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    <title>NOPR Collection:</title>
    <link>http://nopr.niscpr.res.in/handle/123456789/58949</link>
    <description />
    <pubDate>Sat, 10 Oct 2026 01:09:11 GMT</pubDate>
    <dc:date>2026-10-10T01:09:11Z</dc:date>
    <item>
      <title>Implementation of e-CALLISTO Network for study of solar activities</title>
      <link>http://nopr.niscpr.res.in/handle/123456789/58956</link>
      <description>Title: Implementation of e-CALLISTO Network for study of solar activities
Authors: Patil, Dnyandev Bhausaheb; Kale, Vijay Sadashiv; Shaligram, Arvind Digamber
Abstract: The Earth is influenced by the effects of the continuously varying solar wind, the flow of plasma and the embedded&#xD;
magnetic field from the Sun. Life on the earth is driven by the sunlight incident from the Sun. Therefore, the climate is critically&#xD;
sensitive to solar activities. The variation in the Sun’s atmosphere has an important role in changing life on the earth and&#xD;
therefore it becomes necessary to monitor, observe and study solar activities. Many instruments and observatories have been&#xD;
keeping watch on Sun’s activities. The Compound Astronomical Low-cost Low-frequency Instrument for Spectroscopy and&#xD;
Transportable Observatory (CALLISTO) is one of them. It is popular, portable and low-cost instrument. All CALLISTO station&#xD;
spectrometers together form an e-CALLISTO network. The e-CALLISTO network is spread worldwide and has been providing&#xD;
observations from different countries. This paper reports the antenna and receiver of e-CALLISTO network. It represents the&#xD;
information about antenna especially Log-periodic Dipole Antenna (LPDA) which is low cost and easy to design which can&#xD;
help antenna designer to identify the benefits of LPDA. The e-CALLISTO network is still growing, therefore this may help the&#xD;
people who are going to work on solar activity or working on the e-CALLISTO network.
Page(s): 109-114</description>
      <pubDate>Wed, 01 Sep 2021 00:00:00 GMT</pubDate>
      <guid isPermaLink="false">http://nopr.niscpr.res.in/handle/123456789/58956</guid>
      <dc:date>2021-09-01T00:00:00Z</dc:date>
    </item>
    <item>
      <title>Latitudinal variation in vertical distribution of meteor decay time and its relation with mesospheric Ozone in the altitude range of 80-90 km</title>
      <link>http://nopr.niscpr.res.in/handle/123456789/58955</link>
      <description>Title: Latitudinal variation in vertical distribution of meteor decay time and its relation with mesospheric Ozone in the altitude range of 80-90 km
Authors: Battula, Prem Kumar; D V, Phani Kumar; K, Chenna Reddy; K, Kishore Kumar; G, Yellaiah
Abstract: Investigations on meteor trail decay time and its evolution in the mesosphere and lower thermosphere are very important&#xD;
to estimate the temperature in this region. The present study focuses on the vertical distribution of meteor decay times at&#xD;
three different latitudes to understand the mechanism responsible for the deviation of meteor decay time from the theoretical&#xD;
estimations below 90 km of altitude. The present study is based on measurements from three identical meteor radars located&#xD;
at equatorial (Kototabang: 0.2° S, 100.3° E), low (Thumba: 8.5° N, 76.9° E) and polar latitudes (Eureka: 80.0° N, 85.8° W).&#xD;
The results reveal a pronounced seasonal variation of vertical distribution of meteor decay time turning altitude (inflection&#xD;
point) over polar latitudes as compared to that over equatorial and low latitudes. Apart from direct estimations from meteor&#xD;
radar observations, the meteor decay time is estimated using temperature and pressure measurements from the&#xD;
SABER/TIMED. Above 90 km of altitude, decay times estimated from both methods are in good agreement. However,&#xD;
below 90 km of altitude, these estimations start deviating and it has been noted that the deviation increases with decreasing&#xD;
altitude. Further, observed meteor decay times correlated with ozone concentration at three representative altitude bins. The&#xD;
correlation analysis reveals a significant negative correlation at 80 - 90 km of altitude over the three latitudes indicating that&#xD;
an increase in ozone concentration results in decrease in meteor decay time. The significance of the present results lies in&#xD;
analyzing the vertical distribution of meteor decay time simultaneously from three radar locations representing equatorial,&#xD;
low and polar latitudes and evaluating the relation between ozone concentration and meteor decay time, quantitatively.
