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  <channel rdf:about="http://nopr.niscpr.res.in/handle/123456789/26348">
    <title>NOPR Collection: &lt;b&gt;Special Issue on Technologies for Ocean Exploration (Guest Editors: CVK Prasad Rao &amp; C. Revichandran)&lt;/b&gt;</title>
    <link>http://nopr.niscpr.res.in/handle/123456789/26348</link>
    <description>&lt;b&gt;Special Issue on Technologies for Ocean Exploration (Guest Editors: CVK Prasad Rao &amp; C. Revichandran)&lt;/b&gt;</description>
    <items>
      <rdf:Seq>
        <rdf:li rdf:resource="http://nopr.niscpr.res.in/handle/123456789/26431" />
        <rdf:li rdf:resource="http://nopr.niscpr.res.in/handle/123456789/26430" />
        <rdf:li rdf:resource="http://nopr.niscpr.res.in/handle/123456789/26429" />
        <rdf:li rdf:resource="http://nopr.niscpr.res.in/handle/123456789/26428" />
      </rdf:Seq>
    </items>
    <dc:date>2026-10-09T18:17:44Z</dc:date>
  </channel>
  <item rdf:about="http://nopr.niscpr.res.in/handle/123456789/26431">
    <title>Sources of errors in the measurements of underwater profiling radiometer</title>
    <link>http://nopr.niscpr.res.in/handle/123456789/26431</link>
    <description>Title: Sources of errors in the measurements of underwater profiling radiometer
Authors: Silveira, Noah; Suresh, T.; Talaulikar, Madhubala; Desa, Elgar; Matondkar, S.G. Prabhu; Lotlikar, Aneesh
Abstract: There are various sources of errors from&#xD;
the measurements of optical parameters using a radiometer, which can be classified&#xD;
as mode of deployment, instrument and environment. The errors from the&#xD;
deployment are primarily from the ship and superstructure shadows. Instrument&#xD;
could be a source of error arising from its self-shadow, drift in the calibration&#xD;
and temperature effects. There could be large errors, which at times may be&#xD;
unavoidable to environment factors such as wave focusing at the surface layers,&#xD;
sea state conditions which may affect the tilt of the instrument, atmospheric&#xD;
conditions such as cloud cover, solar elevation, wind and rain. Radiometric&#xD;
optical data in water could also get affected due to Raman scattering and&#xD;
fluorescence effects. Here we discuss the above sources of errors and how they could&#xD;
be minimized. From the measurements carried out in the coastal waters off Goa&#xD;
and Arabian Sea using the hypespectral radiometer,&#xD;
we propose simple protocol to measure the data and also screen the erroneous&#xD;
data measured from the radiometer.
Page(s): 88-95</description>
    <dc:date>2014-01-01T00:00:00Z</dc:date>
  </item>
  <item rdf:about="http://nopr.niscpr.res.in/handle/123456789/26430">
    <title>Real Time wave forecasting using artificial neural network with varying input parameter</title>
    <link>http://nopr.niscpr.res.in/handle/123456789/26430</link>
    <description>Title: Real Time wave forecasting using artificial neural network with varying input parameter
Authors: Vimala, J.; Latha, G.; Venkatesan, R.
Abstract: Prediction of significant wave heights&#xD;
(Hs) is of immense importance in ocean and coastal engineering applications. The&#xD;
aim of this study is to predict significant wave height values at buoy&#xD;
locations with the lead time of 3,6,12 and 24 hours using past observations of&#xD;
wind and wave parameters applying Artificial Neural Network. Although there&#xD;
exists a number of wave height estimation models, they do not consider all&#xD;
causative factors without any approximation and consequently their results are&#xD;
more or less a general approximation of the overall dynamic behaviour. Since&#xD;
soft computing techniques are totally data driven, based on the duration of the&#xD;
data availability they can be used for prediction. In the National data buoy&#xD;
program of National institute&#xD;
 of Ocean Technology, not&#xD;
all the buoys have wind sensors and wave sensors and so it is attempted to&#xD;
apply neural network algorithms for prediction of wave heights using wind speed&#xD;
only as the input and then using only wave height as the input. The measurement&#xD;
made by the data buoy at DS3 location in Bay of Bengal&#xD;
(12&lt;sup&gt;o&lt;/sup&gt;11’21"N and 90&lt;sup&gt;o&lt;/sup&gt;43’33"E) are considered, for&#xD;
the period 2003-2004. Out of this, the data of period Jan 2003-Dec 2003 was&#xD;
used for training and the data for the period July 2004- Nov 2004 is used for&#xD;
testing. Real time wave forecasting for 3,6,12 and 24 hours were carried out&#xD;
for a month at the location chosen and the results show that the ANN technique&#xD;
proves encouraging for wave forecasting. Performance of ANN for varying inputs&#xD;
have been analysed and the results are discussed.
