Now showing items 1-50 of 87

    • Assessing the geographical distribution of carnivorous and planktivorous fishes in the western Bay of Bengal 

      Vijith, V.; Anil, A.C.; Shankar, D.; Antony, S.P. (Elsevier, 2023)
      There is a clear distinction in the feeding habits of fishes between the northeastern and southeastern Arabian Sea (west coast of India) � the north is carnivorous, and the south is planktivorous �, but such a distinction ...
    • Seasonal cycle of zooplankton standing stock inferred from ADCP backscatter measurements in the eastern Arabian Sea 

      Aparna, S.G.; Desai, D.V.; Shankar, D.; Anil, A.C.; Dora, S.; Khedekar, R. (Elsevier, 2022)
      We use ADCP (acoustic Doppler current profiler) backscatter, measured during October 2012 to December 2020 at three locations on the continental slope in the eastern Arabian Sea (EAS), to study the seasonal variation in ...
    • Possible zonal asymmetry of the Indian summer monsoon rainfall after ~5 ka BP as revealed by palaeo-salinity in the eastern Arabian Sea 

      Banakar, V.K.; Baidya, S.; Shankar, D.; Nanjundiah, R.S.; Jain, V. (Springer, 2022)
      Data from a high-resolution sediment core off Goa in the eastern Arabian Sea (EAS) show that the Holocene surface-salinity variation off Goa contains four alternating high- and low-salinity events.These events are in ...
    • Variation of salinity in the Sundarbans estuarine system during the equinoctial spring tidal phase of march 2011 

      Chatterjee, Meenakshi; Shankar, D.; Vijith, V.; Sen, G.K.; Sundar, D.; Michael, G.S.; Amol, P.; Chatterjee, Abhisek; Sanyal, P.; Chatterjee, Siddhartha; Basu, Anwesha; Chakraborti, Saranya; Mishra, S.K.; Suprit, K.; Mukherjee, Debabrata; Mukherjee, A.; Mukhopadhyay, Soumya; Mondal, Gopal; Kalla, A.; Das, Madhumita (Springer, 2021)
      The Sundarbans Estuarine System (SES), comprising the southernmost part of the Indian portion of the Ganga-Brahmaputra delta bordering the Bay of Bengal, is India's largest monsoonal, macro-tidal, delta-front estuarine ...
    • Observed variability of the West India Coastal Current on the continental shelf from 2010-2017 

      Chaudhuri, Anya; Amol, P.; Shankar, D.; Mukhopadhyay, S.; Aparna, S.G.; Fernando, V.; Kankonkar, A. (Springer, 2021)
      We describe the variability of the West India Coastal Current (WICC) during 2009-2017 using data from acoustic Doppler current profilers (ADCPs) attached to moorings deployed on the outer shelf at a water-column depth of ...
    • Role of ocean dynamics in the evolution of mixed-layer temperature in the Bay of Bengal during the summer monsoon 

      Jain, V.; Shankar, D.; Vinayachandran, P.N.; Mukherjee, A.; Amol, P. (Elsevier, 2021)
      Earlier studies suggest that the mixed-layer (ML) temperature or sea surface temperature (SST) of the Bay of Bengal during the summer monsoon is determined primarily by air-sea fluxes. We use an oceanic general circulation ...
    • High-resolution Operational Ocean Forecast and reanalysis System for the Indian Ocean 

      Francis, P.A.; Jithin, A.K.; Effy, J.B.; Chatterjee, Abhisek; Chakraborty, Kunal; Paul, A.; Balaji, B.; Shenoi, S.S.C.; Biswamoy, P.; Mukherjee, Arnab; Singh, Prerna; Deepsankar, B.; Reddy, S.S.; Vinayachandran, P.N.; GirishKumar, M.S.; Bhaskar, T.V.S.U.; Ravichandran, M.; Unnikrishnan, A.S.; Shankar, D.; Amol, P.; Aparna, S.G.; Harikumar, R.; Kaviyazhaku, K.; Suprit, K.; Shesu, R.V.; KiranKumar, N.; Rao, N.S.; Annapurnaiah, K.; Venkatesan, R.; Rao, A.S.; Rajagopal, E.N.; Prasad, V.S.; Gupta, M.D.; Nair, T.M.B.; Rao, E.P.R.; Satyanarayana, B.V. (American Meteorological Society, 2020)
      A good understanding of the general circulation features of the oceans, particularly of the coastal waters, and ability to predict the key oceanographic parameters with good accuracy and sufficient lead time are necessary ...
    • Observed variability of the East India Coastal Current on the continental shelf during 2010-2018 

