Search
Now showing items 41-50 of 221
Westward movement of eddies into the Gulf of Aden from the Arabian Sea
(American Geophysical Union, 2007)
Sea level anomalies (SLA) from satellite altimetry (1993-2003) reveal the westward movement of mesoscale eddies in the Gulf of Aden. Inside the gulf the eddies move at a speed of approx. 6.0-8.5 cm s sup(-1), comparable ...
On the dynamics of the Lakshadweep high and low in the southeastern Arabian Sea
(American Geophysical Union, 1997)
Hydrography and altimetry show that a "high" in surface topography forms off southwest India in January (midnortheast monsoon) and that a "low" forms during the southwest monsoon; the high and low, called Lakshadweep high ...
Coupling between suboxic condition in sediments of the western Bay of Bengal and southwest monsoon intensification: A geochemical study
(Elsevier, 2013)
Reconstruction of paleo-redox conditions in a radiocarbon (14C) dated sediment core (SK-218/1), covering the past 45 ka (thousand calendar years), collected from the western Bay of Bengal (Lat: 14 degrees 02′N; Long: 82 ...
Distribution and air–sea exchange of nitrous oxide in the coastal Bay of Bengal during peak discharge period (southwest monsoon)
(Elsevier, 2013)
In order to examine the impact of river discharge from the Indian subcontinent on the concentration and air–sea exchange of nitrous oxide (N sub(2)O) a study was conducted during peak discharge period in the coastal Bay ...
Particulate organic carbon and particulate humic material in the Arabian Sea
(Council of Scientific and Industrial Research, New Delhi, 1999)
Variations in particulate organic carbon (POC) and particulate humic material (PHM) were studied in winter (February-March 1995) and intermonsoon (April-May 1994) seasons in the Arabian Sea. Higher levels of POC were found ...
A semi-diagnostic calculation of climatic circulation in the western Indian Ocean
(NISCAIR, CSIR, 1997)
A 3-dimensional, semi-diagnostic circulation model is used to compute the climatic circulation in the upper levels of western tropical Indian Ocean (20 degrees S-30 degrees N and 35 degrees E-80 degrees E) during the ...
T-S variability and volume transport in the central Bay of Bengal during southwest monsoon
(NISCAIR, CSIR, 1996)
The variability of temperature and salinity along 11 degrees N and 12 degrees N sections in the Bay of Bengal during southwest monsoon months (July-September) was found to be large in the upper 200 m west of 83 degrees E ...
Monsoon induced cobalt enrichment in Porites (coral) from the Arabian Sea
(NISCAIR, CSIR, 1998)
Cobalt concentrations in growth bands of a reef building coral (Porites sp.) collected from Kalpeni Atoll of the Lakshadweep group of islands (Arabian Sea), rvealed that cobalt concentrations and Co/Ca ratios exhibit similar ...
Annual and interannual variation of precipitation over the tropical Indian Ocean
(American Geophysical Union, 1997)
The annual and interannual variability of precipitation over the tropical Indian Ocean is studied for the period June 1986 to December 1990 using the data retrieved from the Indian National Satellite (INSAT). The seasonal ...
On the possible causes of the seasonal phytoplankton blooms along the southwest coast of India
(NISCAIR, CSIR, 1996)
Data collected off the southwest coast of India at the onset of the 1987 southwest monsoon season suggest that the commonly observed high concentrations of chlorophyll and rates of photosynthesis of the season may not be ...