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dc.contributor.authorJoseph, A.
dc.contributor.authorMehra, P.
dc.contributor.authorDesai, R.G.P.
dc.contributor.authorSivadas, T.K.
dc.contributor.authorBalachandran, K.K.
dc.contributor.authorVijaykumar, K.
dc.contributor.authorRevichandran, C.
dc.contributor.authorAgarvadekar, Y.
dc.contributor.authorFrancis, R.
dc.contributor.authorMartin, G.D.
dc.date.accessioned2008-05-01T11:58:38Z
dc.date.available2008-05-01T11:58:38Z
dc.date.issued2008
dc.identifier.citationOceans'08 MTS/IEEE Kobe-Techno-Ocean'08, April 9-11, 2008, Kobe, Japan, 9 pp.
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/1069
dc.description.abstractThermohaline structure of Kochi backwaters (KB) in India and its sensitivity to meteorological disturbances has been identified through measurements of temperature, salinity, and surface meteorological parameters. Silicon p-n junction semiconductor sensors have been used for measurements of subsurface temperature. Linearity and accuracy based on laboratory calibration of the sensors are found to be better than 0.4% and -0.8% respectively beyond 20 degrees C. Induction type conductivity cell was used for salinity measurement. Linearity and accuracy of salinity measurements are found to be better than plus or minus 3% and plus or minus 5% respectively beyond 20 psu. In-situ measurements show that the thermohaline structure of KB exhibits fortnightly spring-neap variability in which thermal and haline variability bear an inverse relationship, with cooling and enhanced salinity during spring tide and vice versa during neap tide. The diurnal variability in temperature is controlled by day/night cyclicity rather than tidal, whereas this feature is absent in haline variability. Horizontal thermohaline structure of the KB is inhomogeneous, where the upstream boundary region is warmer and less saline than the mouth region. Changes in the meteorology disturb the thermohaline structure of KB. Rainfall and associated river influx cause large haline stratification in the mouth region, in which a approx. 1-4 m thick layer of low salinity water (approx. 0-2 psu) floats on the surface.
dc.language.isoen
dc.publisherIEEE
dc.rightsCopyright [2008]. It is tried to respect the rights of the copyright holders to the best of the knowledge. If it is brought to our notice by copyright holder that the rights are voilated then the item would be withdrawn.
dc.titleIdentification of thermohaline structure of a tropical estuary and its sensitivity to meteorological disturbance through temperature, salinity, and surface meteorological measurements
dc.typeConference Article


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