      Mukhopadhyay, S.; Shankar, D.; Aparna, S.G.; Fernando, V.; Kankonkar, A. (Springer, 2020)
      We describe the variability of the East India Coastal Current (EICC) during 2010-2018 on the outer continental shelf using data from four ADCP (acoustic Doppler current profilers) moorings deployed off Gopalpur (~ 19.5�N), ...
    • Observed variability of the West India Coastal Current on the continental slope from 2009-2018 

      Chaudhuri, A.; Shankar, D.; Aparna, S.G.; Amol, P.; Fernando, V.; Kankonkar, A.; Michael, G.S.; Satelkar, N.P.; Khalap, S.T.; Tari, A.P.; Gaonkar, M.G.; Ghatkar, S.; Khedekar, R.R. (2020)
      We describe the variability of the West India Coastal Current (WICC) during October 2008 to October 2018 using data from ADCP (acoustic Doppler current profiler) moorings deployed on the continental slope off the west coast ...
    • Maintenance of the southern Bay of Bengal cold pool 

      Vinayachandran, P.N.; Das, U.; Shankar, D.; Jahfer, S.; Behara, A.; Nair, T.M.B.; Bhat, G.S. (Elsevier, 2020)
      The region of relatively cooler water, sitting in the shadow zone of monsoon rainfall, around southern tip of India and around Sri Lanka, is known as the cold pool. A ship-board observations program to the east of Sri Lanka ...
    • Modulation of chlorophyll concentration by downwelling Rossby waves during the winter monsoon in the southeastern Arabian Sea 

      Amol, P.; Bemal, S.; Shankar, D.; Jain, V.; Thushara, V.; Vijith, V.; Vinayachandran, P.N. (Elsevier Ltd, 2020)
      Signatures of Rossby waves that are evident in satellite ocean colour data in the southeastern Arabian Sea (SEAS) are more prominent during the winter than the summer monsoon. During the winter, the sea level is high, and ...
    • Structure and dynamics of undercurrents in the western boundary current of the Bay of Bengal 

      Francis, P.A.; Jithin, A.K.; Chatterjee, Abhisek; Mukherjee, Arnab; Shankar, D.; Vinayachandran, P.N.; Ramakrishna, S.S.V.S. (Springer, 2020)
      The structure and variability of undercurrents in the East India Coastal Current (EICC), which is the western boundary current system in the Bay of Bengal (BoB), and the mechanisms of their formation are examined in this ...
    • Effect of freshwater advection and winds on the vertical structure of chlorophyll in the northern Bay of Bengal 

      Amol, P.; Vinayachandran, P.N.; Shankar, D.; Thushara, V.; Vijith, V.; Chatterjee, A.; Kankonkar, A. (Elsevier, 2020)
      The northern Bay of Bengal receives a large amount of fresh water through river runoff and rainfall during the Indian summer monsoon (June-September). This fresh water spreads offshore and can modulate the upper-ocean ...
    • Observed variability of the East India Coastal Current on the continental slope during 2009-2018 

      Mukhopadhyay, S.; Shankar, D.; Aparna, S.G.; Mukherjee, A.; Fernando, V.; Kankonkar, A.; Khalap, S.; Satelkar, N.P.; Gaonkar, M.G.; Tari, A.P.; Khedekar, R.R.; Ghatkar, S. (Springer, 2020)
      We describe the variability of the East India Coastal Current (EICC) during 2009-2018 using data from ADCP (acoustic Doppler current profiler) moorings deployed on the continental slope in the western Bay of Bengal. The ...
    • Seasonal variability of sea-surface temperature fronts associated with large marine ecosystems in the north Indian Ocean 

      Sarkar, K.; Aparna, S.G.; Dora, S.; Shankar, D. (Springer India, 2019)
      We use 14 years of satellite-derived sea-surface temperature (SST) data to compute a monthly frontal probability index (FPI) to determine the existence of a front in a pixel. A persistent SST front is deemed to exist if ...
    • Shallow convective mixing promotes massive Noctiluca scintillans bloom in the northeastern Arabian Sea 

