Now showing items 1-10 of 18
Variability of frontal structure in the south Indian/Antarctic Ocean: Possible reason for longitudinal differences in the intensity of the oxygen maximum
(Goa: National Inst of Oceanography, 1987)
On the renewal of the denitrifying layer in the Arabian Sea
A one-dimensional (vertical) advection-diffusion model has been applied to the deep layer characterized by a linear potential temperature(theta)-salinity relationship in the Arabian Sea to estimate the velocity of ascending ...
Marine nitrogen cycling- Some recent observations in the northwestern Indian Ocean
(Trivandrum: University of Kerala, 1987)
Published estimates of the rate of denitrification in the Arabian Sea have been evaluated and some new data on the nitrogen cycle have been presented Secondary nitrite maxima and nitrate reduction appear to be associated ...
Some oceanographic observations in the polynya and along a section in the southwest Indian/ Antarctic Ocean
Hydrographical and hydrochemical observations have been made at a shelf station off Princess Astrid Coast, Dronning Maud Land, Antarctica, and at 11 other stations along a transect from Antarctica to about 30~'S latitude. ...
Some aspects of the oxygen-deficient conditions and denitrification in the Arabian Sea
(Ingenta Connect Publication, 1987)
Utilizing a fairly large amount of recently collected data, some outstanding questions concerning the Arabian Sea denitrification problem are addressed. The true level of dissolved oxygen, determined colorimetrically, are ...
Nutrient uptake and regeneration ratios in the Red sea with reference to the nutrient budgets
The relationships between apparent oxygen utilization and inorganic micronutrients have been studied on the basis of extensive observation in the Red Sea. The ratios obtained are - Delta AOU: Delta SiO4: Delta NO3: Delta ...
Deep and bottom water characteristics in the Owen Fracture Zone, Western Arabian Sea
Hydro chemical studies at a station (10 degrees 34.l'N,56 degrees 31,7'E) in the Owen Fracture zone reveal an active movement of bottom water as approx 75 m thick, cold, low-salinity layer. Silicate profile exhibits a broad ...