94-102Variations in salinity, temperature, dissolved oxygen and zooplankton biomass in the backwaters from Cochin to Alleppey are discussed with reference to conditions prevailing respectively in premonsoon, monsoon and postmonsoon periods. Salinity in general decreases from the mouth of the estuary towards the head. The extent of intrusion of saline water depends on the strength of tidal influx and the fresh water efflux which differ with seasons. Higher temperature values observed in premonsoon fall with the advance of monsoon. High oxygen values recorded during monsoon suggest high primary production at surface during this season. Biomass values fluctuate with seasons and they can be correlated with the hydrographical conditions prevaili...
183-184Regression model for the prediction of zooplankton abundance correlating total numbers of zoo...
Qualitative and quantitative studies on phytoplankton of the Cochin Backwater showed that about 120 ...
154-159As a part of an ecological survey conducted during March 1981 (premonsoon period) at the Akat...
190-195Stratification in salinity and temperature values is prevalent during SW monsoon in the Cochi...
170-172Hydrological conditions of Cochin Backwaters are greatly influenced by seawater intrusion and...
In the Cochin Backwater the tides are of a mixed, semidiurnal type with a maximum range of about 1 m...
The nutrient distribution of the Cochin Backwater was studied at 6 stations throughout the year. The...
Although the extent of the influence of the widely fluctuating environmental factors on the abundan...
196-200Some hydrographic features of Cochin backwaters were studied from September 1974 to August 19...
In connection with the prawn studies of the Sub-station, routine observations on the surface salini...
Not AvailableNo information is available on siphonophores of the estuaries in India. The present inv...
182-186Distribution and biomass of zooplankton in relation to tides and seasons were studied in 2 st...
129-131Assuming temperature of the water layer at 50 m depth along the shore as an inverse index of ...
No information is available on siphonophores of the estuaries in India. The present investigation wa...
Variations in salinity, temperature, dissolved oxygen and zooplankton biomass in the shelf waters of...
183-184Regression model for the prediction of zooplankton abundance correlating total numbers of zoo...
Qualitative and quantitative studies on phytoplankton of the Cochin Backwater showed that about 120 ...
154-159As a part of an ecological survey conducted during March 1981 (premonsoon period) at the Akat...
190-195Stratification in salinity and temperature values is prevalent during SW monsoon in the Cochi...
170-172Hydrological conditions of Cochin Backwaters are greatly influenced by seawater intrusion and...
In the Cochin Backwater the tides are of a mixed, semidiurnal type with a maximum range of about 1 m...
The nutrient distribution of the Cochin Backwater was studied at 6 stations throughout the year. The...
Although the extent of the influence of the widely fluctuating environmental factors on the abundan...
196-200Some hydrographic features of Cochin backwaters were studied from September 1974 to August 19...
In connection with the prawn studies of the Sub-station, routine observations on the surface salini...
Not AvailableNo information is available on siphonophores of the estuaries in India. The present inv...
182-186Distribution and biomass of zooplankton in relation to tides and seasons were studied in 2 st...
129-131Assuming temperature of the water layer at 50 m depth along the shore as an inverse index of ...
No information is available on siphonophores of the estuaries in India. The present investigation wa...
Variations in salinity, temperature, dissolved oxygen and zooplankton biomass in the shelf waters of...
183-184Regression model for the prediction of zooplankton abundance correlating total numbers of zoo...
Qualitative and quantitative studies on phytoplankton of the Cochin Backwater showed that about 120 ...
154-159As a part of an ecological survey conducted during March 1981 (premonsoon period) at the Akat...