Chiranjivi Jayaram,Ch V; Dr. Balchand, A N(Cochin University of Science & Technology, May , 2011)
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Abstract:
In this thesis, a variety of available satellite data products have been made use of
to bring out a synergistic analysis on the upwelling phenomenon in SEAS. Basic
concepts of remote sensing, upwelling and linked oceanography topics have been
dealt in this work .Auxiliary data products utilized in this study are described
in chapter 2. The climatological monthly variability of the upwelling signatures
are detailed under chapter 3. Chapter 4 presents the forcing factors that trigger
the upwelling process in SEAS. Chapter 5 describes the oceanic response to the
forcing factors with respect to the SST cooling and CHLA blooms. Chapter 6
presents the heat budget of the region and the variability of heat budget terms
with respect to upwelling. Chapter 7 describes the inter-annual variability of
upwelling intensity in SEAS and the influence of climatic events on upwelling.
Dipson, P T; Dr.Harindranathan Nair, M V(Cochin University Of Science And Technology, November , 2012)
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Abstract:
Urban developments have exerted immense pressure on wetlands.
Urban areas are normally centers of commercial activity and continue to attract
migrants in large numbers in search of employment from different areas. As a
result, habitations keep coming up in the natural areas / flood plains. This is
happening in various Indian cities and towns and large habitations are coming
up in low-lying areas, often encroaching even over drainage channels. In
some cases, houses are constructed even on top of nallahs and drains.
In the case of Kochi the situation is even worse as the base of the
urban development itself stands on a completely reclaimed island. Also the
topography and geology demanded more reclamation of land when the city
developed as an agglomerative cluster. Cochin is a coastal settlement
interspersed with a large backwater system and fringed on the eastern side by
laterite-capped low hills from which a number of streams drain into the
backwater system. The ridge line of the eastern low hills provides a welldefined
watershed delimiting Cochin basin which help to confine the
environmental parameters within a physical limit. This leads to an obvious
conclusion that if physiography alone is considered, the western flatland is
ideal for urban development. However it will result in serious environmental
deterioration, as it comprises mainly of wetland and for availability of land there
has to be large scale filling up of these wetlands which includes shallow
mangrove-fringed water sheets, paddy fields, Pokkali fields, estuary etc.Chapter 1
School 4 of Environmental Studies
The urban boundaries of Cochin are expanding fast with a consequent
over-stretching of the existing fabric of basic amenities and services.
Urbanisation leads to the transformation of agricultural land into built-up areas
with the concomitant problems regarding water supply, drainage, garbage and
sewage disposal etc. Many of the environmental problems of Cochin are
hydrologic in origin; like water-logging / floods, sedimentation and pollution in
the water bodies as well as shoreline erosion
Description:
School of Environmental Studies
Cochin University of Science and Technology
Annes, V H; Dr.Mohan Kumar, K(Cochin University of Science & Technology, June , 2000)
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Abstract:
The aim of the
present study is to understand the characteristics and properties of different wave
modes and the vertical circulation pattern in the troposphere and lower stratosphere
over Indian region using data obtained from the Indian Mesosphere-Stratosphere Troposphere
(MST) radar, National Center for Environmental Prediction/National
Centres of Atmospheric Research (NCEP/NCAR) reanalysed data and radiosonde observations.Studies on the vertical motion in monsoon Hadley circulation are carried out
and the results are discussed . From the analysis of MST radar data, an
overall picture of vertical motion of air over Indian region is explained and noted that
there exists sinking motion both during winter and summer. Besides, the study shows
that there is an anomalous northerly wind in the troposphere over the southern
peninsular region during southwest monsoon season.The outcome of the study on intrusion of mid-latitude upper tropospheric
trough and associated synoptic-scale vertical velocity over the tropical Indian
latitudes are reported and discussed . It shows that there is interaction
between north Indian latitudes and tropical easterly region, when there is an eastward
movement of Western Disturbance across the country. It explains the strengthening of
westerlies and a change of winter westerlies into easterlies in the tropical troposphere
and lower stratosphere. The divergence field computed over the MST radar station
shows intensification in the downward motion in association with the synoptic
systems of the northwest Indian region.
Description:
Department of Atmospheric Sciences,
Cochin University of Science and Technology