      Sarma, V.V.S.S.; Patil, J.S.; Shankar, D.; Anil, A.C. (Elsevier, 2019)
      The northeastern Arabian Sea (NEAS) experiences convective mixing during winter, but this mixing does not reach up to the silicicline, resulting in the limited supply of silicate (Si) compared to nitrate (N) and phosphate ...
    • Influence of Rainfall Over Eastern Arabian Sea on Its Salinity 

      Behara, A.; Vinayachandran, P.N.; Shankar, D. (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 ...
    • Role of physical processes in determining the nature of fisheries in the eastern Arabian Sea 

      Shankar, D.; Remya, R.; Anil, A.C.; Vijith, V. (Elsevier, 2019)
      We use available data and model simulations to make a case for physical forcing of the spatial variation in the nature of fisheries off the west coast of India in the eastern Arabian Sea (EAS). The approach is heuristic, ...
    • Numerical simulation of the observed near-surface East India Coastal Current on the continental slope 

      Mukherjee, A.; Shankar, D.; Chatterjee, A.; Vinayachandran, P.N. (Springer Berlin Heidelberg, 2018)
      We simulate the East India Coastal Current (EICC) using two numerical models (resolution� 0.1-�0.1-),� an oceanic general circulation model (OGCM) called Modular Ocean Model and a simpler, linear, continuously stratified ...
    • Ecosystem response in temperature fronts in the northeastern Arabian Sea 

      Sarma, V.V.S.S.; Desai, D.V.; Patil, J.S.; Khandeparker, L.; Aparna, S.G.; Shankar, D.; DeSouza, S.; Dalabehera, H.B.; Mukherjee, J.; Sudharani, P.; Anil, A.C. (Elsevier, 2018)
      Productivity is low in tropical waters outside the traditional upwelling regimes, making temperature fronts a potential marker of fish. To test the hypothesis that all temperature fronts harbour high concentrations of ...
    • Picophytoplankton variability: Influence of winter convective mixing and advection in the northeastern Arabian Sea 

      Bemal, S.; Anil, A.C.; Shankar, D.; Remya, R.; Roy, R. (Elsevier, 2018)
      The deepening of mixed layer and ensuing changes in optical and physicochemical properties of euphotic zone can influence phytoplankton community dynamics in the northeastern Arabian Sea during winter monsoon. The response ...
    • Indian summer monsoon forcing on the deglacial polar cold reversals 

      Banakar, V.K.; Baidya, S.; Piotrowski, A.M.; Shankar, D. (Springer, 2017)
      The deglacial transition from the last glacial maximum at similar to 20 kiloyears before present (ka) to the Holocene (11.7 ka to Present) was interrupted by millennial-scale cold reversals, viz., Antarctic Cold Reversal ...
    • Dynamics of Andaman Sea circulation and its role in connecting the equatorial Indian Ocean to the Bay of Bengal 

      Chatterjee, A.; Shankar, D.; McCreary, J.P.; Vinayachandran, P.N.; Mukherjee, A. (Wiley, 2017)
      Circulation in the Bay of Bengal (BoB) is driven not only by local winds, but are also strongly forced by the reflection of equatorial Kelvin waves (EKWs) from the eastern boundary of the Indian Ocean. The equatorial ...
    • Observations of the sub-inertial, near-surface East India Coastal Current 

      Mukhopadhyay, S.; Shankar, D.; Aparna, S.G.; Mukherjee, A. (Elsevier, 2017)
      We present surface current measurements made using two pairs of HF (high-frequency) radars deployed on the east coast of India. The radar data, used in conjunction with data from acoustic Doppler current profiler (ADCP) ...
    • Evidence for the existence of Persian Gulf water and Red Sea water in the Bay of Bengal 

      Jain, V.; Shankar, D.; Vinayachandran, P.N.; Kankonkar, A.; Chatterjee, A.; Amol, P.; Almeida, A.M.; Michael, G.S.; Mukherjee, A.; Chatterjee, M.; Fernandes, R.; Luis, R.; Kamble, A.; Hegde, A.; Chatterjee, S.; Das, U.; Neema, C.P. (Springer, 2017)
      The high-salinity water masses that originate in the North Indian Ocean are Arabian Sea High-Salinity Water (ASHSW), Persian Gulf Water (PGW), and Red Sea Water (RSW). Among them, only ASHSW has been shown to exist in the ...
    • Inhibition of mixed-layer deepening during winter in the northeastern Arabian Sea by the West India coastal current 

