8"?>
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  <title>NOPR Collection:</title>
  <link rel="alternate" href="http://nopr.niscpr.res.in/handle/123456789/36919" />
  <subtitle />
  <id>http://nopr.niscpr.res.in/handle/123456789/36919</id>
  <updated>2026-10-12T15:24:39Z</updated>
  <dc:date>2026-10-12T15:24:39Z</dc:date>
  <entry>
    <title>Study of VLP Attenuation as a Function of Azimuth Using Atmospherics</title>
    <link rel="alternate" href="http://nopr.niscpr.res.in/handle/123456789/36966" />
    <author>
      <name>Gopalakrishna, S</name>
    </author>
    <author>
      <name>Sitaramaswamy, P</name>
    </author>
    <id>http://nopr.niscpr.res.in/handle/123456789/36966</id>
    <updated>2016-11-09T06:18:39Z</updated>
    <published>1980-06-01T00:00:00Z</published>
    <summary type="text">Title: Study of VLP Attenuation as a Function of Azimuth Using Atmospherics
Authors: Gopalakrishna, S; Sitaramaswamy, P
Abstract: From a spectral study of atmospherics received from different azimuth angles, attenuation rates between 5 and 11 kHz have been determined by trial and error method using Wait's equation [&lt;i&gt;Proc. IRE,&lt;/i&gt; 4S (1957), 760; 768]. These values are compared with the values obtained by spectral amplitude ratio (SAR) graphs. The values of Ώ at various angles of azimuth for Waltair have been calculated. Using these values of Ώ the attenuation rates from 5 to 11 kHz have been obtained from the theoretical values of Harth [&lt;i&gt;NRL Rep. No.&lt;/i&gt; 7763 1974, 147]. The results are found to be in agreement with the available data. Further, the non-reciprocity of VLF waves travelling along east-west and west-east has been proved.
Page(s): 112-116</summary>
    <dc:date>1980-06-01T00:00:00Z</dc:date>
  </entry>
  <entry>
    <title>Collisions &amp; Transport of Electrons in the Ionosphere</title>
    <link rel="alternate" href="http://nopr.niscpr.res.in/handle/123456789/36965" />
    <author>
      <name>Aggarwal, K M</name>
    </author>
    <author>
      <name>Setty, C S G K</name>
    </author>
    <id>http://nopr.niscpr.res.in/handle/123456789/36965</id>
    <updated>2016-11-09T06:16:11Z</updated>
    <published>1980-06-01T00:00:00Z</published>
    <summary type="text">Title: Collisions &amp; Transport of Electrons in the Ionosphere
Authors: Aggarwal, K M; Setty, C S G K
Abstract: Analytic expressions are given for the temperature dependent monoenergetic &lt;i&gt;(v&lt;sub&gt;m&lt;/sub&gt;ln) &lt;/i&gt;and the two averaged (&lt;v&gt;/&lt;i&gt;n&lt;/i&gt; and v/n) collision frequencies for the electron impact with N&lt;sub&gt;2&lt;/sub&gt;, O&lt;sub&gt;2&lt;/sub&gt;, N, O, He, Ne, Ar and H in the electron temperature range 100-5000K. These expressions are based on recent experimental and reliable theoretical models of momentum transfer cross-sections for the target gases. Using the latest and reliable atmospheric and ionospheric models for the densities and temperatures of neutral and ionic gas targets, the electron collision frequency &lt;&lt;i&gt;v&lt;sub&gt;g&lt;/sub&gt;&lt;/i&gt;&gt; has been estimated in the upper region of the ionosphere (100-500km). It is observed that at altitudes above 140km, &lt;&lt;i&gt;v&lt;sub&gt;g&lt;/sub&gt;&lt;/i&gt;&gt; values are highest in the winter and lowest in the summer for high solar activity. However, for low solar activity, there is no such change in &lt;&lt;i&gt;v&lt;sub&gt;g&lt;/sub&gt;&lt;/i&gt;&gt;. A study of various electron transport properties shows that their behaviour is opposite to that of &lt;&lt;i&gt;v&lt;sub&gt;g&lt;/sub&gt;&lt;/i&gt;&gt; as expected.
Page(s): 105-111</summary>
    <dc:date>1980-06-01T00:00:00Z</dc:date>
  </entry>
  <entry>
    <title>Effect of Lower Ionosphere on the Propagation of VLP Waves at Low Latitudes</title>
    <link rel="alternate" href="http://nopr.niscpr.res.in/handle/123456789/36964" />
    <author>
      <name>Singh, D P</name>
    </author>
    <author>
      <name>Singh, Birbal</name>
    </author>
    <id>http://nopr.niscpr.res.in/handle/123456789/36964</id>
    <updated>2016-11-09T06:13:52Z</updated>
    <published>1980-06-01T00:00:00Z</published>
    <summary type="text">Title: Effect of Lower Ionosphere on the Propagation of VLP Waves at Low Latitudes
Authors: Singh, D P; Singh, Birbal
Abstract: Full wave technique is employed to determine the Budden's reflection coefficients and polarization for VLF  waves of frequency 5 kHz propagating in the lower region of the ionosphere at low latitudes. The results are  then utilized to determine the propagation losses suffered by the waves in the ionosphere and at different hops  of propagation in the earth-ionosphere waveguide. The daytime losses are found to be much higher than nighttime losses. By utilizing the nighttime losses, the possibility of earth-ionosphere waveguide mode propagation for VLF emissions observed at two low latitude ground stations of Moshiri and Hiraiso is examined.
Page(s): 101-104</summary>
    <dc:date>1980-06-01T00:00:00Z</dc:date>
  </entry>
  <entry>
    <title>Microwave Line-of-sight Link-Tornado Effect</title>
    <link rel="alternate" href="http://nopr.niscpr.res.in/handle/123456789/36963" />
    <author>
      <name>Ramakrishna, M</name>
    </author>
    <author>
      <name>Banerjee, P K</name>
    </author>
    <author>
      <name>Sarkar, S K</name>
    </author>
    <author>
      <name>Dutta, H N</name>
    </author>
    <id>http://nopr.niscpr.res.in/handle/123456789/36963</id>
    <updated>2016-11-09T06:12:50Z</updated>
    <published>1980-06-01T00:00:00Z</published>
    <summary type="text">Title: Microwave Line-of-sight Link-Tornado Effect
Authors: Ramakrishna, M; Banerjee, P K; Sarkar, S K; Dutta, H N
Abstract: The general signal strength prediction methods in tropospheric propagation mode with the statistical knowledge of conventional radiosonde data are inadequate to explain the microwave signal behavior during a  localized phenomenon like tornado. The tornado that struck North Delhi on 17 Mar. 1978, severely affected the  microwave line-of-sight link. A study of the signal behaviour during and after the event is reported.
Page(s): 97-100</summary>
    <dc:date>1980-06-01T00:00:00Z</dc:date>
  </entry>
</feed>

