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  <channel rdf:about="http://nopr.niscpr.res.in/handle/123456789/17263">
    <title>NOPR Community:</title>
    <link>http://nopr.niscpr.res.in/handle/123456789/17263</link>
    <description />
    <items>
      <rdf:Seq>
        <rdf:li rdf:resource="http://nopr.niscpr.res.in/handle/123456789/29997" />
        <rdf:li rdf:resource="http://nopr.niscpr.res.in/handle/123456789/29996" />
        <rdf:li rdf:resource="http://nopr.niscpr.res.in/handle/123456789/29995" />
        <rdf:li rdf:resource="http://nopr.niscpr.res.in/handle/123456789/29994" />
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    </items>
    <dc:date>2026-04-22T05:40:28Z</dc:date>
  </channel>
  <item rdf:about="http://nopr.niscpr.res.in/handle/123456789/29997">
    <title>On the relationship between the magnetic field variations and meteor showers</title>
    <link>http://nopr.niscpr.res.in/handle/123456789/29997</link>
    <description>Title: On the relationship between the magnetic field variations and meteor showers
Authors: Kulkarni, V H; Kane, R P
Abstract: &lt;span style="mso-bidi-language:HI"&gt;The magnetic Z field variation for the period 9-25&#xD;
Dec. 1996, recorded at the stations Sodankyla (67.37°N, 26.63°E), Tromso (69.67°N,&#xD;
18.95°E), Abisko (68.30°N, 18.82°E), and Hornsund (77.00°N, 26.63°E)&#xD;
(http://swdcwww.kugi.kyoto-u.ac.jp) are compared with the Geminids (12-15 Dec. 1996)&#xD;
and Ursids (20-23 Dec. 1996) showers as reported by Yrjola (http://www.rmob.org).&#xD;
The correlation studies show that it is difficult to prove conclusively that&#xD;
the magnetic field fluctuations observed at&#xD;
&#xD;
&lt;span style="mso-bidi-language:HI"&gt;Sodankyla are due to the dust particles in the&#xD;
meteor showers and the associated changes in the ionospheric currents due to&#xD;
them.&#xD;
&#xD;
&lt;/span&gt;&lt;/span&gt;
Page(s): 385-386</description>
    <dc:date>2003-12-01T00:00:00Z</dc:date>
  </item>
  <item rdf:about="http://nopr.niscpr.res.in/handle/123456789/29996">
    <title>Beam shaping of V-slot waveguide antenna using corner reflector</title>
    <link>http://nopr.niscpr.res.in/handle/123456789/29996</link>
    <description>Title: Beam shaping of V-slot waveguide antenna using corner reflector
Authors: Makal, B S; Vani, RM; Hadalgi, P M; Mulgi, S N; Hunagund, P V
Abstract: &lt;span style="mso-bidi-language:HI"&gt;This paper presents the experimental&#xD;
investigations of the variation of on-axis power, half-power beam width and VSWR&#xD;
of V-slot waveguide antenna (V-SWGA) for different parameters of corner reflector&#xD;
(CR). Experimental study reveals that the CR has very predominant effect in&#xD;
improving the antenna parameters of V-SWGA.&#xD;
&#xD;
&lt;/span&gt;
Page(s): 382-384</description>
    <dc:date>2003-12-01T00:00:00Z</dc:date>
  </item>
  <item rdf:about="http://nopr.niscpr.res.in/handle/123456789/29995">
    <title>Equivalence between external electric field with temperature and supersaturation in nucleation process</title>
    <link>http://nopr.niscpr.res.in/handle/123456789/29995</link>
    <description>Title: Equivalence between external electric field with temperature and supersaturation in nucleation process
Authors: Singh, N; Kumar, Anand
Abstract: &lt;span style="mso-bidi-language:HI"&gt;The equivalence between critical temperature&#xD;
corresponding to unit nucleation rate per unit volume has been studied with external&#xD;
electric field applied to water vapours. It has been found that an external&#xD;
electric field of 1 e.s.u. with different supersaturation ratio is equivalent&#xD;
to several orders of temperature. The high electric field is found to&#xD;
correspond with lower temperatures for critical nucleation. The theory of&#xD;
droplet growth in presence of external electric field has been applied to&#xD;
&#xD;
&lt;span style="mso-bidi-language:HI"&gt;water vapour condensation. The radius of critical&#xD;
nucleus is found to depend on electric field and relaxation time. Further in presence&#xD;
of electric field, Gibb's free energy of formation of water molecule changes&#xD;
for a critical nucleus and is found to be much less than that in absence of the&#xD;
electric field, but equilibrium concentration of nuclei is very much larger. &#xD;
&#xD;
&lt;/span&gt;&lt;/span&gt;
Page(s): 379-381</description>
    <dc:date>2003-12-01T00:00:00Z</dc:date>
  </item>
  <item rdf:about="http://nopr.niscpr.res.in/handle/123456789/29994">
    <title>Mixed layer height over Bay of Bengal during Indian summer monsoon using MONTBLEX observations</title>
    <link>http://nopr.niscpr.res.in/handle/123456789/29994</link>
    <description>Title: Mixed layer height over Bay of Bengal during Indian summer monsoon using MONTBLEX observations
Authors: Patil, M N; Parasnis, S S
Abstract: &lt;span style="mso-bidi-language:HI"&gt;The height of mixed layer and cloud base is&#xD;
studied in relation to surface meteorological parameters, surface fluxes of heat&#xD;
and momentum and synoptic weather disturbances. For this study, surface as well&#xD;
as upper air meteorological observations collected over north&#xD;
 Bay of Bengal (20°N, 89°E) during&#xD;
the summer monsoon of 1990 as a part of Monsoon Trough Boundary Layer&#xD;
Experiment (MONTBLEX), were utilized. Empirical relation between the cloud base&#xD;
height and the surface &lt;i&gt;meteorological observations has &lt;/i&gt;been verified &lt;i&gt;for&#xD;
its validity over Bay of Bengal.&#xD;
This height &lt;/i&gt;is further &lt;i&gt;compared with aerological observations. &lt;/i&gt;A &lt;i&gt;simple&#xD;
relation &lt;/i&gt;based on surface air temperature, pressure and &lt;i&gt;wind &lt;/i&gt;speed &lt;i&gt;has&#xD;
&lt;/i&gt;been &lt;i&gt;suggested to &lt;/i&gt;estimate &lt;i&gt;the &lt;/i&gt;cloud &lt;i&gt;base height. &lt;/i&gt;Influence&#xD;
of &lt;i&gt;the turbulent &lt;/i&gt;surface fluxes of &lt;i&gt;heat and momentum &lt;/i&gt;on &lt;i&gt;evolution&#xD;
&lt;/i&gt;of &lt;i&gt;mixed layer &lt;/i&gt;over Bay of Bengal&#xD;
has been brought out.&#xD;
&#xD;
&lt;/span&gt;
Page(s): 373-378</description>
    <dc:date>2003-12-01T00:00:00Z</dc:date>
  </item>
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