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    <title>NISCAIR Online Periodicals Repository Collection: IJRSP Vol.41(1) [February 2012]</title>
    <link>http://nopr.niscair.res.in/handle/123456789/13615</link>
    <description />
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      <title>Return loss improvement of power splitter on EBG</title>
      <link>http://nopr.niscair.res.in/handle/123456789/13632</link>
      <description>Title: Return loss improvement of power splitter on EBG
&lt;br/&gt;
&lt;br/&gt;Authors: Mukherjee, Biswajeet
&lt;br/&gt;
&lt;br/&gt;Abstract: In the present paper, the improvement of the return loss of a power&#xD;
splitter/ divider, designed by partial removal of electromagnetic band gap (EBG)&#xD;
rods, has been investigated. The EBG used is a rod structure and shows a band&#xD;
gap in &#xD;
the range 2.2395 - 2.5774 GHz. The power splitter has a return loss of 2.45 GHz&#xD;
which falls in the range of the band gap. &#xD;
It has been found that a larger matrix of the EBG structure is needed in order&#xD;
to improve the return loss significantly. However, the removal of rods, as the&#xD;
matrix size is increased, needs to be done with a fixed ratio of the input feed&#xD;
length to coupling length in order to maintain the same resonant frequency. The&#xD;
improvement in the return loss has been significant from -19.932 dB (for a 5×5&#xD;
matrix) to -37.214 dB (for a 17×17 matrix).
&lt;br/&gt;
&lt;br/&gt;Page(s): 58-61</description>
      <pubDate>Sun, 29 Jan 2012 22:58:59 GMT</pubDate>
    </item>
    <item>
      <title>Prediction of annual and seasonal soil temperature variation using  artificial neural network</title>
      <link>http://nopr.niscair.res.in/handle/123456789/13631</link>
      <description>Title: Prediction of annual and seasonal soil temperature variation using  artificial neural network
&lt;br/&gt;
&lt;br/&gt;Authors: Jebamalar, A S; Raja, S Abraham Thambi; Bai, S Jeslin Sunitha
&lt;br/&gt;
&lt;br/&gt;Abstract: The back propagation algorithm, an artificial neural network (ANN) training algorithm, is a widely applied mathematical implementation&#xD;
for spatial monitoring and is used in the present study for the analysis and prediction&#xD;
of soil temperature. The soil temperature data at 10 and 20 cm soil depths were&#xD;
collected from the Agricultural&#xD;
 College and Research&#xD;
Institute, Killikulam, Tuticorin District of Tamil Nadu. The observed values during&#xD;
the year 2004 at 10 and 20 cm&#xD;
soil depths were plotted to understand the annual and seasonal behaviour of the&#xD;
temperature wave. The wave characteristics such as range of soil temperature&#xD;
and rate of change of temperature/week were estimated and tabulated. Data for 1993 – 1997 (5 years) and 1993 – 2002 (10 years) were separately used as inputs&#xD;
for the prediction of soil temperature in 2004 using ANN. The predicted values&#xD;
were compared with the observed values and statistically validated. The&#xD;
characteristics of predicted annual and seasonal wave were also compared with&#xD;
observed values. It was found that the predicted values of annual wave fitted&#xD;
well with observed ones with little variation for the seasonal waves. The range&#xD;
of soil temperature for predicted values coincided almost with the observed&#xD;
ones with regard to the annual and the seasonal waves for both 10 and 20 cm soil depths. The rate&#xD;
of change of temperature/week of the predicted values coincided well with the observed ones for 10 cm soil depth. For 20 cm soil depth, the&#xD;
predicted values deviated from the observed ones for the winter season while&#xD;
the annual and pre-monsoon seasonal waves coincided well with the observed&#xD;
values. The surface temperature was also predicted independently from 10 and 20 cm soil temperature and&#xD;
error validation was done. From these, it may be convincingly stated that the&#xD;
ANN can be used as a good mathematical model for the prediction of soil&#xD;
temperature.
