Search
Now showing items 1-10 of 20
Hydrography of the Wadge bank - premonsoon and monsoon seasons
(Indian Association for Limnology and Oceanography, 1989)
The hydrography of the Wadge Bank during premonsoon and monsoon seasons is presented. The thermocline slopes downward towards the central region. Upwelling is prominent in the entire region during monsoon and is observed ...
Seasonal variation of the salinity in the Zuari estuary, Goa
(Indian Academy of Sciences, Bangalore, 1987)
The annual salt budget of the Zuari is examined. The characteristics of the estuary differ markedly from the low run off season during November - May to the heavy run off period of the southwest monsoon from June to October. ...
Watermass structure and current system in the equatorial western Indian Ocean during August, 1985
(Hamburg : Das Institut, 1987)
During the 17th cruise of ORV Sagar Kanya (3rd to 21st August, 1985), two meridional sections were occupied between 4 degrees N and 6 degrees n S in the equatorial Western Indian Ocean. The Dynamic Method was employed to ...
Watermass structure in the Bay of Bengal
(Indian Association for Limnology and Oceanography, 1985)
The distributions of temperature, salinity thermosteric anomaly, density flux function and stability along 88 degrees E in the Bay of Bengal are presented. The surface salinities showed strong gradients both horizontally ...
Water characteristics and transport of the Antarctic circumpolar current in the Indian Ocean
(Indian Academy of Sciences, Bangalore, 1988)
Geostrophic velocities are computed across meridians 37 degrees E and 105 degrees E using hydrographic data. The estimated mass transport is represented on a temperature - salinity diagram. The characteristics of the water ...
Proloculus size variation in Recent benthic foraminifera: Implications for paleoclimatic studies
(Elsevier, 1987)
Ratios of dimorphic (microspheric/megalospheric) forms of Foraminifera are affected by temperature and hence are useful in paleoclimatic studies. In some cases, however, it is not possible to distinguish between the dimorphic ...
Watermass structure in the western Indian Ocean: Part 1. Watermasses and their thermohaline indices
(India Meteorological Department, 1986)
The concept of "Indian Ocean Common Watermass" is introduced and its characteristics are defined. The temperature-salinity structures which would result when one, two or more watermasses of different temperature and salinity ...
Reproductive behaviour of benthic foraminifera: A key to palaeoclimate
(Indian Academy of Sciences, Bangalore, 1988)
Many benthic foraminiferal species exhibit dimorphism associated with reproduction. The two resultant forms are known as microspheric and megalospheric forms. Culture studies, though limited in number, show that ratios of ...
Gyres in the NW Bay of Bengal - Some observed evidences
(CSIR-NISCAIR, 1987)
Continuous observations of temperature, salinity and the flow at 4 stations off the rivers of Krishna, Godavari, Mahanadi and off New Moore Island, along the east coast of India, were made prior to the onset of the SW ...
Watermass structure in the western Indian Ocean - Part 2. The spreading and transformation of the Persian Gulf water
(India Meteorological Department, 1986)
The spreading and the transformation of the Persian Gulf Watermass (PGW) in the Arabian Sea and the Indian Ocean have been presented. The core layer of this watermass is found in the depth range of 250-300 m over most of ...