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  <title>NOPR Collection:</title>
  <link rel="alternate" href="http://nopr.niscpr.res.in/handle/123456789/33395" />
  <subtitle />
  <id>http://nopr.niscpr.res.in/handle/123456789/33395</id>
  <updated>2026-10-09T19:51:59Z</updated>
  <dc:date>2026-10-09T19:51:59Z</dc:date>
  <entry>
    <title>GNSS positioning accuracy over Nigeria during geomagnetic storm of 24-27 October 2011 and 7-10 October 2012</title>
    <link rel="alternate" href="http://nopr.niscpr.res.in/handle/123456789/33400" />
    <author>
      <name>Joseph, Omojola</name>
    </author>
    <author>
      <name>Johnson, Abimbola Oladiran</name>
    </author>
    <id>http://nopr.niscpr.res.in/handle/123456789/33400</id>
    <updated>2016-07-20T06:07:12Z</updated>
    <published>2015-09-01T00:00:00Z</published>
    <summary type="text">Title: GNSS positioning accuracy over Nigeria during geomagnetic storm of 24-27 October 2011 and 7-10 October 2012
Authors: Joseph, Omojola; Johnson, Abimbola Oladiran
Abstract: &lt;span style="font-size:11.0pt;mso-bidi-font-size:&#xD;
10.0pt;font-family:" times="" new="" roman","serif";mso-fareast-font-family:"times="" roman";="" letter-spacing:-.1pt;mso-ansi-language:en-gb;mso-fareast-language:en-us;="" mso-bidi-language:ar-sa"="" lang="EN-GB"&gt;The present work investigates the positioning error of&#xD;
five Nigeria GNSS network stations during the geomagnetic storm of 24-27&#xD;
October 2011, a sudden storm commencement (SSC) with disturbance storm time&#xD;
(Dst) minimum of -134 nT; and &#xD;
7-10 October 2012, a gradual storm commencement (GSC) with Dst minimum -105 nT.&#xD;
Satellite data were obtained from Nigeria GNSS network stations and Dst values&#xD;
were obtained from World Data Center (WDC) for Geomagnetism Kyoto, Japan while&#xD;
the quiet period was selected with Ap index of zero (0) and one (1) for the two&#xD;
storms, respectively from the same World Data Center. RTKLIB (version 2.4.2), a&#xD;
GNSS analysis software, was used to determine the positioning of the stations&#xD;
during the selected storm period and quiet period and the results were analyzed&#xD;
using MATLAB. This investigation revealed that during the selected storm&#xD;
period, the positioning error of the stations increase; though the two storms&#xD;
do not show the same characteristics on GNSS positioning. The GSC of 7-10&#xD;
October 2012 showed a latitudinal effect, which may be as a result of local&#xD;
variation in the electron density and enhancement of ionospheric irregularity&#xD;
during the storm. This was not clearly depicted in the SSC of 24–27 October&#xD;
2011.&lt;/span&gt;
Page(s): 138-146</summary>
    <dc:date>2015-09-01T00:00:00Z</dc:date>
  </entry>
  <entry>
    <title>Electrical conductivity of the stratosphere over Hyderabad,  India: Results from Balloon borne measurements</title>
    <link rel="alternate" href="http://nopr.niscpr.res.in/handle/123456789/33399" />
    <author>
      <name>Gupta, S P</name>
    </author>
    <author>
      <name>Thampi, Smitha V</name>
    </author>
    <id>http://nopr.niscpr.res.in/handle/123456789/33399</id>
    <updated>2016-07-20T06:06:21Z</updated>
    <published>2015-09-01T00:00:00Z</published>
    <summary type="text">Title: Electrical conductivity of the stratosphere over Hyderabad,  India: Results from Balloon borne measurements
Authors: Gupta, S P; Thampi, Smitha V
Abstract: &lt;span style="font-size:11.0pt;mso-bidi-font-size:&#xD;
10.0pt;font-family:" times="" new="" roman","serif";mso-fareast-font-family:"times="" roman";="" mso-ansi-language:en-us;mso-fareast-language:en-us;mso-bidi-language:ar-sa"="" lang="EN-US"&gt;The&#xD;
stratospheric conductivity is an important parameter of the global electric&#xD;
circuit. In this paper, the stratospheric conductivity measurements are&#xD;
presented, which were made using high altitude balloon flights from Hyderabad&#xD;
(geographic 17.5°N, 78.5°E; magnetic lat 8.5°N), India as a part of the IMAP (1982-1994)&#xD;
program of India. The vertical profiles of ion conductivity were measured from&#xD;
Hyderabad during periods with different solar activity levels and during&#xD;
different seasons using different techniques. It was observed that conductivity&#xD;
values in stratosphere are larger in high solar activity period as compared to&#xD;
low solar activity period. This is similar in nature to the observations from&#xD;
mid-latitudes. The observed positive correlation with solar activity is&#xD;
discussed in terms of composition changes due to the change in intensity of the&#xD;
