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  <title>NOPR Collection:</title>
  <link rel="alternate" href="http://nopr.niscpr.res.in/handle/123456789/25563" />
  <subtitle />
  <id>http://nopr.niscpr.res.in/handle/123456789/25563</id>
  <updated>2026-10-12T11:08:27Z</updated>
  <dc:date>2026-10-12T11:08:27Z</dc:date>
  <entry>
    <title>Harmful electromagnetic environment near transmission tower</title>
    <link rel="alternate" href="http://nopr.niscpr.res.in/handle/123456789/25801" />
    <author>
      <name>Pathak, P P</name>
    </author>
    <author>
      <name>Kumar, Vijay</name>
    </author>
    <author>
      <name>Vats, R P</name>
    </author>
    <id>http://nopr.niscpr.res.in/handle/123456789/25801</id>
    <updated>2014-01-29T16:53:31Z</updated>
    <published>2003-08-01T00:00:00Z</published>
    <summary type="text">Title: Harmful electromagnetic environment near transmission tower
Authors: Pathak, P P; Kumar, Vijay; Vats, R P
Abstract: The penetration of&#xD;
RF and microwave electromagnetic fields into human body and its possible consequences&#xD;
are studied. Earlier observations are theoretically verified which show that the&#xD;
radiation from high power transmission tower is more harmful to the people living&#xD;
nearby as compared to that from the low power transmission tower. Absorption of&#xD;
electric&#xD;
&#xD;
component of&#xD;
electromagnetic radiation falling on the body, which increases with frequency, may&#xD;
result into temperature rise in the body. However, the magnetic induction, being&#xD;
very weak in comparison to the earth's magnetic field, is expected to have no effect&#xD;
on the human body.
Page(s): 238-241</summary>
    <dc:date>2003-08-01T00:00:00Z</dc:date>
  </entry>
  <entry>
    <title>Aerosol optical depth variation observed using sun-photometer over Indore</title>
    <link rel="alternate" href="http://nopr.niscpr.res.in/handle/123456789/25800" />
    <author>
      <name>Gupta, Pawan</name>
    </author>
    <author>
      <name>Gadhavi, Harish</name>
    </author>
    <author>
      <name>Jayaraman, A</name>
    </author>
    <id>http://nopr.niscpr.res.in/handle/123456789/25800</id>
    <updated>2014-01-17T16:51:23Z</updated>
    <published>2003-08-01T00:00:00Z</published>
    <summary type="text">Title: Aerosol optical depth variation observed using sun-photometer over Indore
Authors: Gupta, Pawan; Gadhavi, Harish; Jayaraman, A
Abstract: Columnar aerosol&#xD;
optical depth measurements have been made over Indore (22.7° N, 75.9° E) during&#xD;
May 2001-March 2002 at four spectral bands centred around 400, 499, 668 and 858&#xD;
nm using a hand-held sun-photometer. The aerosol optical depth (AOD) shows&#xD;
seasonal variation with high values in summer and low values in winter. The&#xD;
summer-increase is found to be due to the high wind speed producing larger amount&#xD;
of wind-derived dust particles. As the summer monsoon sets in at the end of&#xD;
June there is an appreciable decrease in the AOD values. The AOD values decrease&#xD;
further in winter and the decrease is more at higher wavelengths indicating that&#xD;
there is a general reduction in the number of bigger particles. Also during winter&#xD;
months the wind direction changed to southerly and south-easterly which brings air&#xD;
that is more rural to the measurement site. The amplitude of the observed high AOD&#xD;
values in summer and low during winter, is higher for longer wavelengths which shows&#xD;
that the coarse particles contribute more to the observed variation as compared&#xD;
to sub-micron particles. Comparison of the AOD values over Indore with that of Trivandrum&#xD;
and Visakhapatnam shows that the Indore values are comparable to that of Vi sakhapatnam,&#xD;
but much higher than the Trivandrum values indicating the influence of&#xD;
&#xD;
industrialization&#xD;
and higher population.
