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  <channel rdf:about="http://nopr.niscpr.res.in/handle/123456789/25573">
    <title>NOPR Collection:</title>
    <link>http://nopr.niscpr.res.in/handle/123456789/25573</link>
    <description />
    <items>
      <rdf:Seq>
        <rdf:li rdf:resource="http://nopr.niscpr.res.in/handle/123456789/25888" />
        <rdf:li rdf:resource="http://nopr.niscpr.res.in/handle/123456789/25887" />
        <rdf:li rdf:resource="http://nopr.niscpr.res.in/handle/123456789/25886" />
        <rdf:li rdf:resource="http://nopr.niscpr.res.in/handle/123456789/25885" />
      </rdf:Seq>
    </items>
    <dc:date>2026-10-10T12:25:35Z</dc:date>
  </channel>
  <item rdf:about="http://nopr.niscpr.res.in/handle/123456789/25888">
    <title>Characteristics of the observed low latitude very low frequency emission periods and whistler-mode group delays at Jammu</title>
    <link>http://nopr.niscpr.res.in/handle/123456789/25888</link>
    <description>Title: Characteristics of the observed low latitude very low frequency emission periods and whistler-mode group delays at Jammu
Authors: Lalmani; Kumar, Rajou; Singh, Rajesh; Singh, Birbal
Abstract: First observations&#xD;
on the relationship between whistlers and periodic very low frequency (VLF) emissions&#xD;
observed at low latitude ground station Jammu (geomagn. lat., 22° 26&lt;i&gt;'&lt;/i&gt; N;&#xD;
&lt;i&gt;L &lt;/i&gt;= 1.17) are presented. The results have been discussed in the present paper.&#xD;
To explain the results it is proposed that the periodic VLF emissions are generated&#xD;
near the equatorial region at &lt;i&gt;L ~ &lt;/i&gt;1.2 as a result of interaction between&#xD;
trapped energetic particles and one-hop whistlers under cyclotron resonance mechanism&#xD;
and propagated to the ground station Jammu in nonducted mode of whistler propagation.
Page(s): 214-216</description>
    <dc:date>2001-08-01T00:00:00Z</dc:date>
  </item>
  <item rdf:about="http://nopr.niscpr.res.in/handle/123456789/25887">
    <title>Ionospheric electron content near anomaly crest as precursor of earthquake</title>
    <link>http://nopr.niscpr.res.in/handle/123456789/25887</link>
    <description>Title: Ionospheric electron content near anomaly crest as precursor of earthquake
Authors: Devi, M; Barman, M K; Barbara, A K; Depueva, A
Abstract: Ionospheric electron&#xD;
content (IEC) values, derived from Faraday rotations of VHF radio beacons from satellites&#xD;
and recorded at an equatorial anomaly crest station, Guwahati&#xD;
&#xD;
(lat.26.2° N, long.91.75°E;&#xD;
and situated at a seismically active zone of east Himalayas), have been examined&#xD;
to see if these data could be used as precursor of earthquake. The earthquake&#xD;
events are so selected that the epicentres lie within 12°-30° N and 81°- 120&lt;sup&gt;o&lt;/sup&gt;E.&#xD;
The paper analyses IEC variations during and prior to an earthquake event, in relation&#xD;
to epicentric position.
Page(s): 209-213</description>
    <dc:date>2001-08-01T00:00:00Z</dc:date>
  </item>
  <item rdf:about="http://nopr.niscpr.res.in/handle/123456789/25886">
    <title>Triangular microstrip stacked antenna for dual band operation</title>
    <link>http://nopr.niscpr.res.in/handle/123456789/25886</link>
    <description>Title: Triangular microstrip stacked antenna for dual band operation
Authors: Vasistha, Prashant; Vishvakarma, Babau R
Abstract: Experimental investigations&#xD;
conducted on triangular microstrip stacked antenna (TMSSA) to achieve dual band&#xD;
operation by optimizing the number of elements reveal that TMSSA attains the&#xD;
maximum -10 dB return-loss band of 688.6 MHz for (1+3) structure for second resonance.&#xD;
The air gap spacing of 2.5 mm in (1+1) structure improved -10 dB return-loss&#xD;
&#xD;
(RL) band by&#xD;
612.14 MHz as compared to 242.3 MHz for zero spacing in first resonance (&lt;i&gt;f&lt;/i&gt;&lt;sub&gt;rl&lt;/sub&gt;)&lt;i&gt;.&#xD;
&lt;/i&gt;It is also observed that -10 dB return-loss band depends heavily on the angular&#xD;
rotation (non-alignment) in the (1+1) structure.
Page(s): 205-208</description>
    <dc:date>2001-08-01T00:00:00Z</dc:date>
  </item>
  <item rdf:about="http://nopr.niscpr.res.in/handle/123456789/25885">
    <title>Response of microwave scattering from crop (wheat) and crop covered soil moisture for remote sensing</title>
    <link>http://nopr.niscpr.res.in/handle/123456789/25885</link>
    <description>Title: Response of microwave scattering from crop (wheat) and crop covered soil moisture for remote sensing
Authors: Singh, D; Sharan, S K; Singh, K P
Abstract: The present study&#xD;
investigates the potential use&#xD;
of active microwave observations at 9.5 GHz frequency of X-band to monitor soil&#xD;
moisture and vegetation leaf area index (LAI) over a wheat cover for remote sensing. Using an X-band (9.5&#xD;
GHz) scatterometer, measurements have&#xD;
been made out for different growth stage of crop (wheat). The leaf area index (LAI)&#xD;
is an important parameter for understanding the crop characteristics. Here an&#xD;
attempt has been made to highlight&#xD;
the effect of crop (wheat) LAI and crop covered soil moisture (&lt;i&gt;m&lt;/i&gt;&lt;sub&gt;g&lt;/sub&gt;)&#xD;
on microwave scattering. Using simple scattering model, an empirical relation has&#xD;
been developed for observing the LAI and &lt;i&gt;m&lt;/i&gt;&lt;sub&gt;g&lt;/sub&gt;&lt;i&gt; &lt;/i&gt;effect on&#xD;
scattering coefficient. The angular and&#xD;
&#xD;
polarization&#xD;
dependence of scattering coefficient on crop LAI and crop covered soil moisture&#xD;
has been investigated, which indicates that, when incidence angle is less than 30°, the crop&#xD;
(wheat) covered soil moisture&#xD;
is&#xD;
well observed, whereas when the incidence angle is greater than 30°, crop effect&#xD;
is more dominant at 9.5 GHz&lt;i&gt;. &lt;/i&gt;The VV-polarization is more sensitive to sense the crop effect than HH-polarization.&#xD;
This type of study is helpful to&#xD;
make the algorithm for air- or space-borne data to access the crop parameters and&#xD;
crop covered soil moisture. All the&#xD;
data can also be used as reference data for space-borne sensors.
Page(s): 198-204</description>
    <dc:date>2001-08-01T00:00:00Z</dc:date>
  </item>
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