      Shankar, D.; Remya, R.; Vinayachandran, P.N.; Chatterjee, Abhisek; Behera, A. (Springer, 2016)
      Though the deep mixed layers (MLs) that form in the northeastern Arabian Sea (NEAS) during the winter monsoon (November–February) have been attributed to convective mixing driven by dry, cool northeasterly winds from the ...
    • Consequences of inhibition of mixed-layer deepening by the West India coastal current for winter phytoplankton bloom in the northeastern Arabian Sea 

      Vijith, V.; Vinayachandran, P.N.; Thushara, V.; Amol, P.; Shankar, D.; Anil, A.C. (American Geophysical Union, 2016)
      The intense winter phytoplankton bloom during November-February in the northeastern Arabian Sea (NEAS) was thought, until recently, to be controlled only by a convective deepening of the mixed layer (ML) owing to cool and ...
    • Understanding our seas: National Institute of Oceanography, Goa 

      Naqvi, S.W.A.; Afzulpurkar, S.; Anil, A.C.; Chakraborty, P.; Dewangan, P.; Desai, D.V.; DeSouza, L.; Kessarkar, P.M.; Khandeparker, L.; Krishna, K.S.; Kurian, S.; Madhan, R.; Mascarenhas, A.A.M.Q.; Mazumdar, A.; Maurya, P.; Murty, V.S.N.; Nath, B.N.; Naik, H.; Navelkar, G.S.; PrasannaKumar, S.; Rao, V.P.; RameshKumar, M.R.; Ravichandran, C.; SanilKumar, V.; Saraswat, R.; Sarma, V.V.S.S.; Shankar, D.; Sharma, R.; Shenoy, D.M.; Suneel, V.; Thakur, N.L.; Unnikrishnan, A.S.; Vethamony, P.; Yatheesh, V. (Current Science Association, 2015)
      The present article summarizes the research done at the CSIR–National Institute of Oceanography in 2014 in ocean science, resources and technology. Significant research has been conducted on air–sea interactions and coastal ...
    • Evolution and sub-surface characteristics of a sea-surface temperature filament and front in the northeastern Arabian Sea during November–December 2012 

      Vipin, P.; Sarkar, K.; Aparna, S.G.; Shankar, D.; Sarma, V.V.S.S.; Gracias, D.G.; Krishna, M.S.; Srikanth, G.; Mandal, R.; RamaRao, E.P.; Rao, N.S. (Elsevier, 2015)
      We used satellite-derived sea-surface-temperature (SST) data along with in-situ data collected along a meridional transect between 18.85 and 20.25°N along 69.2°E to describe the evolution of an SST filament and front during ...
    • Observed intraseasonal and seasonal variability of the West India coastal current on the continental slope. 

      Amol, P.; Shankar, D.; Fernando, V.; Mukherjee, A.; Aparna, S.G.; Fernandes, R.; Michael, G.S.; Khalap, S.T.; Satelkar, N.P.; Agarvadekar, Y.; Gaonkar, M.G.; Tari, A.P.; Kankonkar, A.; Vernekar, S. (Indian Academy of Sciences, 2014)
      We present current data from acoustic Doppler current profilers (ADCPs) moored on the continental slope off the west coast of India. The data were collected at four locations (roughly at Kanyakumari, Kollam, Goa, and Mumbai) ...
    • Observed seasonal and intraseasonal variability of the East India Coastal Current on the continental slope. 

      Mukherjee, A.; Shankar, D.; Fernando, V.; Amol, P.; Aparna, S.G.; Fernandes, R.; Michael, G.S.; Khalap, S.T.; Satelkar, N.P.; Agarvadekar, Y.; Gaonkar, M.G.; Tari, A.P.; Kankonkar, A.; Vernekar, S. (Indian Academy of Sciences, 2014)
      We present data from three acoustic Doppler current profilers (ADCPs) moored off Cuddalore (12 Degree N), Kakinada (16.5 Degree N), and Gopalpur (19 Degree N) on the continental slope of the western Bay of Bengal and one ...
    • Near-inertial currents off the east coast of India 

