The knowledge of the water currents in the locality being essential for understanding the causes of forma tion, maintenance, movement and dissipation of mudbanks, the current system over two tidal cycles, one in May, before the formation, and the other in August, toward the end of the mudbank period, in 1975, at Alleppey mudbank was studied. Marked difference in the direction and velocity of the current was noticed between the two occasions. In May the effect of the tides was not noticeable on the direction of the current, which was southerly, whereas in August, though the major current con tinued to be southerly, the speed was considerably reduced due to tidal influence. Introducing thereb...
I. Hydrodynamics and Suspended sediment As part of an interdisciplinary experiment, a series of...
As a component of an investigation into biofouling problems near the Norfolk Naval Shipyard, a field...
THE MUDBANKS, the formation of which is a curious phenomenon reported hitherto from only the...
Not AvailableThe knowledge of the water currents in the locality being essential for understand...
The variations in physical and chemical parameters of the Alleppey mudbank waters are discu...
The standing crop of phytcplankton, in terms of biomass, chloropliyll a and total ceils, record...
Most of the natural processes are common to all coastlines and their physico-chemical characteristi...
Mud banks are unique, clearly demarked naturally occurring calm areas which occur mainly in the ins...
The formation of mud banks is a uaique phenomenon occurring only at defenite locaiities between C...
The natural format ion of mudbanks (Chagaras) at certain locations along the Kera'a coast during Th...
The mud banks and coastal erosion are two contrasting phenomena that occur along the west coast of I...
In 1993 an interdisciplinary research programme on the behaviour of mud in tidal waters was initiate...
We have documented reports of the mudbanks along the south-west coast between Mangalore and...
Currents on either side of Well Bank were recorded for 41 days in May–June 1981, in order to disting...
Tidal dynamics including water level variation and movement describe the characteristics of a coasta...
I. Hydrodynamics and Suspended sediment As part of an interdisciplinary experiment, a series of...
As a component of an investigation into biofouling problems near the Norfolk Naval Shipyard, a field...
THE MUDBANKS, the formation of which is a curious phenomenon reported hitherto from only the...
Not AvailableThe knowledge of the water currents in the locality being essential for understand...
The variations in physical and chemical parameters of the Alleppey mudbank waters are discu...
The standing crop of phytcplankton, in terms of biomass, chloropliyll a and total ceils, record...
Most of the natural processes are common to all coastlines and their physico-chemical characteristi...
Mud banks are unique, clearly demarked naturally occurring calm areas which occur mainly in the ins...
The formation of mud banks is a uaique phenomenon occurring only at defenite locaiities between C...
The natural format ion of mudbanks (Chagaras) at certain locations along the Kera'a coast during Th...
The mud banks and coastal erosion are two contrasting phenomena that occur along the west coast of I...
In 1993 an interdisciplinary research programme on the behaviour of mud in tidal waters was initiate...
We have documented reports of the mudbanks along the south-west coast between Mangalore and...
Currents on either side of Well Bank were recorded for 41 days in May–June 1981, in order to disting...
Tidal dynamics including water level variation and movement describe the characteristics of a coasta...
I. Hydrodynamics and Suspended sediment As part of an interdisciplinary experiment, a series of...
As a component of an investigation into biofouling problems near the Norfolk Naval Shipyard, a field...
THE MUDBANKS, the formation of which is a curious phenomenon reported hitherto from only the...