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  <title>NOPR Collection:</title>
  <link rel="alternate" href="http://nopr.niscpr.res.in/handle/123456789/24965" />
  <subtitle />
  <id>http://nopr.niscpr.res.in/handle/123456789/24965</id>
  <updated>2026-10-10T22:00:41Z</updated>
  <dc:date>2026-10-10T22:00:41Z</dc:date>
  <entry>
    <title>Retrieval of water vapour profiles from radio occultation refractivity  using artificial neural network</title>
    <link rel="alternate" href="http://nopr.niscpr.res.in/handle/123456789/24978" />
    <author>
      <name>Shyam, Abhineet</name>
    </author>
    <author>
      <name>Gohil, B S</name>
    </author>
    <author>
      <name>Basu, Sujit</name>
    </author>
    <id>http://nopr.niscpr.res.in/handle/123456789/24978</id>
    <updated>2014-01-02T16:50:49Z</updated>
    <published>2013-12-01T00:00:00Z</published>
    <summary type="text">Title: Retrieval of water vapour profiles from radio occultation refractivity  using artificial neural network
Authors: Shyam, Abhineet; Gohil, B S; Basu, Sujit
Abstract: Artificial neural network (ANN) technique&#xD;
has been used to derive water vapour pressure profiles in the troposphere from&#xD;
radio occultation data over India and adjoining region. A fully connected&#xD;
three-layer network, with one hidden layer, has been constructed and standard&#xD;
back&lt;span style="mso-bidi-font-family:Arial" lang="EN-GB"&gt; propagation algorithm has been used to train the network. While month, latitude&#xD;
and vertical profile of refractivity&lt;span style="mso-bidi-font-family:&#xD;
Arial" lang="EN-GB"&gt;/bending angle constitute the input vector, the&#xD;
water v&lt;span style="mso-bidi-font-family:Arial" lang="EN-GB"&gt;apour &lt;span style="mso-bidi-font-family:Arial" lang="EN-GB"&gt;partial &lt;span style="mso-bidi-font-family:Arial" lang="EN-GB"&gt;pressure profile forms the output vector. Only the moisture-laden summer&#xD;
monsoon months of June, July, August and September of 2010 have been considered&#xD;
for developing the retrieval algorithm. There are 2120 input and output pairs,&#xD;
out of which 1696 pairs form the training set while the remaining pairs&#xD;
constitute the validation set. The retrieved profiles of water vapour pressures&#xD;
in the validation set have been compared with the corresponding COSMIC&#xD;
operational products of water vapour pressure profiles. The effectiveness of&#xD;
the algorithm is apparent from this comparison and also from the vertical&#xD;
profiles of bias and root mean square error (RMSE). &lt;span style="mso-bidi-font-family:Arial" lang="EN-GB"&gt;The statistics show&#xD;
better performance of the algorithm with refractivity as one of the inputs than&#xD;
with bending angle. The RMSE in water vapour retrieval from refractivity is&#xD;
within 1.5-2 hPa compared to markedly higher values of 6 hPa when derived from&#xD;
bending angle. Additionally, the algorithm has &lt;span style="mso-bidi-font-family:Arial" lang="EN-GB"&gt;also &lt;span style="mso-bidi-font-family:Arial" lang="EN-GB"&gt;been&#xD;
tested in an independent year 2009 and the performance of the refractivity&#xD;
based retrieval has been found to be &lt;span style="mso-bidi-font-family:&#xD;
Arial" lang="EN-GB"&gt;highly consistent in the year 2010, with RMSE&#xD;
within 1.5 hPa&lt;span style="mso-bidi-font-family:Arial" lang="EN-GB"&gt;. &#xD;
&#xD;
&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;
Page(s): 411-419</summary>
    <dc:date>2013-12-01T00:00:00Z</dc:date>
  </entry>
  <entry>
    <title>Assessment of electromagnetic radiation for second and third generation frequency spectrum on human body</title>
    <link rel="alternate" href="http://nopr.niscpr.res.in/handle/123456789/24977" />
    <author>
      <name>Sharma, Pragati</name>
    </author>
    <author>
      <name>Gautam, A K</name>
    </author>
    <author>
      <name>Kumar, Sandeep</name>
    </author>
    <id>http://nopr.niscpr.res.in/handle/123456789/24977</id>
    <updated>2013-12-23T16:46:12Z</updated>
    <published>2013-12-01T00:00:00Z</published>
    <summary type="text">Title: Assessment of electromagnetic radiation for second and third generation frequency spectrum on human body
Authors: Sharma, Pragati; Gautam, A K; Kumar, Sandeep
Abstract: The rapid&#xD;
diffusion of wireless communication systems such as mobile phones has caused an&#xD;
increased concern for the potential effects on human health deriving from&#xD;
exposure to electromagnetic fields emitted by antennas and base stations of&#xD;
these systems. A number of studies have been conducted on the topic of&#xD;
electromagnetic field effects over human body. All earlier studies were&#xD;
centered on the second generation (2G) global system for mobile communication&#xD;
(GSM). Now, third generation (3G) mobiles and towers have been launched in the&#xD;
market, therefore, it is high time to calculate the radiation effect of increased&#xD;
frequency of 3G system over human body. In this paper, the specific absorption&#xD;
rate (SAR) value for skin (dry and wet) tissues of human body have been&#xD;
evaluated at 900, 1800 and 2140 MHz frequency bands. The first two frequencies&#xD;
represent the second generation (2G) and the third frequency represents the&#xD;
third generation (3G), respectively. The skin exposure due to base transceiver&#xD;
station (BTS) is calculated through SAR up to a distance of 3.5 mm inside skin&#xD;
for these frequencies. It has been found that values of SAR for electromagnetic&#xD;
radiation due to 2G and 3G frequency spectrums are very highly distributed near&#xD;
the source of radiation (BTS) and SAR have more effect on skin as one moves&#xD;
towards higher frequency band.
