Browsing by Title
Now showing items 9008-9027 of 9167
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What Controls the Flushing Efficiency and Particle Transport Pathways in a Tropical Estuary? Cochin Estuary, Southwest Coast of India
(MDPI AG, 2020)Estuaries with poor flushing and longer residence time retain effluents and pollutants, ultimately resulting in eutrophication, a decline in biodiversity and, finally, deterioration of water quality. Cochin Estuary (CE), ... -
What do barnacle larvae feed on ? Implications in biofouling ecology
(Marine Biological Association of the United Kingdom, 2010)Barnacles are one of the dominant macrofouling organisms found in the intertidal region throughout the world. Among the different species of barnacles Balanus amphitrite (= Amphibalanus amphitrite) is a favoured candidate ... -
What drives nearshore sediment transport controls on the depletion of beach placers at Manavalakurichi, Southwest Coast of India?.
(Taylor and Francis, 2014)An in-depth analysis has been made to simulate hydrodynamic scenarios for understanding the nearshore sediment transport controls of placer mineral depletion at Manavalakurichi, India. From the analyses of topographic ... -
What drives the biological productivity of the northern Indian Ocean?
(American Geophysical Union, 2009)The northern Indian Ocean consists of two unique tropical basins: the Arabian Sea and the Bay of Bengal. The Arabian Sea is one of the most highly productive regions of the world ocean, while the Bay of Bengal is a basin ... -
What drives the increased phytoplankton biomass in the Arabian Sea?
(Current Science Association, 2010)The seasonal variability of phytoplankton biomass in the Arabian Sea, though a well researched topic, its inter-annual variability is less explored and understood. Analysis of the satellite-derived chlorophyll pigment ... -
Why do satellite imageries show exceptionally high chlorophyll in the Gulf of mannar and the Palk bay during the norteast monsoon?.
(Springer, 2014)The Gulf of Mannar (GoM) and the Palk Bay (PB) are two least studied marine environments located between India and Sri Lanka. Exceptionally high chlorophyll a concentration in the GoM and the PB during the Northeast Monsoon ... -
Why is Bay of Bengal warmer than Arabian Sea during the summer monsoon?
(School of Naval Oceanology and Meteorology, India, 2004)The near-surface Bay of Bengal remains significantly warmer than the Arabian Sea during summer monsoon (June-September). Analysis of the heat budgets of the near-surface Arabian Sea and Bay of Bengal shows significant ... -
Why is mean sea level along the Indian coast higher in the Bay of Bengal than in the Arabian Sea?
(Americal Geophysical Union, 2001)Levelling observations conducted during the Great Trigonometrical Survey of India (1858-1909) and subsequent observations showed that mean sea level along the coast of India is higher in the Bay of Bengal than in the Arabian ... -
Why is the Bay of Bengal experiencing a reduced rate of sea surface warming?
(Royal Meteorological Society, 2016)The sea surface temperature (SST) in the Bay of Bengal (BoB) during the period 1960–1995 showed a decadal cycle, riding over a warming trend. The disruption of the decadal cycle was noticed post-1995 and was followed by a ... -
Why is the Bay of Bengal less productive during summer monsoon compared to the Arabian Sea?
(American Geophysical Union, 2002)The Bay of Bengal is traditionally considered to be a less productive basin compared to the Arabian Sea. We explore the reasons for this in the central Bay during summer when both are subjected to strong monsoon forcing. ... -
Why the Gulf of Mannar is a marine biological paradise?
(Springer, 2021)The Gulf of Mannar (GoM), located between India and Sri Lanka, has astonishing faunal richness and diversity. Two oceanographic data sets supplemented with satellite remote sensing observations are discussed here to show ... -
Why were cool SST anomalies absent in the Bay of Bengal during the 1997 Indian Ocean Dipole event?
(American Geophysical Union, 2002)The most important center of atmospheric convection associated with the Indian summer monsoon is located in the Bay of Bengal. This tendency was enhanced during the 1997 Indian Ocean Dipole (IOD) event and cool SST anomalies ... -
Why were historical period ports of Goa located away from the coast? The decline of Gopakapatana
(CSIR-NISCAIR, 2014)Most of the ports of the historical period of the east and west coasts of India were located away from the seafront But in later period, new ports were established mostly along the coastal regions The reasons attributed ... -
Widespread fluorescence in terrestrial and marine samples investigated from India
(Elsevier, 2021)The discovery of green fluorescent protein (GFP) from jellyfish Aequorea victoria has provoked numerous studies to unveil the myriads of biomedical applications. Consequently, several studies also revealed the prevalence ... -
Widespread occurrence of methane seeps in deep-water regions of Krishna-Godavari basin, Bay of Bengal
(Elsevier Ltd, 2021)Drilling/coring activities during NGHP-Expeditions 01 and 02 discovered significant gas hydrate deposits in the Krishna-Godavari (KG) basin, a proven petroliferous basin located along the eastern continental margin of ... -
Will the aerosol derived from the OCM satellite sensor be representative of the aerosol over Goa?
(Indian Aerosol Science and Technology Association, 2007)Most of the ocean color satellite sensors such as IRS-P4 OCM, SeaWiFS and MODIS are sun synchronous and have pass over the regions during noon. From our measurements of aerosol optical properties using five-channel ... -
Wind fields of storms from surface isobars for wave hindcasting
(Allied, Chennai (India), 1996)Marine operations of various types are critically linked to mean and extreme wave statistics. In the Indian seas extreme wave conditions are caused by cyclones and steady strong monsoon winds. Wave data from cyclone areas ... -
Wind stress, curl and vertical velocity in the Bay of Bengal during southwest monsoon, 1984
(CSIR-NISCAIR, 1989)Wind distribution observed during southwest monsoon of 1984 has used to derive the mean wind stress for the season at every 1 degree square grid and curl over the Bay of Bengal. Two regions of maximum wind stress are present ... -
Wind waves - An introduction
(1989) -
Wind-driven coastal upwelling along the western boundary of the Bay of Bengal during the southwest monsoon
(Pergamon, 1991)A hydrographic survey during the southwest monsoon (July-August 1989) showed that along most of the western boundary of the Bay of Bengal, in an approximately 40 km wide band, isopycnals from depths up to about 70 m surfaced ...