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Relevant bibliographies by topics / Storm; Wind waves; West coast- India

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Journal articles

Academic literature on the topic 'Storm; Wind waves; West coast- India'

Author: Grafiati

Published: 6 September 2023

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Journal articles on the topic "Storm; Wind waves; West coast- India"

1

Glejin, J., V. Sanil Kumar, T. N. Balakrishnan Nair, and J. Singh. "Influence of winds on temporally varying short and long period gravity waves in the near shore regions of Eastern Arabian Sea." Ocean Science Discussions 9, no. 5 (2012): 3021–47. http://dx.doi.org/10.5194/osd-9-3021-2012.

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Abstract. Wave data collected off Ratnagiri, west coast of India during 1 May 2010 to 30 April 2012 is used in the study. Seasonal and annual variation in wave data controlled by the local wind system such as sea breeze and land breeze, and remote wind generated long period waves observed along the west coast of India, is studied. Sea breeze plays an important role in determining the sea state during pre and post monsoon seasons and the maximum wave height is observed during peak hours of sea breeze at 15:00 UTC. Long period waves (peak period over 13 s) are observed mainly during the pre and

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2

Glejin, J., V. Sanil Kumar, T. M. Balakrishnan Nair, and J. Singh. "Influence of winds on temporally varying short and long period gravity waves in the near shore regions of the eastern Arabian Sea." Ocean Science 9, no. 2 (2013): 343–53. http://dx.doi.org/10.5194/os-9-343-2013.

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Abstract. Wave data collected off Ratnagiri, west coast of India, during 1 May 2010 to 30 April 2012 are used in this study. Seasonal and annual variations in wave data controlled by the local wind system such as sea breeze and land breeze, and remote wind generated long period waves are also studied. The role of sea breeze on the sea state during pre- and postmonsoon seasons is studied and it is found that the maximum wave height is observed at 15:00 UTC during the premonsoon season, with an estimated difference in time lag of 1–2 h in maximum wave height between premonsoon and postmonsoon se

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3

Poulose, Jismy, A. D. Rao, and Prasad K. Bhaskaran. "Role of continental shelf on non-linear interaction of storm surges, tides and wind waves: An idealized study representing the west coast of India." Estuarine, Coastal and Shelf Science 207 (July 2018): 457–70. http://dx.doi.org/10.1016/j.ecss.2017.06.007.

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4

DATTATRI, J., and P. VIJAYA KUMAR. "Wave Prediction for the east coast of India under storm conditions in the Bay of Bengal." MAUSAM 25, no. 2 (2022): 211–22. http://dx.doi.org/10.54302/mausam.v25i2.5195.

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Cyclonic storms are frequent in the Bay of Bengal particularly during the NE monsoon period. Some of these storms are severe and generate high waves which cause havoc in the coastal regions. This paper presents an analysis of the cyclonic storm which hit coastal Andhra Pradesh on 7 November 1969. Wave prediction under storm conditions involves an analysis of moving fetches and variable wind speeds. Wilson's graphical method incorporating the latest available wave prediction relations was used for wave predicted waves which are deep water waves, were modified to account for refraction, sh

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5

Mehra, P., S. Mohan, P. Vethamony, et al. "Coastal sea level response to the tropical cyclonic forcing in the north Indian Ocean." Ocean Science Discussions 11, no. 1 (2014): 575–611. http://dx.doi.org/10.5194/osd-11-575-2014.

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Abstract. The study examines the observed storm-generated sea-level variation due to deep depression (Event-E1) in the Arabian Sea from 26 November–1 December 2011 and a cyclonic storm "THANE" (Event-E2) over the Bay of Bengal during 25–31 December 2011. The sea-level and surface meteorological measurements collected during these extreme events exhibit strong synoptic disturbances leading to storm surge up to 43 cm on the west coast and 29 cm on the east coast of India due to E1 and E2. E1 generated sea level oscillations at the measuring stations on the west coast (Ratnagiri, Verem and Karwar

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6

Cousineau, Julien, and Enda Murphy. "Numerical Investigation of Climate Change Effects on Storm Surges and Extreme Waves on Canada’s Pacific Coast." Atmosphere 13, no. 2 (2022): 311. http://dx.doi.org/10.3390/atmos13020311.

