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  <channel rdf:about="http://nopr.niscpr.res.in/handle/123456789/26774">
    <title>NOPR Collection: &lt;b&gt;Special Issue: Improved understanding of the structure and dynamics of the middle atmosphere and its response to various geophysical phenomena (Guest Editor: Gopa Dutta)&lt;/b&gt;</title>
    <link>http://nopr.niscpr.res.in/handle/123456789/26774</link>
    <description>&lt;b&gt;Special Issue: Improved understanding of the structure and dynamics of the middle atmosphere and its response to various geophysical phenomena (Guest Editor: Gopa Dutta)&lt;/b&gt;</description>
    <items>
      <rdf:Seq>
        <rdf:li rdf:resource="http://nopr.niscpr.res.in/handle/123456789/27170" />
        <rdf:li rdf:resource="http://nopr.niscpr.res.in/handle/123456789/27169" />
        <rdf:li rdf:resource="http://nopr.niscpr.res.in/handle/123456789/27168" />
        <rdf:li rdf:resource="http://nopr.niscpr.res.in/handle/123456789/27167" />
      </rdf:Seq>
    </items>
    <dc:date>2026-10-10T02:23:25Z</dc:date>
  </channel>
  <item rdf:about="http://nopr.niscpr.res.in/handle/123456789/27170">
    <title>Large scale anomalous temperature and wind variations in the lower and middle atmospheres during the solar eclipse of 15 January 2010</title>
    <link>http://nopr.niscpr.res.in/handle/123456789/27170</link>
    <description>Title: Large scale anomalous temperature and wind variations in the lower and middle atmospheres during the solar eclipse of 15 January 2010
Authors: Ramkumar, T K; Ghosh, Priyanka; Reddy, K Krishna; Kumar, K Niranjan; Kumar, S Balaji; Reddy, A Hari Krishna; Reddy, M Venkatrami; Prasad, S B Surendra
Abstract: During 12-17 January 2010 centered around 15&#xD;
January, annular solar eclipse event occurred over the Indian tropical region.&#xD;
The Indian Space Research Organisation (ISRO) sponsored and provided 18 GPS&#xD;
radiosondes (ISRO developed Dr Pisharoty sondes) to the Department of Physics, Yogi Vemana&#xD;
 University, Kadapa&#xD;
(14.5°N, 78.9°E), to study the effects of solar eclipse on the atmospheric&#xD;
dynamics and structure. The analyses of the data obtained from these&#xD;
radiosondes launched by balloons indicate that during this eclipse period, the&#xD;
atmosphere experienced ever recorded largest stratospheric cooling (maximum&#xD;
cooling of ~15 K at 36 km). As a first time ever report, significant localized&#xD;
variations in the strength of the large-scale zonal Walker and meridional Hadley circulations&#xD;
were also found over the Indian longitude region during this solar eclipse&#xD;
event.
Page(s): 75-82</description>
    <dc:date>2014-02-01T00:00:00Z</dc:date>
  </item>
  <item rdf:about="http://nopr.niscpr.res.in/handle/123456789/27169">
    <title>A case study of gravity waves observed in OH rotational temperatures at  Kolhapur (16.8ºN, 74.1ºE), India</title>
    <link>http://nopr.niscpr.res.in/handle/123456789/27169</link>
    <description>Title: A case study of gravity waves observed in OH rotational temperatures at  Kolhapur (16.8ºN, 74.1ºE), India
Authors: Parihar, Navin; Mukherjee, G K
Abstract: &lt;span style="mso-bidi-font-family:" times="" new="" roman""="" lang="EN-GB"&gt;Ground-based&#xD;
measurements of OH (8, 3) Meinel band emissions were carried out at Kolhapur (16.8ºN, 74.1ºE), India during November 2002 – May&#xD;
2003 using two tilting filter photometers. OH rotational temperature ~ a proxy&#xD;
of atmospheric temperature around 87 km, were derived from the intensity&#xD;
information of P&lt;sub&gt;1&lt;/sub&gt;(2) and P&lt;sub&gt;1&lt;/sub&gt;(4) lines of OH (8, 3) band.&#xD;
On most nights, strong well-defined oscillations having periodicities in the&#xD;
range of 1 – 3 h were observed in OH temperature series. In this paper, a case&#xD;
study of such short-period oscillations, observed on few nights in the OH&#xD;
temperature, has been presented.&#xD;
&#xD;
&lt;/span&gt;
Page(s): 67-74</description>
    <dc:date>2014-02-01T00:00:00Z</dc:date>
  </item>
  <item rdf:about="http://nopr.niscpr.res.in/handle/123456789/27168">
    <title>Modulation of thermal structure in the upper troposphere and lower stratosphere (UTLS) region by inertia gravity waves: A case study inferred from simultaneous MST radar and GPS sonde observations</title>
    <link>http://nopr.niscpr.res.in/handle/123456789/27168</link>
    <description>Title: Modulation of thermal structure in the upper troposphere and lower stratosphere (UTLS) region by inertia gravity waves: A case study inferred from simultaneous MST radar and GPS sonde observations
Authors: Das, Siddarth Shankar; Kumar, K K; Uma, K N; Ratnam, M V; Patra, A K; Das, S K; Ghosh, A K; Jain, A R
Abstract: The observations of multiple layer&#xD;
structures in the MST radar backscattering echoes in the upper troposphere and&#xD;
lower stratosphere (UTLS) region are discussed in this paper. The fact remains&#xD;
same that the enhanced echoes seen in the radar backscattering are due to the&#xD;
strong positive and negative thermal gradients. Simultaneous observations of&#xD;
MST radar &#xD;
(1 hourly) and GPS sonde (6 hourly) over a tropical station Gadanki (13.5°N,&#xD;
79.2°E) reveal the presence of 1.5-2 km vertical wavelength in the winds,&#xD;
temperature and radar backscattering echoes in the UTLS region during Indian&#xD;
summer monsoon (ISM). The analysis also reveals that the presence of inertia gravity&#xD;
wave (IGW) triggered due to tropical easterly jet (TEJ) associated with ISM is&#xD;
the prime candidate for the observed thermal gradients in the UTLS region.
