Zobrazeno 1 - 10
of 91
pro vyhledávání: '"P. N. Vinayachandran"'
Autor:
J. Giddings, K. J. Heywood, A. J. Matthews, M. M. Joshi, B. G. M. Webber, A. Sanchez-Franks, B. A. King, P. N. Vinayachandran
Publikováno v:
Ocean Science, Vol 17, Pp 871-890 (2021)
Chlorophyll has long been known to influence air–sea gas exchange and CO2 drawdown. But chlorophyll also influences regional climate through its effect on solar radiation absorption and thus sea surface temperature (SST). In the Bay of Bengal, the
Externí odkaz:
https://doaj.org/article/ea76bfedc06b4b8abbdc9d563a61c86f
Publikováno v:
Frontiers in Marine Science, Vol 9 (2022)
The Irrawaddy (IR) is the largest river discharging into the Andaman Sea and plays an important role in the salinity distribution and the mixed layer physics of the Andaman Sea. This study presents the first report of the IR plume pathways in the And
Externí odkaz:
https://doaj.org/article/50d94ff99c294a98b29e06f9cfcb6f4f
Autor:
Fraser Davidson, Aida Alvera-Azcárate, Alexander Barth, Gary B. Brassington, Eric P. Chassignet, Emanuela Clementi, Pierre De Mey-Frémaux, Prasanth Divakaran, Christopher Harris, Fabrice Hernandez, Patrick Hogan, Lars R. Hole, Jason Holt, Guimei Liu, Youyu Lu, Pablo Lorente, Jan Maksymczuk, Matthew Martin, Avichal Mehra, Arne Melsom, Huier Mo, Andrew Moore, Paolo Oddo, Ananda Pascual, Anne-Christine Pequignet, Villy Kourafalou, Andrew Ryan, John Siddorn, Gregory Smith, Deanna Spindler, Todd Spindler, Emil V. Stanev, Joanna Staneva, Andrea Storto, Clemente Tanajura, P. N. Vinayachandran, Liying Wan, Hui Wang, Yu Zhang, Xueming Zhu, Ziqing Zu
Publikováno v:
Frontiers in Marine Science, Vol 6 (2019)
Operational oceanography can be described as the provision of routine oceanographic information needed for decision-making purposes. It is dependent upon sustained research and development through the end-to-end framework of an operational service, f
Externí odkaz:
https://doaj.org/article/59d80a964ea548c0985f34a86da8b84d
Publikováno v:
Limnology and Oceanography. 67:1416-1428
Autor:
Aditya Kottapalli, P N Vinayachandran
The northward propagating intraseasonal Oscillation (ISO) is one of the dominant modes of tropical variability during Boreal summers. Several mechanisms have been proposed to explain northward propagation. Yet the factors that decide the ISO rainfall
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a2f993f36fc34569491e49007b648108
https://doi.org/10.21203/rs.3.rs-2415890/v1
https://doi.org/10.21203/rs.3.rs-2415890/v1
Publikováno v:
Environmental Research Letters, Vol 15, Iss 5, p 054013 (2020)
Climate model projections for the 21st century predict an elongated dry season in the Amazon basin, potentially reducing the discharge into the equatorial Atlantic Ocean. In order to understand the climatic role of Amazon runoff into the ocean, sensi
Externí odkaz:
https://doaj.org/article/f02d5a7cc55e403f896fdf63a1288616
Publikováno v:
Journal of Physical Oceanography. 51:505-518
The inflow of high-saline water from the Arabian Sea (AS) into the Bay of Bengal (BoB) and its subsequent mixing with the relatively fresh BoB water is vital for the north Indian Ocean salt budget. During June–September, the Summer Monsoon Current
Autor:
P. A. Francis, A. K. Jithin, J. B. Effy, A. Chatterjee, K. Chakraborty, A. Paul, B. Balaji, S. S. C. Shenoi, P. Biswamoy, A. Mukherjee, P. Singh, B. Deepsankar, S. Siva Reddy, P. N. Vinayachandran, M. S. Girish Kumar, T. V. S. Udaya Bhaskar, M. Ravichandran, A. S. Unnikrishnan, D. Shankar, A. Prakash, S. G. Aparna, R. Harikumar, K. Kaviyazhahu, K. Suprit, R. V. Shesu, N. Kiran Kumar, N. Srinivasa Rao, K. Annapurnaiah, R. Venkatesan, A. S. Rao, E. N. Rajagopal, V. S. Prasad, M. D. Gupta, T. M. Balakrishnan Nair, E. P. R. Rao, B. V. Satyanarayana
Publikováno v:
Bulletin of the American Meteorological Society. 102:137-142
Publikováno v:
Ocean Dynamics. 71:125-156
Response of Ganga-Brahmaputra river plume to wind forcing in the Bay of Bengal is studied using a numerical ocean circulation model. Four different wind forcing scenarios, namely, winds over the entire model domain, no winds anywhere over the model d