Browsing by Title
Now showing items 4182-4201 of 9145
-
Influence of hypoxia on phosphorus cycling in Alappuzha mud banks, southwest coast of India
(2020)The southwest coast of India is known to experience two concurrent processes during the southwest monsoon, namely coastal upwelling and mud banks at selected stretches such as that off Alappuzha. The mud bank sediments ... -
Influence of Indian summer monsoon variability on the surface waves in the coastal regions of eastern Arabian Sea
(Copernicus, 2016)We assess the influence of monsoon variability on the surface waves using measured wave data covering 7 years and reanalysis data from 1979 to 2015 during the Indian summer monsoon (JJAS) in the eastern Arabian Sea. The ... -
Influence of low-temperature fluids and post-depositional changes in the siliceous-pelagic sediments of the Central Indian Ocean Basin
(Springer, 2021)In this paper, we discuss the possible reasons for the mass disappearance of radiolarians, hiatus in sedimentation, low-temperature alteration of sediments, and formation of palagonite and phillipsites in the Central Indian ... -
Influence of marginal highs on the accumulation of organic carbon along the continental slope off western India
(Pergamon, 2000)Twenty five surficial sediment samples were collected from the central western continental margin of India, which consists of diverse physiographic entities, continental slope, shelf margin basin, marginal high, and the ... -
Influence of monsoon upwelling on the planktonic foraminifera off Oman during Late Quaternary
(NISCAIR, CSIR, 2007)Planktonic foraminifer abundances, fluxes, test sizes, and coiling properties are influenced in various ways by the southwest monsoon winds and associated upwelling in the western Arabian Sea. The influence of monsoon ... -
Influence of morphodynamic variability over seasonal beach sediments and its probable effect on coastal development
(Elsevier, 2011)Seasonal variations and effect of oceanographic processes such as erosion and/or accretion along beaches are important to understand their impact on coastal morphological variations. Detailed investigations were taken up ... -
Influence of natural and anthropogenic factors on the water quality of the coastal waters around the South Andaman in the Bay of Bengal
(Springer, 2015)During the last decade, the Andaman and Nicobar Islands (ANI) have witnessed a marginal population growth with associated variations and degradation in the water quality of the inhabited coastal region. Monthly water quality ... -
Influence of net ecosystem metabolism in transferring riverine organic carbon to atmospheric CO2 in a tropical coastal lagoon (Chilka Lake, India)
(Springer, 2008)Studies on biogeochemical cycling of carbon in the Chilka Lake, Asia’s largest brackish lagoon on the east coast of India, revealed, for the first time, strong seasonal and spatial variability associated with salinity ... -
Influence of northeasterly trade winds on intensity of winter bloom in the northern Arabian Sea
(Indian Academy of Sciences, 2006)Chlorophyll and wind pattern retrieved from remote sensing data have been used to study biological activity in the oceanic waters of Northern Arabian Sea (NAS) during February–March 2002–05. Occurrence of algal bloom in ... -
Influence of oil and gas exploration activities on the macrobenthic community structure of the Krishna-Godavari basin (Ravva coast), Western Bay of Bengal
(Pergamon, 2021)The influence of oil and gas exploration activities on the macrobenthic community of an offshore oil and gas drilling site was investigated along the Krishna-Godavari basin (KG), Western Bay of Bengal. In the oil well ... -
Influence of orographically enhanced SW monsoon flux on coastal processes along the SE Arabian Sea
(American Geophysical Union, 2011)The Arabian Sea has an excess evaporation over precipitation regime. The southeast Arabian Sea is, however, anomalous because it has ~2800–4800 mm rainfall during the southwest monsoon (SWM). Despite a high rainfall, the ... -
Influence of particulate matter on microfouling biomass in the Arabian Sea
(Harwood Academic Publishers GmbH, 1990) -
Influence of physical and biological processes on the seasonal cycle of biogenic flux in the equatorial Indian Ocean
(European Geosciences Union, 2013)Seasonal cycle of biogenic fluxes obtained from sediment trap at two locations 5°24` N, 86°46` E (southern Bay of Bengal trap; SBBT) and 3°34` N, 77°46` E (equatorial Indian Ocean trap; EIOT) within the equatorial Indian ... -
Influence of physical processes and freshwater discharge on the seasonality of phytoplankton regime in the Bay of Bengal
(Pergamon, 2000)The seasonality of phytoplankton was examined in the western and northern Bay of Bengal using shipboard data collected during three seasons as well as ocean colour imagery from OCTS and Sea WiFS. Seasonal changes in the ... -
Influence of phytoplankton pigment composition and primary production on pCO2 levels in the Indian Ocean
(Springer, 2021)The tropical Indian Ocean is a net sink for the carbon dioxide (CO2) in the atmosphere and phytoplankton production plays a crucial role in CO2 fixation and determines the direction of CO2 flux at the sea-to-air interface. ... -
Influence of pollution of boron chlorinity ratio
(Society of Biosciences, Muzaffarnagar, India, 1992)Presence of boron in domestic wastewater has resulted in high B/CI ratio at some locations in the coastal water around Bombay. A widest range (0.215-0.281) of B/CI was observed at a location with high influence of wastewater ... -
Influence of Rainfall Over Eastern Arabian Sea on Its Salinity
(2019)The west coast of India and the adjoining eastern Arabian Sea (EAS) is one of the high rainfall zones of Indian summer monsoon. The summer monsoon rainfall in this region is about 1,036 km3, which is comparable to the ... -
Influence of regional and local topography on the distribution of polymetallic nodules in Central Indian Ocean Basin
(Springer, 1988)Detailed bathymetric surveys from part of the Central Indian Ocean revealed several bathymetric features such as hills, slopes, valleys, and plains. Areas with a local relief of a few to hundreds of meters generally have ...