Page(s): 11-23</description>
    <dc:date>2014-02-01T00:00:00Z</dc:date>
  </item>
  <item rdf:about="http://nopr.niscpr.res.in/handle/123456789/27167">
    <title>Effect of cumulus and microphysical parameterizations on the &lt;i style="mso-bidi-font-style:normal"&gt;JAL&lt;/i&gt; cyclone prediction</title>
    <link>http://nopr.niscpr.res.in/handle/123456789/27167</link>
    <description>Title: Effect of cumulus and microphysical parameterizations on the &lt;i style="mso-bidi-font-style:normal"&gt;JAL&lt;/i&gt; cyclone prediction
Authors: Reddy, M Venkatarami; Prasad, S B Surendra; Krishna, U V Murali; Reddy, K Krishna
Abstract: &lt;span style="mso-fareast-font-family:Calibri;mso-bidi-language:HI" lang="EN-GB"&gt;Weather&#xD;
Research and Forecasting (WRF) model is used to predict the track and intensity&#xD;
of &lt;i style="mso-bidi-font-style:normal"&gt;JAL&lt;/i&gt; cyclone, which formed during 04-08 November 2010 &lt;span style="mso-fareast-font-family:&#xD;
Calibri;mso-bidi-language:HI" lang="EN-GB"&gt;over the Bay of Bengal.&#xD;
The model has been simulated with numerous experiments using the logical/scientific&#xD;
combination of convection and micro-physics schemes. The model simulations have&#xD;
been conducted &#xD;
with different initial conditions to know the effective track and intensity&#xD;
prediction of &lt;i style="mso-bidi-font-style:normal"&gt;JAL&lt;/i&gt; cyclone. In&#xD;
addition, t&lt;span style="mso-fareast-font-family:PMingLiU;&#xD;
mso-fareast-language:ZH-TW;mso-bidi-language:HI" lang="EN-GB"&gt;he effect of cumulus&#xD;
parameterization schemes at different resolution (27 and 9 km) on the cyclone&#xD;
track and intensity &lt;span style="mso-fareast-font-family:&#xD;
Calibri;mso-bidi-language:HI" lang="EN-GB"&gt;is reported&lt;span style="mso-fareast-font-family:PMingLiU;mso-fareast-language:ZH-TW;mso-bidi-language:&#xD;
HI" lang="EN-GB"&gt;. &#xD;
The model simulated results showed the importance of cumulus schemes and their&#xD;
role at 9 km horizontal resolution. &#xD;
The results indicate that the track predicted by&#xD;
&lt;span style="mso-bidi-font-style:italic"&gt;Kain-Fritsch (KF) scheme is in&#xD;
good agreement with the observed track in all the experiments and the land fall&#xD;
error is minimum (~11 km) for the combination of Ferrier and KF scheme &lt;span style="mso-fareast-font-family:Calibri;mso-bidi-language:HI" lang="EN-GB"&gt;with &lt;span style="mso-bidi-font-style:italic" lang="EN-GB"&gt;0000 hrs UTC on 04 November 2010&#xD;
as &lt;span style="mso-fareast-font-family:Calibri;mso-bidi-language:&#xD;
HI" lang="EN-GB"&gt;initial condition.&lt;span style="mso-fareast-font-family:Calibri;mso-bidi-language:HI" lang="EN-GB"&gt; Strong intensity&#xD;
is produced by KF, New Grell (&lt;span style="mso-bidi-font-style:&#xD;
italic"&gt;NG)&lt;span style="mso-fareast-font-family:Calibri;&#xD;
mso-bidi-language:HI" lang="EN-GB"&gt; schemes and weak intensity is produced by &lt;span style="mso-bidi-font-style:italic" lang="EN-GB"&gt;Betts-Miller-Janjic (BMJ)&lt;span style="mso-fareast-font-family:Calibri;mso-bidi-language:HI" lang="EN-GB"&gt; scheme&#xD;
with all microphysics parameterization&lt;span style="mso-fareast-font-family:&#xD;
PMingLiU;mso-fareast-language:ZH-TW;mso-bidi-language:HI" lang="EN-GB"&gt; (&lt;span style="mso-fareast-font-family:PMingLiU;mso-bidi-language:TE" lang="EN-GB"&gt;MP&lt;span style="mso-fareast-font-family:PMingLiU;mso-fareast-language:ZH-TW;&#xD;
mso-bidi-language:TE" lang="EN-GB"&gt;)&lt;span style="mso-fareast-font-family:&#xD;
Calibri;mso-bidi-language:HI" lang="EN-GB"&gt; combinations. Further, the d&lt;span style="mso-fareast-font-family:PMingLiU;mso-fareast-language:ZH-TW;&#xD;
mso-bidi-language:HI" lang="EN-GB"&gt;ependency of intensity of cyclone has been studied in&#xD;
terms of surface latent heat flux, divergence and vorticity fields. To validate the model performance, different&#xD;
meteorological parameters are derived from the model simulations over three&#xD;
different regions and are compared with the observed meteorological parameters.&#xD;
The model results are in good agreement with the observed parameters, but&#xD;
variations are observed at the landfall /dissipation of the cyclone.&lt;span style="mso-fareast-font-family:Calibri;mso-bidi-language:HI" 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;&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): 103-123</description>
    <dc:date>2014-02-01T00:00:00Z</dc:date>
  </item>
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