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  <title>NOPR Collection: &lt;b&gt;Special Issue on Coastal Dynamics, Marine Environment &amp; Resources, Ocean Engineering, Port and Harbour Engineering (Guest Editors: Jaya Kumar Seelam &amp; R. Mani Murali)&lt;/b&gt;</title>
  <link rel="alternate" href="http://nopr.niscpr.res.in/handle/123456789/34411" />
  <subtitle>&lt;b&gt;Special Issue on Coastal Dynamics, Marine Environment &amp; Resources, Ocean Engineering, Port and Harbour Engineering (Guest Editors: Jaya Kumar Seelam &amp; R. Mani Murali)&lt;/b&gt;</subtitle>
  <id>http://nopr.niscpr.res.in/handle/123456789/34411</id>
  <updated>2026-10-10T21:41:53Z</updated>
  <dc:date>2026-10-10T21:41:53Z</dc:date>
  <entry>
    <title>Thermal pollution modelling of cooling water discharge into a closed creek system</title>
    <link rel="alternate" href="http://nopr.niscpr.res.in/handle/123456789/34462" />
    <author>
      <name>Buvaneshwari, S.</name>
    </author>
    <author>
      <name>Ravichandran, Vijaya</name>
    </author>
    <author>
      <name>Mudgal, B. V.</name>
    </author>
    <id>http://nopr.niscpr.res.in/handle/123456789/34462</id>
    <updated>2016-07-20T06:38:45Z</updated>
    <published>2014-07-01T00:00:00Z</published>
    <summary type="text">Title: Thermal pollution modelling of cooling water discharge into a closed creek system
Authors: Buvaneshwari, S.; Ravichandran, Vijaya; Mudgal, B. V.
Abstract: &lt;span style="font-size:9.0pt;font-family:" times="" new="" roman";="" mso-fareast-font-family:"times="" roman";mso-bidi-font-family:"times="" mso-ansi-language:en-in;mso-fareast-language:ja;mso-bidi-language:ar-sa"=""&gt;This&#xD;
paper is focused on the behaviour of the heated effluent discharged at an&#xD;
elevated temperature into the Ennore creek by North Chennai Thermal Power&#xD;
Station (NCTPS). Functioning of thermal power plants near tidal creeks and&#xD;
estuaries, due to the feasibility of intake and discharge of water for cooling&#xD;
poses serious environmental concern from heated water discharge due to the flow&#xD;
characteristics of the creek. Discharge of the heated effluent and its&#xD;
dispersion is a function of ebb and flood flow into the Ennore creek as the&#xD;
creek mouth remains closed for most part of the year. This study aims to&#xD;
investigate the dispersion characteristics of the heated effluent in the&#xD;
near-field and far-field under various discharge and dynamic conditions of the&#xD;
creek using calibrated hydrodynamic models and comparison with the field data&#xD;
measured during varying tidal conditions.&lt;/span&gt;
Page(s): 1415-1421</summary>
    <dc:date>2014-07-01T00:00:00Z</dc:date>
  </entry>
  <entry>
    <title>Mean surface meteorological parameter characterization at Kavaratti, Lakshadweep Island, South-East Arabian Sea</title>
    <link rel="alternate" href="http://nopr.niscpr.res.in/handle/123456789/34461" />
    <author>
      <name>Kumar, Vijay</name>
    </author>
    <author>
      <name>Mehra, Prakash</name>
    </author>
    <author>
      <name>Nair, Balakrishnan</name>
    </author>
    <author>
      <name>Agarvadekar, Yogesh</name>
    </author>
    <author>
      <name>Luis, Ryan</name>
    </author>
    <author>
      <name>Ghatge, Devika</name>
    </author>
    <author>
      <name>Lobo, Shane</name>
    </author>
    <author>
      <name>Harmalkar, Bharat</name>
    </author>
    <id>http://nopr.niscpr.res.in/handle/123456789/34461</id>
    <updated>2016-07-20T06:38:29Z</updated>
    <published>2014-07-01T00:00:00Z</published>
    <summary type="text">Title: Mean surface meteorological parameter characterization at Kavaratti, Lakshadweep Island, South-East Arabian Sea
Authors: Kumar, Vijay; Mehra, Prakash; Nair, Balakrishnan; Agarvadekar, Yogesh; Luis, Ryan; Ghatge, Devika; Lobo, Shane; Harmalkar, Bharat