UV &#xD;
(200-300 nm) radiation with solar activity. It was found that the dissociation&#xD;
of heavy cluster ions to lighter ions, as conjectured by Gupta [Solar cycle&#xD;
variation of stratospheric conductivity over low latitude, &lt;i&gt;Adv Space Res&lt;/i&gt;&#xD;
(&lt;i&gt;UK&lt;/i&gt;), 26 (2000.) pp 1225–1229] is the main reason for the observed&#xD;
positive correlation of stratospheric conductivity with solar activity. No&#xD;
significant seasonal effect was noticed. In addition, conductivity profile&#xD;
obtained from Hyderabad is compared to that obtained from Cachoeira Paulista,&#xD;
Brazil.&lt;/span&gt;
Page(s): 132-137</summary>
    <dc:date>2015-09-01T00:00:00Z</dc:date>
  </entry>
  <entry>
    <title>Climatic variance and its effects on decametric Jovian signal reception at a high altitude station Darjeeling</title>
    <link rel="alternate" href="http://nopr.niscpr.res.in/handle/123456789/33398" />
    <author>
      <name>Mondal, S</name>
    </author>
    <author>
      <name>Bhattacharya, A B</name>
    </author>
    <id>http://nopr.niscpr.res.in/handle/123456789/33398</id>
    <updated>2016-07-20T06:05:20Z</updated>
    <published>2015-09-01T00:00:00Z</published>
    <summary type="text">Title: Climatic variance and its effects on decametric Jovian signal reception at a high altitude station Darjeeling
Authors: Mondal, S; Bhattacharya, A B
Abstract: &lt;span style="font-size:11.0pt;font-family:&#xD;
" times="" new="" roman","serif";mso-fareast-font-family:"times="" roman";mso-bidi-font-family:="" mangal;mso-ansi-language:en-gb;mso-fareast-language:en-us;mso-bidi-language:="" hi"="" lang="EN-GB"&gt;In this paper precipitation, firing related to extraterrestrial bodies and&#xD;
other ionospheric effects on decametric Jovian radio signal reception at high&#xD;
altitude has been discussed. Jovian signal is observed at 20.1 MHz in the&#xD;
observatory installed at Darjeeling. As Jovian signal is studied under light of&#xD;
Jupiter-Io coupling, it is found that rainfall, out of different atmospheric&#xD;
components, has highest potential to influence reception of Jovian non-Io&#xD;
emission. The observations show that rainfall density plays crucial role in&#xD;
screening extra-terrestrial signal reception from Earth based observatories.&#xD;
The primitive study also suggests that cumulonimbus cloud may have effect on&#xD;
radio signal reception at high altitude. Some interesting findings regarding&#xD;
climatic influence on Jovian signal reception are reported in this paper.&lt;/span&gt;
Page(s): 126-131</summary>
    <dc:date>2015-09-01T00:00:00Z</dc:date>
  </entry>
  <entry>
    <title>Solar cycle variation of coronal green line index</title>
    <link rel="alternate" href="http://nopr.niscpr.res.in/handle/123456789/33397" />
    <author>
      <name>Kane, R P</name>
    </author>
    <id>http://nopr.niscpr.res.in/handle/123456789/33397</id>
    <updated>2016-07-20T06:04:09Z</updated>
    <published>2015-09-01T00:00:00Z</published>
    <summary type="text">Title: Solar cycle variation of coronal green line index
Authors: Kane, R P
Abstract: &lt;span style="font-size:11.0pt;mso-bidi-font-size:&#xD;
10.0pt;font-family:" times="" new="" roman","serif";mso-fareast-font-family:"times="" roman";="" mso-ansi-language:en-gb;mso-fareast-language:en-us;mso-bidi-language:ar-sa"="" lang="EN-GB"&gt;During&#xD;
1966-2008 (solar cycles 20-23), the evolutions of sunspots (Rz) and solar flare&#xD;
index (SF) show similar evolution, i.e. a rising phase, a broad maximum and a&#xD;
declining phase in each cycle. On the other hand, coronal holes are more&#xD;
frequent in the declining phase of each cycle. Hence, the coronal green line&#xD;
index (CG), which represents coronal heating, is expected to be similar to&#xD;
sunspots and solar flare index during the rising and maximum phases of solar&#xD;
cycle but dissimilar in the declining phase. Observations show that this was&#xD;
true, but the excess of CG in the declining phase is small compared to the CG&#xD;
intensities at solar maximum. Thus, the contribution of coronal hole could not&#xD;
be unique or even major one for the large coronal heating. There are many solar&#xD;
parameters which evolve differently from the sunspot numbers. But in the&#xD;
present paper, it is assumed that comparison with sunspot numbers may be a&#xD;
reasonable one.&lt;/span&gt;
Page(s): 122-125</summary>
    <dc:date>2015-09-01T00:00:00Z</dc:date>
  </entry>
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