Page(s): 82-87</description>
    <dc:date>2014-01-01T00:00:00Z</dc:date>
  </item>
  <item rdf:about="http://nopr.niscpr.res.in/handle/123456789/26429">
    <title>Prospects for developing a minor port facility at Betul, Goa</title>
    <link>http://nopr.niscpr.res.in/handle/123456789/26429</link>
    <description>Title: Prospects for developing a minor port facility at Betul, Goa
Authors: Mathai, Thomas; Kumar, Satish; Rajarama, K. N.; Kumar, P. Praveen; Chandran, M. Suresh
Abstract: Marine and Coastal Surveys Division of&#xD;
Geological Survey of India, initiated preliminary, integrated geological, geotechnical&#xD;
and geophysical surveys off Betul for making an appraisal of the developmental&#xD;
possibilities of setting up a minor port in this sector. Detailed surveys&#xD;
helped generate a bathymetric map of the area indicating a smooth and gently sloping&#xD;
seafloor without any hazards, ideal for port development. Sediment cores were&#xD;
studied to evaluate the sub-seabed sediment package and visualize the seabed&#xD;
sediment distribution. Mean size of the seabed surface sediments broadly&#xD;
signifies a sediment milieu encompassing variants from silt to clay, broadly&#xD;
classified as silty clay. Geotechnical analysis of the sediments helped to&#xD;
evaluate the engineering properties of the seabed and sub-seabed sediments&#xD;
quintessential for development of a port in this sector. Clayey sediments have&#xD;
a high degree of plasticity with a &lt;i&gt;very high swelling&lt;/i&gt; &lt;i&gt;potential. &lt;/i&gt;Shear&#xD;
resistance is almost unregistered at almost all levels of the sediment package.&#xD;
Geotechnical characteristics&#xD;
&#xD;
of the sediments are generally conducive&#xD;
for offshore structures. Side scan sonar surveys brought out a clear seafloor, generally&#xD;
monotonous and thus well suited for a navigational channel access. Current&#xD;
Observations carried out in the nearshore sector indicate low velocity currents&#xD;
and are not influenced by tidal variations. Environmental parameters including&#xD;
Temperature, &lt;i&gt;p&lt;/i&gt;H, Salinity, Conductivity and Dissolved Oxygen were&#xD;
studied to record the conditions prevalent in this sector, for post-development&#xD;
comparison.
Page(s): 76-81</description>
    <dc:date>2014-01-01T00:00:00Z</dc:date>
  </item>
  <item rdf:about="http://nopr.niscpr.res.in/handle/123456789/26428">
    <title>Oscillating environmental responses of the eastern Arabian Sea</title>
    <link>http://nopr.niscpr.res.in/handle/123456789/26428</link>
    <description>Title: Oscillating environmental responses of the eastern Arabian Sea
Authors: Gerson, Vijay John; Madhu, N V; Jyothibabu, R; Balachandran, K K; Nair, Maheswari; Revichandran, C
Abstract: Characteristics of two distinct physical&#xD;
processes, the coastal upwelling and convective overturning, which enhance&#xD;
phytoplankton productivity in the west coast of India, are discussed in this study.&#xD;
Systematic &lt;i&gt;in-situ &lt;/i&gt;data collected during the two contrasting monsoon&#xD;
(summer and winter) periods were utilized for the study. During summer monsoon,&#xD;
the colder (27°C), less oxygenated (&lt;190 μM), nitrate rich (NO&lt;sub&gt;3&lt;/sub&gt;-N&#xD;
&gt;2 μM) waters were evidenced in the upper layers of the southwest coast of&#xD;
India, along with higher level of primary production (surface - 76 mgC m&lt;sup&gt;-3&lt;/sup&gt;d&lt;sup&gt;-1&lt;/sup&gt;&#xD;
&amp; column -1629 mgC m&lt;sup&gt;-2&lt;/sup&gt;d&lt;sup&gt;-1&lt;/sup&gt;) and chlorophyll &lt;i&gt;a &lt;/i&gt;(surface&#xD;
- 1.2 mgm&lt;sup&gt;-3&lt;/sup&gt; &amp; column -45.7 mgm&lt;sup&gt;-2&lt;/sup&gt;). In contrast,&#xD;
during winter, the upper thermohaline layer of the northeastern Arabian Sea exhibited colder sea surface temperature&#xD;
(SST, 25-26°C), and deeper mixed layer depth (MLD, &gt;70 m). This area was&#xD;
distinguished by less oxygenated (&lt;180 μM), nitrate rich (&gt;2μM) and high&#xD;
productive (surface - &gt;10 mgC m&lt;sup&gt;-3&lt;/sup&gt;d&lt;sup&gt;-1&lt;/sup&gt; &amp; column -&#xD;
&gt;800 mgC m&lt;sup&gt;-2&lt;/sup&gt; d&lt;sup&gt;-1&lt;/sup&gt;) waters. I can be stated that the physically&#xD;
forced chemical changes occurred in the upper layers of both southeastern and&#xD;
northeastern Arabian Sea, appeared in an oscillating manner with respect to&#xD;
monsoonal changes, seemed to trigger the enhancement of phytoplankton productivity&#xD;
of the area.
Page(s): 67-75</description>
    <dc:date>2014-01-01T00:00:00Z</dc:date>
  </item>
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