Abstract: &lt;span style="font-size:9.0pt;font-family:" times="" new="" roman";="" mso-fareast-font-family:"times="" roman";mso-bidi-font-family:mangal;="" mso-ansi-language:en-in;mso-fareast-language:en-us;mso-bidi-language:hi"=""&gt;Soon&#xD;
after the south-west monsoon, mean surface meteorological parameters at the Kavaratti Island begin to change. Wind, which was&#xD;
south-west in direction during the monsoon period, turns to north-north and&#xD;
eventually to north-east direction with lesser intensity. Monthly mean wind&#xD;
speed in October was ~2 ms&lt;sup&gt;-1&lt;/sup&gt; while in July it was~7 ms&lt;sup&gt;-1&lt;/sup&gt;.&#xD;
Monthly mean surface air pressure in October was ~1008 hPa as against ~1007 hPa&#xD;
in July. Surface air-temperature and relative humidity also exhibited similar&#xD;
variability. Monthly mean air temperature and humidity in October were ~28&lt;sup&gt;&lt;span style="font-size:9.0pt;font-family:" times="" new="" roman";mso-fareast-font-family:="" "times="" roman";mso-bidi-font-family:"times="" roman";mso-ansi-language:="" en-in;mso-fareast-language:en-us;mso-bidi-language:hi"=""&gt;°&lt;/span&gt;&lt;/sup&gt;&lt;span style="font-size:9.0pt;font-family:" times="" new="" roman";mso-fareast-font-family:="" "times="" roman";mso-bidi-font-family:mangal;mso-ansi-language:en-in;="" mso-fareast-language:en-us;mso-bidi-language:hi"=""&gt;C, and ~76% respectively,&#xD;
while in July ~26&lt;sup&gt;&lt;span style="font-size:9.0pt;font-family:" times="" new="" roman";="" mso-fareast-font-family:"times="" roman";mso-bidi-font-family:"times="" mso-ansi-language:en-in;mso-fareast-language:en-us;mso-bidi-language:hi"=""&gt;°&lt;/span&gt;&lt;/sup&gt;&lt;span style="font-size:9.0pt;font-family:" times="" new="" roman";mso-fareast-font-family:="" "times="" roman";mso-bidi-font-family:mangal;mso-ansi-language:en-in;="" mso-fareast-language:en-us;mso-bidi-language:hi"=""&gt;C, and ~87% respectively were&#xD;
recorded. In general, wind was predominantly in the north/north-westerly&#xD;
direction throughout the year, except June-July during which a west/south-westerly&#xD;
winds was observed. Minimum atmospheric pressure occurs during June-July&#xD;
(southwest monsoon period) and the maximum during December-January (northeast&#xD;
monsoon period). Air temperature demonstrates steady increase from January to&#xD;
May before descending to minimum during July-August. During the observational&#xD;
period (2009) inverse relationships between barometric pressure and&#xD;
air-temperature was observed. Similar relationship between relative humidity&#xD;
and air-temperature was also noticed.&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;
Page(s): 1407-1414</summary>
    <dc:date>2014-07-01T00:00:00Z</dc:date>
  </entry>
  <entry>
    <title>Site selection for offshore wind farms along the Indian coast</title>
    <link rel="alternate" href="http://nopr.niscpr.res.in/handle/123456789/34460" />
    <author>
      <name>Murali, R. Mani</name>
    </author>
    <author>
      <name>Vidya, P.J.</name>
    </author>
    <author>
      <name>Modi, Poonam</name>
    </author>
    <author>
      <name>Kumar, Seelam Jaya</name>
    </author>
    <id>http://nopr.niscpr.res.in/handle/123456789/34460</id>
    <updated>2016-07-20T06:38:17Z</updated>
    <published>2014-07-01T00:00:00Z</published>
    <summary type="text">Title: Site selection for offshore wind farms along the Indian coast
Authors: Murali, R. Mani; Vidya, P.J.; Modi, Poonam; Kumar, Seelam Jaya
Abstract: &lt;span style="font-size:9.0pt;font-family:" times="" new="" roman";="" mso-fareast-font-family:"times="" roman";mso-bidi-font-family:mangal;="" mso-ansi-language:en-in;mso-fareast-language:en-in;mso-bidi-language:hi"=""&gt;This&#xD;