      Mukherjee, A.; Shankar, D.; Aparna, S.G.; Amol, P.; Fernando, V.; Fernandes, R.; Khalap, S.T.; Satlekar, N.P.; Agarvadekar, Y.; Gaonkar, M.G.; Tari, A.P.; Kankonkar, A.; Vernekar, S. (Elsevier, 2013)
      We use data from moorings equipped with Acoustic Doppler Current Profilers (ADCPs) and deployed in the Bay of Bengal off the east coast of India from May 2009 to February 2012 to study the near-inertial currents (NICs) on ...
    • Tidal variations in the Sundarbans estuarine system, India 

      Chatterjee, M.; Shankar, D.; Sen, G.K.; Sanyal, P.; Sundar, D.; Michael, G.S.; Chatterjee, A.; Amol, P.; Mukherjee, D.; Suprit, K.; Mukherjee, A.; Vijith, V.; Chatterjee, S.; Basu, A.; Das, M.; Chakraborti, S.; Kalla, A.; Misra, S.K.; Mukhopadhyay, S.; Mandal, G.; Sarkar, K. (Indian Academy of Sciences, 2013)
      Situated in the eastern coastal state of West Bengal, the Sundarbans Estuarine System (SES) is India’s largest monsoonal, macro-tidal delta-front estuarine system. It comprises the southernmost part of the Indian portion ...
    • A summer monsoon pump to keep the Bay of Bengal salty 

      Vinayachandran, P.N.; Shankar, D.; Vernekar, S.; Sandeep, K.K.; Amol, P.; Neema, C.P.; Chatterjee, A. (American Geophysical Union, 2013)
      The Bay of Bengal receives a large influx of freshwater from precipitation and river discharge. Outflow of excess freshwater and inflow of saltier water is required to prevent the bay from freshening. Relatively fresh water ...
    • Yanai waves in the western equatorial Indian Ocean 

      Chatterjee, A.; Shankar, D.; McCreary, J.P.; Vinayachandran, P.N. (American Geophysical Union, 2013)
      Observations and models have shown the presence of intraseasonal fluctuations in 20-30-day and 10-20-day bands in the equatorial Indian Ocean west of 60 degrees E (WEIO). Their spatial and temporal structures characterize ...
    • Observational evidence from direct current measurements for propagation of remotely forced waves on the shelf off the west coast of India 

      Amol, P.; Shankar, D.; Aparna, S.G.; Shenoi, S.S.C.; Fernando, V.; Shetye, S.R.; Mukherjee, A.; Agarvadekar, Y.; Khalap, S.; Satelkar, N.P. (American Geophysical Union, 2012)
      We use data from six Acoustic Doppler Current Profiler (ADCP) moorings deployed during March–September 2008 on the continental shelf and slope off Bhatkal, Goa, and Jaigarh on the central west coast of India to present ...
    • Signatures of Indian Ocean dipole and El Nino-Southern Oscillation events in sea level variations in the Bay of Bengal 

      Aparna, S.G.; McCreary, J.P.; Shankar, D.; Vinayachandran, P.N. (American Geophysical Union, 2012)
      We investigate the impact of the Indian Ocean Dipole (IOD) and El Nino and the Southern Oscillation (ENSO) on sea level variations in the North Indian Ocean during 1957-2008. Using tide-gauge and altimeter data, we show ...
    • A new atlas of temperature and salinity for the North Indian Ocean 

      Chatterjee, A.; Shankar, D.; Shenoi, S.S.C.; Reddy, G.V.; Michael, G.S.; Ravichandran, M.; Gopalakrishna, V.V.; Rao, E.P.R.; UdayaBhaskar, T.V.S.; Sanjeevan, V.N. (Indian Academy of Sciences, 2012)
      The most used temperature and salinity climatology for the world ocean, including the Indian Ocean, is the World Ocean Atlas (WOA) because of the vast amount of data used in its preparation. The WOA climatology does not, ...
    • Simulating the daily discharge of the Mandovi River, west coast of India 

      Suprit, K.; Shankar, D.; Venugopal, V.; Bhatkar, N.V. (Taylor & Francis, 2012)
      A hydrological modelling framework was assembled to simulate the daily discharge of the Mandovi River on the Indian west coast. Approximately 90% of the west-coast rainfall, and therefore discharge, occurs during the summer ...
    • Factors controlling January–April rainfall over southern India and Sri Lanka 