Page(s): 115-124</description>
      <pubDate>Wed, 01 Sep 2021 00:00:00 GMT</pubDate>
      <guid isPermaLink="false">http://nopr.niscpr.res.in/handle/123456789/58955</guid>
      <dc:date>2021-09-01T00:00:00Z</dc:date>
    </item>
    <item>
      <title>Equatorial Electrojet and electron density over Southeast Asian Region during moderate solar activity condition</title>
      <link>http://nopr.niscpr.res.in/handle/123456789/58954</link>
      <description>Title: Equatorial Electrojet and electron density over Southeast Asian Region during moderate solar activity condition
Authors: Bello, Saeed Abioye; Hamid, Nurul Shazana Abdul; Abdullah, Mardina; Yoshikawa, Akimasa; Hozumi, Kornyanat; Tsugawa, Takuya
Abstract: The study presents a simultaneous variation of equatorial electrojet (EEJ) current and the ionospheric F2-layer maximum&#xD;
electron density (NmF2) during geomagnetic quiet days and moderate solar conditions (solar radio flux, 𝐹10.7 􀵎 120 sfu).&#xD;
The geomagnetic measurements at Kotatobang (KTB) and Langkawi (LKW) stations have been used to estimate the&#xD;
magnetic daily variation in H-component and in deriving EEJ. The NmF2 data set is from Frequency Modulation&#xD;
Continuous Wave (FM-CW), an analogue ionosonde located at the KTB station. The study examines both the diurnal and&#xD;
seasonal variation in EEJ and the corresponding effect on the measured NmF2. The results obtained show that the derived&#xD;
EEJ at LKW shows a daytime peak which coincides with the period NmF2 measurement at KTB station depleted to a&#xD;
daytime low value. The role of EEJ at the LKW station correlates poorly with the NmF2 at KTB in which their correlation&#xD;
coefficient (r) is in the range of 0.02 to 0.04 for equinox, summer and winter, respectively. However, an r-value of 0.33 was&#xD;
observed when the whole data set for the year 2012 was considered. The poor correlation coefficient between derived EEJ&#xD;
and NmF2 measured at KTB during the moderate solar condition suggest that EEJ has little or no influence on the prevailing&#xD;
ionospheric condition at a low latitude station located outside the EEJ strip.
Page(s): 125-131</description>
      <pubDate>Wed, 01 Sep 2021 00:00:00 GMT</pubDate>
      <guid isPermaLink="false">http://nopr.niscpr.res.in/handle/123456789/58954</guid>
      <dc:date>2021-09-01T00:00:00Z</dc:date>
    </item>
    <item>
      <title>Study of functional Ionospheric Models</title>
      <link>http://nopr.niscpr.res.in/handle/123456789/58953</link>
      <description>Title: Study of functional Ionospheric Models
Authors: Chatterjee, Purbita
Abstract: The ionosphere has played an important role for propagation of electromagnetic waves. They contribute to a major&#xD;
portion of the propagation delay, especially for the low frequency navigation signals, as they pass through earth’s&#xD;
atmosphere. The amount of delay of these signals depends on ionospheric total electron content, which has a spatio-temporal&#xD;
variation. While the dual frequency users can remove the delay errors in signals, these delays pose a major threat mostly for&#xD;
single frequency users, who has to resort to the ionospheric models for the removal these delay errors in the signals, and&#xD;
hence for improving the positioning accuracy. This work has reviewed various Ionospheric Models, both theoretical and&#xD;
Empirical, which have been designed for a better determination of variation of TEC values. These models, still useful for&#xD;
both the navigation and other scientific purposes are important for understanding the characteristics of the ionosphere and&#xD;
gaining insight about its temporal and spatial variations.
Page(s): 132-141</description>
      <pubDate>Wed, 01 Sep 2021 00:00:00 GMT</pubDate>
      <guid isPermaLink="false">http://nopr.niscpr.res.in/handle/123456789/58953</guid>
      <dc:date>2021-09-01T00:00:00Z</dc:date>
    </item>
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