Page(s): 229-237</summary>
    <dc:date>2003-08-01T00:00:00Z</dc:date>
  </entry>
  <entry>
    <title>Diurnal and seasonal variations of point discharge current during thunderstorms at a tropical inland station</title>
    <link rel="alternate" href="http://nopr.niscpr.res.in/handle/123456789/25799" />
    <author>
      <name>Kandalgaonkar, S S</name>
    </author>
    <author>
      <name>Tinmaker, M I R</name>
    </author>
    <author>
      <name>Kulkarni, M K</name>
    </author>
    <author>
      <name>Nath, Asha</name>
    </author>
    <id>http://nopr.niscpr.res.in/handle/123456789/25799</id>
    <updated>2014-01-18T16:51:04Z</updated>
    <published>2003-08-01T00:00:00Z</published>
    <summary type="text">Title: Diurnal and seasonal variations of point discharge current during thunderstorms at a tropical inland station
Authors: Kandalgaonkar, S S; Tinmaker, M I R; Kulkarni, M K; Nath, Asha
Abstract: The data of&#xD;
point discharge current (PDC) measurements during a total of 65 thunderstorms at&#xD;
Pune (18°32&lt;i&gt;'&lt;/i&gt;N, 73°51&lt;i&gt;'&lt;/i&gt;E) are analyzed to study the PDC local diurnal&#xD;
variation and some issues related with the current. The analysis shows that about&#xD;
83% of the total quarter hours occupied by PDC are localized between 1400 hrs LT&#xD;
and 2400 hrs LT and the remaining 17% are sparsely distributed over midnight to&#xD;
early hours in the morning. The net result of this study revealed that PDC is the&#xD;
dominant agent for the negative charging of the earth’s surface and should be&#xD;
identified as an active element participating in global electrical circuit. The&#xD;
phase relationship between the positive and negative current during the diurnal&#xD;
period suggests that the active period of current of one polarity has a preferred&#xD;
time of occurrence over the other and by the late night hours the positive&#xD;
charge showed its sustained occurrence over the negative one. The seasonal&#xD;
relationship between storm averaged PDC and monthly mean maximum surface air&#xD;
temperature has also been examined. The comparison of seasonal&#xD;
&#xD;
average amplitude&#xD;
of PDC has suggested a strong positive correlation with the monthly mean maximum&#xD;
surface air temperature. The average amplitude of PDC during thunderstorm in premonsoon&#xD;
season is found to be about three times higher than those during the monsoon season.&#xD;
An examination of association between duration and amplitude variation of PDC showed&#xD;
that storms that are closer to the station within 4 km have longer duration and&#xD;
stronger current amplitude than when they are more than 4 km away.
Page(s): 221-228</summary>
    <dc:date>2003-08-01T00:00:00Z</dc:date>
  </entry>
  <entry>
    <title>Drop size distribution of rainfall of different intensities</title>
    <link rel="alternate" href="http://nopr.niscpr.res.in/handle/123456789/25798" />
    <author>
      <name>Kumar, V Sasi</name>
    </author>
    <author>
      <name>Sampath, S</name>
    </author>
    <author>
      <name>Vinayak, P V S S K</name>
    </author>
    <id>http://nopr.niscpr.res.in/handle/123456789/25798</id>
    <updated>2014-01-20T16:52:03Z</updated>
    <published>2003-08-01T00:00:00Z</published>
    <summary type="text">Title: Drop size distribution of rainfall of different intensities
Authors: Kumar, V Sasi; Sampath, S; Vinayak, P V S S K
Abstract: Drop size distribution&#xD;
was measured at Thiruvananthapuram, Kerala State, India, during April, June and&#xD;
July 2001 using a Joss-Waldvogel type disdrometer. The instrument gives the number&#xD;
of drops in 20 size classes ranging from 0.3 mm to &gt; 5 mm. Each month's data&#xD;
were sorted, based on rainfall intensity, into periods of rainfall intensity &lt;&#xD;
1 mm/h r, 1-3 mm/ hr, 3-10 mm/hr, 10-30 mm/hr and &gt; 30 mm/hr. The average number&#xD;
of drops in each size class was computed for each set of data. Exponential and&#xD;
Г distribution functions were then fitted to each data set. The results showed that,&#xD;
in June and July, the data approximated an exponential distribution for low rainfall&#xD;
intensities, but became closer to the Г distribution at higher intensities. However,&#xD;
in April all data fitted the Г distribution, irrespective of rainfall intensity.
Page(s): 217-220</summary>
    <dc:date>2003-08-01T00:00:00Z</dc:date>
  </entry>
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