Page(s): 425-428</summary>
    <dc:date>2013-12-01T00:00:00Z</dc:date>
  </entry>
  <entry>
    <title>Comparison of SMOS soil moisture/brightness temperatures for morning  and evening passes</title>
    <link rel="alternate" href="http://nopr.niscpr.res.in/handle/123456789/24976" />
    <author>
      <name>Calla, O P N</name>
    </author>
    <author>
      <name>Sharma, Rahul</name>
    </author>
    <author>
      <name>Gadri, Kishan Lal</name>
    </author>
    <author>
      <name>Kalla, Abhishek</name>
    </author>
    <author>
      <name>Agrahari, Sunil Kumar</name>
    </author>
    <author>
      <name>Rathore, Gaurav</name>
    </author>
    <id>http://nopr.niscpr.res.in/handle/123456789/24976</id>
    <updated>2013-12-23T16:46:04Z</updated>
    <published>2013-12-01T00:00:00Z</published>
    <summary type="text">Title: Comparison of SMOS soil moisture/brightness temperatures for morning  and evening passes
Authors: Calla, O P N; Sharma, Rahul; Gadri, Kishan Lal; Kalla, Abhishek; Agrahari, Sunil Kumar; Rathore, Gaurav
Abstract: Soil moisture is an essential element, which&#xD;
controls the land-atmospheric system and thus, its continuous monitoring is&#xD;
extremely important. Regular monitoring of spatio-temporal variability of&#xD;
surface soil moisture can be done using microwave remote sensing techniques, as&#xD;
there is high contrast in dielectric properties of pure dry soil (2-3) and pure&#xD;
water (80) at microwave frequencies. Variation in surface soil moisture is not&#xD;
only affected by precipitation, evaporation and transpiration, but often&#xD;
groundwater and root zone moisture also play an important role. In the present&#xD;
paper, surface soil moisture data from Soil Moisture and Ocean Salinity (SMOS)&#xD;
satellite is used to analyse the changes in surface soil moisture from evening&#xD;
to next or following morning (6.00 PM and 6.00 AM) in an arid region of&#xD;
Rajasthan, India. An increase in surface soil moisture is observed for maximum&#xD;
data from evening to following morning. The same trends were also verified&#xD;
using polarization index values.
Page(s): 420-424</summary>
    <dc:date>2013-12-01T00:00:00Z</dc:date>
  </entry>
  <entry>
    <title>Effects of backscattering enhancement considering multiple scattering in rain on MMW radar performance</title>
    <link rel="alternate" href="http://nopr.niscpr.res.in/handle/123456789/24975" />
    <author>
      <name>Yang, Rui-Ke</name>
    </author>
    <author>
      <name>Li, Li</name>
    </author>
    <author>
      <name>Ma, Hui-Hui</name>
    </author>
    <id>http://nopr.niscpr.res.in/handle/123456789/24975</id>
    <updated>2013-12-23T16:45:58Z</updated>
    <published>2013-12-01T00:00:00Z</published>
    <summary type="text">Title: Effects of backscattering enhancement considering multiple scattering in rain on MMW radar performance
Authors: Yang, Rui-Ke; Li, Li; Ma, Hui-Hui
Abstract: The theory of the&#xD;
second order backscattering enhancement in discrete random medium is discussed&#xD;
in this paper. &#xD;
The effects of rainfall on millimeter wave (MMW) radar performance are analysed&#xD;
based on Mie theory, Monte Carlo (MC) simulation and backscattering enhancement&#xD;
theory, at 35 and 95 GHz, respectively. The rain attenuation considering the&#xD;
raindrops multiple scattering is introduced into the estimation of the signal&#xD;
to clutter ratios (S/C) and the clutter to noise ratios (C/N) for MMW radar. The&#xD;
S/C and C/N are calculated by means of the backscattering enhancement, Mie&#xD;
theory and MC simulation method, respectively under the condition of rain&#xD;
environment. The results show that the S/C obtained by backscattering&#xD;
enhancement theory is smaller than the results by Mie and MC. The C/N by&#xD;
backscattering enhancement is greater than the results by other. The Mie and MC&#xD;
methods do not consider backscatter enhancement, underestimate the effect of&#xD;
raindrops scattering on radar performance. Hence, it is shown that the&#xD;
attenuation and backscattering enhancement induced by raindrops multiple&#xD;
scattering are necessarily taken into account for the performance estimation of&#xD;
MMW radar operating in&#xD;
heavy rainfall environment.
Page(s): 404-410</summary>
    <dc:date>2013-12-01T00:00:00Z</dc:date>
  </entry>
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