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Artykuły w czasopismach na temat „Storm; Wind waves; West coast- India”

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Data publikacji: 6 września 2023

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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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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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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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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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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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11

BEHERA, S. K., and P. S. SALVEKAR. "Numerical investigation of coastal circulation around India." MAUSAM 49, no. 3 (2021): 345–60. http://dx.doi.org/10.54302/mausam.v49i3.3640.

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A simple wind driven ocean circulation model with one active layer is used to simulate the coastal circulation around India. The close agreement of numerical results to that of the observed fields ind1cate the influence of wind on the coastal circulation. The northward currents along the west coast of India during winter months are dominated by remote forcing from Bay of Bengal; however the southward currents during summer months are less influenced by the remote forcing. The coastaly trapped Kelvin waves which give rise to the remote forcing response are found to be produced by the annual cyc

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12

Kettle, Anthony J. "Storm Anatol over Europe in December 1999: impacts on societal and energy infrastructure." Advances in Geosciences 56 (December 23, 2021): 141–53. http://dx.doi.org/10.5194/adgeo-56-141-2021.

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Abstract. Storm Anatol impacted the North Sea and northern Europe on 3–4 December 1999. It brought hurricane force winds to Denmark and northern Germany, and high winds also in Sweden and countries around the Baltic Sea. For many meteorological stations in Denmark, the wind speeds were the highest on record and the storm was ranked as a century event. The storm impacts included extensive forest damage, fatalities, hundreds of injuries, power outages, transportation interruptions, as well as storm surge flooding on the west coast of Denmark. Strongly committed to wind energy, Denmark lost 13 on

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13

Abbasi, Esmaeil, Hana Etemadi, Joseph M. Smoak, et al. "Investigation of Atmospheric Conditions Associated with a Storm Surge in the South-West of Iran." Atmosphere 12, no. 11 (2021): 1429. http://dx.doi.org/10.3390/atmos12111429.

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Severe thunderstorms are often accompanied by strong vertical air currents, temporary wind gusts, and heavy rainfall. The development of this atmospheric phenomenon over tropical shallow water zones, such as bays, can lead to intensification of atmospheric disturbances and produce a small-scale storm surge. Here, the storm surge that occurred on 19 March 2017 in the Persian Gulf coastal area has been investigated. Air temperature, precipitation, mean sea level pressure, wave height, wind direction, wind speed, geopotential height, zonal components, meridional winds, vertical velocity, relative

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14

Chen, Yongping, Shunqi Pan, Judith Wolf, and Yanliang Du. "DOWNSCALING EFFECTS ON MODELLING WAVES, TIDES AND STORM SURGE." Coastal Engineering Proceedings 1, no. 32 (2011): 33. http://dx.doi.org/10.9753/icce.v32.waves.33.

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This paper presents the results of downscaling effects when modelling waves, tides and storm surge using a nested modelling system. In this study, the coupled POLCOMS/ProWAM models are used, with 3 nested computational domains, the largest of which covers part of north-eastern Atlantic Ocean with a coarse resolution grid and the smallest covers the surrounding waters of south-west Cornish coast of the UK with a finer resolution grid. Applying the identical surface wind forcing to all 3 computational domains and the wave and tide boundary conditions provided from the coarse to finer domains, th

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15

Glejin, Johnson, V. Sanil Kumar, T. M. Balakrishnan Nair, Jai Singh, and Prakash Mehra. "Observational Evidence of Summer Shamal Swells along the West Coast of India*." Journal of Atmospheric and Oceanic Technology 30, no. 2 (2013): 379–88. http://dx.doi.org/10.1175/jtech-d-12-00059.1.

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Abstract Wave data collected off Ratnagiri, which is on the west coast of India, in 2010 and 2011 are used to examine the presence of the summer shamal swells. This study also aims to understand variations in wave characteristics and associated modifications in wind sea propagation at Ratnagiri. Wind data collected using an autonomous weather station (AWS), along with Advanced Scatterometer (ASCAT) and NCEP data, are used to identify the presence of summer shamal winds along the west coast of the Indian subcontinent and on the Arabian Peninsula. NCEP and ASCAT data indicate the presence of sum

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16

Rashmi, R., V. M. Aboobacker, P. Vethamony, and M. P. John. "Co-existence of wind seas and swells along the west coast of India during non-monsoon season." Ocean Science 9, no. 2 (2013): 281–92. http://dx.doi.org/10.5194/os-9-281-2013.