&lt;br/&gt;
&lt;br/&gt;Page(s): 48-57</description>
      <pubDate>Sun, 29 Jan 2012 22:58:59 GMT</pubDate>
    </item>
    <item>
      <title>Pc4 Occurrence and its dependence on Kp values at low latitudes in India</title>
      <link>http://nopr.niscair.res.in/handle/123456789/13630</link>
      <description>Title: Pc4 Occurrence and its dependence on Kp values at low latitudes in India
&lt;br/&gt;
&lt;br/&gt;Authors: Ansari, I A; Khan, M T
&lt;br/&gt;
&lt;br/&gt;Abstract: A study has been&#xD;
undertaken for Pc4 geomagnetic pulsations ( in 6.7 – 22.2 mHz frequency range)&#xD;
at three very low latitude stations, viz. Pondicherry (PON) (geomagnetic&#xD;
latitude 2.5ºN, geomagnetic longitude 151.97ºE), Nagpur (NAG) (geomagnetic&#xD;
latitude 11.72ºN, geomagnetic longitude 151.93ºE), Hanle (HAN) (geomagnetic&#xD;
latitude 23.38ºN, geomagnetic longitude 151.89ºE) in India employing three axis&#xD;
fluxgate magnetometers, established and operated by the Indian Institute of Geomagnetism&#xD;
(IIG), Navi Mumbai. Digital dynamic spectra (DDS) for the north-south (X),&#xD;
east-west (Y) and vertical (Z) components of the recorded data were constructed&#xD;
for each day for one year (1 January to 31 December 2005). The X and Y&#xD;
components of these DDS were investigated for carrying out statistical study of&#xD;
the dependence of diurnal and seasonal variations of occurrence of Pc4 events&#xD;
on Kp.&#xD;
&lt;br&gt;&lt;br&gt;&#xD;
The monthly variation of Pc4 occurrence has&#xD;
a Kp dependence range from 0 to 9-. However, the yearly Pc4 occurrence was&#xD;
found to be evenly distributed with magnetic activity over Kp range from 2- to&#xD;
4 at all the three stations with the peak occurrence recorded at Kp = 3-. The&#xD;
magnitudes of durations of Pc4 occurrence decreased in the station order PON,&#xD;
HAN and NAG, respectively. The prominent peaks in the seasonal Pc4 occurrence&#xD;
were observed at Kp = 3-, 3 for all the seasons. However, additional peaks were&#xD;
observed at Kp = 1-, 1 and 1+ for the autumn season. It is also worth noting&#xD;
that Pc4 in winter was observed during intense magnetic activity when 5+ &lt;&#xD;
Kp &lt; 8+.
&lt;br/&gt;
&lt;br/&gt;Page(s): 39-47</description>
      <pubDate>Sun, 29 Jan 2012 22:58:59 GMT</pubDate>
    </item>
    <item>
      <title>Diurnal and seasonal variations in sporadic E-layer (Es layer) occurrences over equatorial, low and mid latitude stations - A comparative study</title>
      <link>http://nopr.niscair.res.in/handle/123456789/13629</link>
      <description>Title: Diurnal and seasonal variations in sporadic E-layer (Es layer) occurrences over equatorial, low and mid latitude stations - A comparative study
&lt;br/&gt;
&lt;br/&gt;Authors: Prasad, S N V S; Prasad, D S V V D; Venkatesh, K; Niranjan, K; Rao, P V S Rama
&lt;br/&gt;
&lt;br/&gt;Abstract: The simultaneous hourly ionograms, from an equatorial station Trivandrum&#xD;
(8.47°N, 76.91°E), a low latitude station&#xD;
Waltair (17.70N, 83.3°E) in the Indian sector and a&#xD;
mid latitude station Kokubunji (35.7°N, 139.5°E) in the Japanese sector during the high sunspot year&#xD;
2001, are scaled for the study of E-region parameters, namely the virtual&#xD;
height of sporadic E-layer (h’Es) and the critical frequency of sporadic&#xD;
E-layer (foEs). The diurnal, seasonal and day-to-day variations in h’Es and&#xD;
foEs are studied for all the three stations. It is observed that the sporadic&#xD;
E-layer is absent in the early morning and post sunset hours over Trivandrum during three&#xD;
different seasons. The values of h’Es are more at Kokubunji as compared to&#xD;
those at equatorial (Trivandrum)&#xD;
and low latitude (Waltair) stations during the three different seasons. The&#xD;
critical frequency of sporadic E-layer (foEs) over Trivandrum shows higher values, compared to&#xD;
those over Waltair and Kokubunji during daytime hours, in three different&#xD;
seasons indicating that foEs decrease as the latitude increases. The seasonal&#xD;
variation in foEs shows higher values during daytime hours of equinox and&#xD;
winter months over equator (Trivandrum) compared to those over low (Waltair)&#xD;
and mid (Kokubunji) latitude stations. The variations in h’Es and foEs for&#xD;
quiet and disturbed conditions indicate that the h’Es variation during quiet&#xD;
days of equinoctial months at Kokubunji shows a primary peak around morning&#xD;
hours while it is absent at Waltair and Trivandrum. Further, the behaviour of&#xD;
blanketing frequency of Es layer fbEs, and foEs-fbEs are also studied.
&lt;br/&gt;
&lt;br/&gt;Page(s): 26-38</description>
      <pubDate>Sun, 29 Jan 2012 22:58:59 GMT</pubDate>
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