study deals with the location of the potential sites for offshore wind farms&#xD;
and also deals with the feasibility of installing offshore wind farms through&#xD;
scientific examination along the coast of India. Offshore wind energy is almost&#xD;
unexplored along the Indian coast. Potential and feasible regions need to be&#xD;
found and studied in detail. In this regard, few of the essential primary&#xD;
parameters such as bathymetry, wind velocity, proximity to the coast, ports,&#xD;
harbours, marine protected areas and marine sanctuaries were considered.&#xD;
Suitable sites for offshore wind farms were demarcated in a GIS environment.&#xD;
Weekly climatology (1999-2009) of wind speed was used to explore the seasonal&#xD;
wind potential. GIS analysis has brought out potential wind farms regions of&#xD;
32,000 km&lt;sup&gt;2&lt;/sup&gt; in north east Arabian Sea (Off Mumbai and Off Ratnagiri)&#xD;
where bathymetry is in the range of 20 m to 75 m. Wind velocity ranges between&#xD;
1.9 m/s to 10.2 m/s in these regions. The second potential site has been&#xD;
identified at off Mangalore with 6490 km&lt;sup&gt;2&lt;/sup&gt;. The third prospective&#xD;
site is at Off Hooghly estuary.&lt;/span&gt;
Page(s): 1401-1406</summary>
    <dc:date>2014-07-01T00:00:00Z</dc:date>
  </entry>
  <entry>
    <title>Repercussions of embarkation wharves in Lakshadweep Islands on coral communities and their ecology</title>
    <link rel="alternate" href="http://nopr.niscpr.res.in/handle/123456789/34459" />
    <author>
      <name>Ravindran, J.</name>
    </author>
    <author>
      <name>Manikandan, B.</name>
    </author>
    <author>
      <name>Venkatesh, M.</name>
    </author>
    <author>
      <name>Murali, R. Mani</name>
    </author>
    <author>
      <name>Marimuthu, N.</name>
    </author>
    <author>
      <name>Wafar, M.V.M.</name>
    </author>
    <id>http://nopr.niscpr.res.in/handle/123456789/34459</id>
    <updated>2016-07-20T06:31:30Z</updated>
    <published>2014-07-01T00:00:00Z</published>
    <summary type="text">Title: Repercussions of embarkation wharves in Lakshadweep Islands on coral communities and their ecology
Authors: Ravindran, J.; Manikandan, B.; Venkatesh, M.; Murali, R. Mani; Marimuthu, N.; Wafar, M.V.M.
Abstract: &lt;span style="font-size:9.0pt;font-family:" times="" new="" roman";="" mso-fareast-font-family:"times="" roman";mso-bidi-font-family:mangal;="" mso-ansi-language:en-in;mso-fareast-language:en-us;mso-bidi-language:hi"=""&gt;Present&#xD;
study infers that the construction of embarkation wharves in four of the&#xD;
Lakshadweep islands (Agatti, Amini, Kavaratti and Minicoy) in the last 5 years&#xD;
was accompanied by a marked degradation of coral community structure and coral&#xD;
biodiversity. Reduction in live coral percent cover was significant, from 31%&#xD;
to 4.69% in Agatti, 24% to 5.92% in Minicoy, 22% to 3.49% in Amini and 30.5% to&#xD;
4.4% in Kavaratti, with a simultaneous rise in the percent cover of other&#xD;
abiotic components. Species diversity of corals dominated by the massive&#xD;
reef-building corals was lost, affecting the structure and stability of the&#xD;
reef at these sites. Resilience potential of the reef became poor due to the&#xD;
monospecific colonization of corals belonging to very few genera like &lt;i style="mso-bidi-font-style:normal"&gt;Pocillopora &lt;/i&gt;and&lt;i style="mso-bidi-font-style:&#xD;
normal"&gt; Montipora.&lt;/i&gt; Reduction in coral cover and its diversity endangered&#xD;
the strength of the reef frame in the activity site and enhanced its&#xD;
vulnerability to the natural stress or calamities.&lt;/span&gt;
Page(s): 1391-1400</summary>
    <dc:date>2014-07-01T00:00:00Z</dc:date>
  </entry>
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