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Storm surges and waves are key climate-driven parameters affecting the design and operation of ports and other infrastructure on the coast. Reliable predictions of future storm surges and waves are not yet available for the west coast of Canada, and this data gap hinders effective climate risk assessment, planning and adaptation. This paper presents numerical simulations of storm surges and waves in British Columbia coastal waters under a future climate (Representative Concentration Pathway) scenario (RCP8.5). The numerical models were first forced by wind and surface pressure fields from the

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7

Eerkes-Medrano, Laura, David E. Atkinson, Hajo Eicken, et al. "Slush-Ice Berm Formation on the West Coast of Alaska." ARCTIC 70, no. 2 (2017): 190. http://dx.doi.org/10.14430/arctic4644.

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Some coastal communities in western Alaska have observed the occurrence of “slush-ice berms.” These features typically form during freeze-up, when ice crystal – laden water accumulates in piles on the shore. Slush-ice berms can protect towns from storm surge, and they can limit access to the water. Local observations from the communities of Gambell, Shaktoolik, Shishmaref, and Wales were synthesized to develop a taxonomy of slush-ice berm types and a conceptual process model that describes how they form and decay. Results indicated two types of slush-ice berm formation processes: in situ (form

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8

Prince, Harshith Clifford, R. Nirmala, R. S. Mahendra, and P. L. N. Murty. "Storm Surge Hazard Assessment Along the East Coast of India using Geospatial Techniques." Asian Journal of Water, Environment and Pollution 19, no. 6 (2022): 51–57. http://dx.doi.org/10.3233/ajw220088.

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The study aims to estimate the extent of inundation and depth due to a storm surge event by selecting a worst-case cyclone track scenario for Andhra Pradesh, Odisha and West Bengal on the basis of historic data. Storm surge model results for the Orissa cyclone suggest that over 2,150 km2 of land is inundated with an extent of 45 km from the shoreline and 1,100 km2 area submerged with 1-2 m from the ground. Andhra’s model suggests that about 450 km2 of the area is inundated due to which the majority of the area is submerged <1 m from the ground. The West Bengal model is carried out using a s

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9

Sanil Kumar, V., C. Sajiv Philip, and T. N. Balakrishnan Nair. "Waves in shallow water off west coast of India during the onset of summer monsoon." Annales Geophysicae 28, no. 3 (2010): 817–24. http://dx.doi.org/10.5194/angeo-28-817-2010.

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Abstract. The wave growth characteristics during the onset of summer monsoon in a swell dominated open ocean at a location off the west coast of India at 14 m water depth are studied. 67% of the measured waves are due to the swells arriving from south and south-west and the balance was due to the seas from south-west to north-west. Wave age of the measured data indicates that the measured waves are young sea with presence of swells. Even when the wind speed reduced to less than 3 m/s, significant wave height more than 2 m is present due to the swells in the Arabian Sea. The maximum wave height

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10

Mehra, P., M. Soumya, P. Vethamony, et al. "Coastal sea level response to the tropical cyclonic forcing in the northern Indian Ocean." Ocean Science 11, no. 1 (2015): 159–73. http://dx.doi.org/10.5194/os-11-159-2015.

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Abstract. The study examines the observed storm-generated sea level variation due to deep depression (event 1: E1) in the Arabian Sea from 26 November to 1 December 2011 and a cyclonic storm "THANE" (event 2: E2) over the Bay of Bengal during 25–31 December 2011. The sea level and surface meteorological measurements collected during these extreme events exhibit strong synoptic disturbances leading to storm surges of up to 43 cm on the west coast and 29 cm on the east coast of India due to E1 and E2. E1 generated sea level oscillations at the measuring stations on the west coast (Ratnagiri, Ver

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