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    <title>NOPR Collection:</title>
    <link>http://nopr.niscpr.res.in/handle/123456789/31309</link>
    <description />
    <pubDate>Sat, 10 Oct 2026 17:18:18 GMT</pubDate>
    <dc:date>2026-10-10T17:18:18Z</dc:date>
    <item>
      <title>Methane emission from open drain</title>
      <link>http://nopr.niscpr.res.in/handle/123456789/31328</link>
      <description>Title: Methane emission from open drain
Authors: Purkait, N N; Chakrabarty, D K
Abstract: Solid waste that comes along with the&#xD;
wastewater from household gets deposited at the bottom of the drain. With&#xD;
passage of time, this solid waste starts decomposing and starts releasing&#xD;
methane. Methane is an important greenhouse gas, which is non-toxic but highly&#xD;
flammable. It is also an asphyxiant and can be fatal. Every year several people&#xD;
die for this reason while cleaning solid sewage of choked drains. Methane&#xD;
emission measurements from three drains of Kolkata were made during 2009-2010.&#xD;
The results are presented in this communication. It is found that methane&#xD;
emission from drains is ~4-100 times greater than that from paddy field. Data&#xD;
obtained in this work will be a valuable input for making reliable prediction&#xD;
of methane loading in the atmosphere and alert workers of the danger in order to&#xD;
take adequate safety measure before cleaning sewage sediments.
Page(s): 56-59</description>
      <pubDate>Sun, 01 Mar 2015 00:00:00 GMT</pubDate>
      <guid isPermaLink="false">http://nopr.niscpr.res.in/handle/123456789/31328</guid>
      <dc:date>2015-03-01T00:00:00Z</dc:date>
    </item>
    <item>
      <title>A simple model for estimation of snow/ice surface temperature of Antarctic ice sheet using remotely sensed thermal band data</title>
      <link>http://nopr.niscpr.res.in/handle/123456789/31327</link>
      <description>Title: A simple model for estimation of snow/ice surface temperature of Antarctic ice sheet using remotely sensed thermal band data
Authors: Gusain, H S; Mishra, V D; Brar, Gursewak Singh; Ganju, Ashwagosha
Abstract: In this paper, a model has been developed to&#xD;
estimate surface temperature of Antarctic ice sheet using thermal bands of&#xD;
Moderate Resolution Imaging Spectroradiometer (MODIS) sensor images and in situ&#xD;
surface temperature measurements. The brightness temperature of snow/ice surface&#xD;
of Antarctica has been estimated for MODIS bands 31 and 32 using Planck’s&#xD;
spectral radiation equation. Split window technique has been used to develop&#xD;
the model from brightness temperature and Automatic Weather Station recorded&#xD;
surface temperature. The model has been validated using &lt;i&gt;in situ &lt;/i&gt;measurements&#xD;
of surface temperature of the ice sheet near Indian Antarctic Research Station&#xD;
‘Maitri’. High coefficient of determination (R2 in the range 0.952 - 0.99) and&#xD;
low root mean square error (0.8 - 1.2°C) has been obtained between modeled and &lt;i&gt;in&#xD;
situ&lt;/i&gt; recorded surface temperature. The model is easy to use and can&#xD;
generate the surface temperature maps at spatial resolution of 1.0 km. These&#xD;
maps can be useful in various glaciological, hydrological, climatological and&#xD;
ecological studies of the ice sheet.
Page(s): 51-55</description>
      <pubDate>Sun, 01 Mar 2015 00:00:00 GMT</pubDate>
      <guid isPermaLink="false">http://nopr.niscpr.res.in/handle/123456789/31327</guid>
      <dc:date>2015-03-01T00:00:00Z</dc:date>
    </item>
    <item>
      <title>Rain attenuation using Ka and Ku band frequency beacons at Delhi Earth Station</title>
      <link>http://nopr.niscpr.res.in/handle/123456789/31326</link>
      <description>Title: Rain attenuation using Ka and Ku band frequency beacons at Delhi Earth Station
Authors: Sujimol, M R; Acharya, Rajat; Singh, Gajendra; Gupta, Ravi Kumar
Abstract: Quantitative analysis and prediction of&#xD;
radio signal attenuation is necessary in order to improve the reliability of&#xD;
satellite-earth communication links and for economically efficient design. The Ka&#xD;
band suffers large attenuation due to rain and as most of the parts of India are&#xD;
situated in the tropical region, the impact of rain on Ka band propagation is&#xD;
severe. None of the existing ITU-R models is validated for prediction of rain&#xD;
attenuation over India and only a few over the tropical region and hence, it&#xD;
calls for a propagation experiment to validate the existing models. In this&#xD;
paper, study on the effect of rain attenuation&#xD;
on the propagation of satellite signals in Ka band has been carried out by&#xD;
receiving signal of frequency 20.199 GHz from the IPSTAR (Thaicom-4&#xD;
Satellite) and a Ku band beacon signal of frequency 11.698 GHz from GSAT-8&#xD;
satellite at Delhi Earth Station of ISRO. It has been observed that the&#xD;
difference between the ITU-R predicted rain attenuations and the observed rain&#xD;
attenuations for Ka band varies from 1.5 to 4.5 dB and that for Ku band from&#xD;
2.1 to 3.7 dB. The long-term probability distribution of fade slope for any&#xD;
definite base value of attenuation is symmetric on both positive and negative&#xD;
sides and this feature is independent of frequency. This observation&#xD;
corroborates earlier findings.
