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    <title>NISCAIR Online Periodicals Repository Collection: IJRSP Vol.39(3) [June 2010]</title>
    <link>http://nopr.niscair.res.in/handle/123456789/9730</link>
    <description />
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      <title>A dual-band stacked rectangular microstrip antenna</title>
      <link>http://nopr.niscair.res.in/handle/123456789/9808</link>
      <description>Title: A dual-band stacked rectangular microstrip antenna
&lt;br/&gt;
&lt;br/&gt;Authors: Vishwakarma, Rajesh Kumar; Tiwari, Sanjay
&lt;br/&gt;
&lt;br/&gt;Abstract: A dual-band characteristic of stacked&#xD;
rectangular microstrip antenna is experimentally studied. It is a probe fed&#xD;
antenna for impedance matching with 50Ω coaxial cable. This antenna works well&#xD;
in the frequency range 2.86-4.63 GHz. It is basically a low cost, light weight&#xD;
medium gain antenna which is used for mobile communication. The variations of&#xD;
the length and width (1 mm) of the stacked rectangular patch antenna have been&#xD;
done. It is found to have dual resonance with increasing lower resonance&#xD;
frequency and almost constant upper resonance frequency with increases of the&#xD;
length and width of rectangular microstrip antenna. The input impedance and&#xD;
voltage standing wave ratio (VSWR) return loss have been measured with the help&#xD;
of network analyzer.
&lt;br/&gt;
&lt;br/&gt;Page(s): 163-169</description>
      <pubDate>Sat, 29 May 2010 22:58:59 GMT</pubDate>
    </item>
    <item>
      <title>Single layer modified rectangular microstrip array antenna for multi band and wide band applications</title>
      <link>http://nopr.niscair.res.in/handle/123456789/9807</link>
      <description>Title: Single layer modified rectangular microstrip array antenna for multi band and wide band applications
&lt;br/&gt;
&lt;br/&gt;Authors: Mallikarjun, S L; Hadalgi, P M
&lt;br/&gt;
&lt;br/&gt;Abstract: A four-element modified rectangular&#xD;
microstrip array antenna (4MRMSAA) is designed and further extended to eight&#xD;
element modified rectangular microstrip array antenna (8MRMSAA). A comparative&#xD;
study is made between the proposed antennas. The experimental results show that&#xD;
4MRMSAA operates for multi band and 8MRMSAA operates for wide band with an&#xD;
improvement (39.34%) in impedance bandwidth. This improvement in the impedance&#xD;
bandwidth of 8MRMSAA is 13.80 times more as compared to single rectangular&#xD;
radiating element (RMSA). The experimental results of the proposed antennas have&#xD;
been presented in terms of impedance bandwidth, return loss, gain, half power&#xD;
beam width (HPBW) and cross polarization levels. These multi band and wide band&#xD;
antennas have applications in modern communications and radar communication&#xD;
systems.
&lt;br/&gt;
&lt;br/&gt;Page(s): 156-162</description>
      <pubDate>Sat, 29 May 2010 22:58:59 GMT</pubDate>
    </item>
    <item>
      <title>Relationship between Dst and solar wind conditions during intense geomagnetic storms</title>
      <link>http://nopr.niscair.res.in/handle/123456789/9806</link>
      <description>Title: Relationship between Dst and solar wind conditions during intense geomagnetic storms
&lt;br/&gt;
&lt;br/&gt;Authors: Bakare, N O; Chukwuma, V U
&lt;br/&gt;
&lt;br/&gt;Abstract: A&#xD;
study of 83 geomagnetic storms during 1996-2006 has been carried out to&#xD;
investigate the relationship between Dst and solar wind plasma parameters&#xD;
during intense geomagnetic storms. The geomagnetic storms are primarily&#xD;
associated with two classes of drivers: the magnetic cloud and complex ejecta.&#xD;
It was found that magnetic cloud were drivers in 43 geomagnetic storm (~ 51.8%)&#xD;
while complex ejecta were responsible for 40 geomagnetic storms (~ 48.2%). The&#xD;
correlation between Dst and magnetic field B; and between Dst and Bs was 0.76&#xD;
and 0.90, respectively for geomagnetic storms resulting from magnetic clouds.&#xD;
The correlation between Dst and B; and between Dst and Bs was 0.71 and 0.64,&#xD;
respectively for geomagnetic storms resulting from complex ejecta. Furthermore,&#xD;
it was shown that the correlation between the Dst and solar wind speed V for&#xD;
magnetic cloud and complex ejecta was 0.58 and 0.57, respectively. It was&#xD;
observed that the correlation between Dst and VBs for magnetic cloud and&#xD;
complex ejecta were 0.77 and 0.71, respectively. The present results suggest&#xD;
that though both classes of drivers can cause intense geomagnetic storm but&#xD;
magnetic cloud is more geo-effective than complex ejecta.
&lt;br/&gt;
&lt;br/&gt;Page(s): 150-155</description>
      <pubDate>Sat, 29 May 2010 22:58:59 GMT</pubDate>
    </item>
    <item>
      <title>Scattering of VLF signals from localized perturbations in the lower ionosphere</title>
      <link>http://nopr.niscair.res.in/handle/123456789/9805</link>
      <description>Title: Scattering of VLF signals from localized perturbations in the lower ionosphere
&lt;br/&gt;
&lt;br/&gt;Authors: Singh, Vikram; Singh, Birbal
&lt;br/&gt;
&lt;br/&gt;Abstract: A wave-slab interaction model has been used to study the scattering of very&#xD;
low frequency (VLF) ground transmitter signals from localized enhancements of ionization&#xD;
in the lower ionosphere caused by transient luminous events (TLEs) such as sprites.&#xD;
The variation of reflection coefficients has been studied for a fixed frequency&#xD;
VLF transmitter signal of frequency 19.8 kHz (NWC, Australia) monitored at Agra&#xD;
for different slab thicknesses, incident angles, and enhancement factors. The results&#xD;
show that sufficient strength of the reflected signals is obtained for a slab thickness&#xD;
of 3 km, enhancement factor between 2.5 and 3, and incident angle around 75&lt;sup&gt;0&lt;/sup&gt;.&#xD;
These results explain satisfactorily the VLF amplitude and phase anomalies in sub-ionospheric&#xD;
VLF transmitter signals recorded at Agra station which are interpreted as caused&#xD;
by transient luminous events.
&lt;br/&gt;
&lt;br/&gt;Page(s): 144-149</description>
      <pubDate>Sat, 29 May 2010 22:58:59 GMT</pubDate>
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