      Vialard, J.; Terray, P.; Duvel, J.-P.; Nanjundiah, R.S.; Shenoi, S.S.C.; Shankar, D. (Springer, 2011)
      The factors controlling rainfall over southern India and Sri Lanka between January and April, i.e. outside of the southwest and northeast monsoons are explored. This period accounts for 20% of annual precipitation over Sri ...
    • Hydrological modelling of the west coast of India 

      Suprit, K. (Goa University, 2010)
      A hydrological modelling framework was assembled for simulating discharges of the west-coast rivers of India. The framework is applied to the Mandovi river, Goa, a typical west-coast river. The modelling framework consisted ...
    • Minima of interannual sea-level variability in the Indian Ocean 

      Shankar, D.; Aparna, S.G.; McCreary, J.P.; Suresh, I.; Neetu, S.; Durand, F.; Shenoi, S.S.C.; Al Saafani, M.A. (Elsevier, 2010)
      Wavelet analysis of altimeter sea level in the Indian Ocean shows regions of high variability (maxima) and low variability (minima) at all time scales. At interannual time scales, i.e., at periods of 17 months or more, ...
    • Biophysical processes in the Indian Ocean 

      McCreary, J.P.; Murtugudde, R.; Vialard, J.; Vinayachandran, P.N.; Wiggert, J.D.; Hood, R.R.; Shankar, D.; Shetye, S.R. (American Geophysical Union, 2009)
      Basic physical processes that impact biological activity in the Indian Ocean (IO), namely, near-surface processes (upwelling, entrainment, detrainment, and advection) and subsurface circulations (shallow overturning cells ...
    • Spatiotemporal structure of the East India Coastal Current from satellite altimetry 

      Durand, F.; Shankar, D.; Birol, F.; Shenoi, S.S.C. (American Geophysical Union, 2009)
      A newly processed altimeter data set to present a hitherto unprecedented description of the spatiotemporal structure of the East India Coastal Current (EICC) is used: the data set resolves timescales ranging from a few ...
    • Intraseasonal response of the northern Indian Ocean coastal waveguide to the Madden-Julian Oscillation 

      Vialard, J.; Shenoi, S.S.C.; McCreary, J.P.; Shankar, D.; Durand, F.; Fernando, V.; Shetye, S.R. (American Geophysical Union, 2009)
      A new observational record of upper-ocean currents at 15 degrees N on the western coast of India is dominated by intraseasonal (55-110 day) variations of alongshore currents, whereas sea level at the same location has a ...
    • Resolving orographic rainfall on the Indian west coast 

      Suprit, K.; Shankar, D. (Royal Meteorological Society, 2008)
      We discuss a method to obtain the spatial estimates of rainfall on the Indian west coast for calculating the surface water budget. The region includes the basin of the Mandovi River, a typical west-coast river whose catchment ...
    • Observational evidence for remote forcing of the west India coastal current 

      Shetye, S.R.; Suresh, I.; Shankar, D.; Sundar, D.; Jayakumar, S.; Mehra, P.; Desai, R.G.P.; Pednekar, P.S. (American Geophysical Union, 2008)
      Circulation in the north Indian Ocean is influenced by both local and remote wind forcing. So far, however, determining the contribution of these two forcing mechanisms at a location has been possible only in numerical ...
    • Estimating boundary currents from satellite altimetry: A case study for the east coast of India 

      Durand, F.; Shankar, D.; Birol, F.; Shenoi, S.S.C. (The Oceanographic Society of Japan, 2008)
      A methodology to derive surface geostrophic current from a newly released altimetric sea-level data set is presented. TOPEX/Poseidon data were first completely reprocessed from Geophysical Data Records using new algorithms ...
    • Are sea-level-rise trends along the coasts of the north Indian Ocean consistent with global estimates? 

      Unnikrishnan, A.S.; Shankar, D. (Elsevier, 2007)
      Mean-sea-level data from coastal tide gauges in the north Indian Ocean wereare used to show that low-frequency variability is consistent among the stations in the basin. Statistically significant trends obtained from records ...
    • Vertical propagation of baroclinic Kelvin waves along the west coast of India 

      Nethery, D.; Shankar, D. (Indian Academy of Sciences, 2007)
      A linear, continuously stratified ocean model is used to investigate vertical propagation of remotely forced, baroclinic Kelvin waves along the Indian west coast. The extent of vertical propagation over the length of the ...