Page(s): 45-50</description>
      <pubDate>Sun, 01 Mar 2015 00:00:00 GMT</pubDate>
      <guid isPermaLink="false">http://nopr.niscpr.res.in/handle/123456789/31326</guid>
      <dc:date>2015-03-01T00:00:00Z</dc:date>
    </item>
    <item>
      <title>Atmospheric turbulences over Guwahati and their association with tropospheric dynamics</title>
      <link>http://nopr.niscpr.res.in/handle/123456789/31325</link>
      <description>Title: Atmospheric turbulences over Guwahati and their association with tropospheric dynamics
Authors: Medhi, A; Devi, M; Goswami, H; Barbara, A K
Abstract: &lt;span style="letter-spacing:-.1pt;mso-fareast-language:&#xD;
AS;mso-bidi-language:AS" lang="EN-GB"&gt;The paper presents an analysis of structure constant&#xD;
parameter (Cn&lt;sup&gt;2&lt;/sup&gt;) over Guwahati (26.2°N, 91.75°E&lt;span style="letter-spacing:-.1pt;mso-fareast-language:AS;mso-bidi-language:AS" lang="EN-GB"&gt;) in&#xD;
relation to tropospheric dynamics involving atmospheric variabilities, like&#xD;
temperature, potential temperature and specific humidity. Data collected from radiosonde operated at Guwahati are utilised for&#xD;
drawing seasonal profiles of Cn&lt;sup&gt;2&lt;/sup&gt; up to the tropopause height. The&#xD;
results show that depending on season, the average values of Cn&lt;sup&gt;2&lt;/sup&gt; may&#xD;
vary between 10&lt;sup&gt;-14.5&lt;/sup&gt; and 10&lt;sup&gt;-19&lt;/sup&gt; m&lt;sup&gt;-2/3&lt;/sup&gt; and that&#xD;
their magnitude decreases gradually to reach a minimum of -18.3 m&lt;sup&gt;-2/3 &lt;/sup&gt;at&#xD;
around 10 km and then starts increasing up to the tropopause height of 15-16&#xD;
km. The analysis, further, demonstrates that Cn&lt;sup&gt;2&lt;/sup&gt; value reaches&#xD;
maximum in summer and minimum in winter, within the height range of 1-10 km. Bu&lt;span style="letter-spacing:-.1pt;mso-ansi-language:EN-SG;mso-fareast-language:&#xD;
AS;mso-bidi-language:AS" lang="EN-SG"&gt;t beyond the altitude of 10 km, Cn&lt;sup&gt;2&lt;/sup&gt; shows&#xD;
higher values in winter as compared to its summer time counterparts. &lt;span style="letter-spacing:-.1pt;mso-fareast-language:AS;mso-bidi-language:&#xD;
AS" lang="EN-GB"&gt;The paper also highlights that at pre earthquake (EQ) ambiences, &lt;span style="letter-spacing:-.1pt;mso-ansi-language:EN-SG;mso-fareast-language:&#xD;
AS;mso-bidi-language:AS" lang="EN-SG"&gt;this parameter&lt;span style="letter-spacing:-.1pt;mso-fareast-language:AS;mso-bidi-language:AS" lang="EN-GB"&gt; may&#xD;
dip down by two to three orders of magnitude from its average normal range. The&#xD;
seasonal transition pattern of Cn&lt;sup&gt;2 &lt;/sup&gt;with height and the EQ time&#xD;
changes in Cn&lt;sup&gt;2&lt;/sup&gt; features are put to a correlative analysis with the&#xD;
tropospheric dynamics for an explanation. &#xD;
&#xD;
&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;
Page(s): 35-44</description>
      <pubDate>Sun, 01 Mar 2015 00:00:00 GMT</pubDate>
      <guid isPermaLink="false">http://nopr.niscpr.res.in/handle/123456789/31325</guid>
      <dc:date>2015-03-01T00:00:00Z</dc:date>
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