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Abstract. An attempt has been made to understand the co-existence of wind seas and swells along the west coast of India during non-monsoon season. Wave data were collected in different years during non-monsoon season (off Goa during May 2005, off Ratnagiri during January–February 2008 and off Dwarka during December 2007–January 2008), which is fairly a calm weather season along these regions. Diurnal variation in wave parameters is noticeable along the central west coast of India (off Goa and Ratnagiri), which is due to the interaction of multidirectional waves (both wind seas and swells) of v

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17

Li, Yuanyi, Huan Feng, Guillaume Vigouroux, et al. "Storm Surges in the Bohai Sea: The Role of Waves and Tides." Water 12, no. 5 (2020): 1509. http://dx.doi.org/10.3390/w12051509.

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A storm surge is a complex phenomenon in which waves, tide and current interact. Even though wind is the predominant force driving the surge, waves and tidal phase are also important factors that influence the mass and momentum transport during the surge. Devastating storm surges often occur in the Bohai Sea, a semi-enclosed shallow sea in North China, due to extreme storms. However, the effects of waves on storm surges in the Bohai Sea have not been quantified and the mechanisms responsible for the higher surges that affect part of the Bohai Sea have not been thoroughly studied. In this study

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18

Kharitonova, Lyudmila, Dmitrii Alekseev, and Vladimir Fomin. "Mathematical simulation of the Ay-Todor bay wave regime." InterCarto. InterGIS 27, no. 3 (2021): 16–31. http://dx.doi.org/10.35595/2414-9179-2021-3-27-16-31.

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Investigation of wave regime of coastal water areas is practically important for safe shipping, constructing and using of coastal infrastructure objects. At the present paper statistical characteristics and space distribution of parameters of wind waves in the Ay-Todor Bay region placed on the Crimea South Coast of the Black Sea are obtained on the basis of mathematical simulation. Analysis of the wind wave parameters for the year diapason of 1979–2017 has shown that waves running from the east and having 0.5 m heights and 3.0–3.5 s mean periods are the most repeatable. The most durable storms

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Sinha, Mourani, Ravi Kumar Yadav, and Paromita Chakraborty. "Island Modeling Using Unstructured Grid during a Tropical Storm." International Journal of Oceanography 2016 (February 15, 2016): 1–8. http://dx.doi.org/10.1155/2016/5834572.

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The coastal wave dynamics of Agatti island situated on a coral atoll in Lakshadweep, India, having a notable topographic feature of steeper eastern shore over the western shore, is analysed in this study. A multinested model setup is generated using the global third-generation models WAM (Wave Modeling) and SWAN (Simulating Waves Nearshore). A high resolution unstructured grid is generated for the domain containing the island using SMS (Surface-Water Modeling System) interpolated with merged GEBCO (General Bathymetric Chart of the Oceans) and SRTM (Shuttle Radar Topography Mission) bathymetry.

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Caillouët, Kevin A., and Suzanne L. Robertson. "Temporal and Spatial Impacts of Hurricane Damage on West Nile Virus Transmission and Human Risk." Journal of the American Mosquito Control Association 36, no. 2s (2020): 106–19. http://dx.doi.org/10.2987/19-6887.1.

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ABSTRACT Hurricanes have profound impacts on zoonotic pathogen ecosystems that exhibit spatial and temporal waves in both distance from and time since the event. Wind, rain, and storm surge directly affect mosquito vectors and animal hosts of these pathogens. In this analysis, we apply a West Nile virus transmission model parameterized for the Northern coast of the Gulf of Mexico to explore the effect of event timing of hurricane landfall, time since the event, and damage extent on human West Nile virus neuro-invasive disease (WNV-NID) risk. Early-season hurricanes, which make landfall prior t

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Dietrich, J. C., J. J. Westerink, A. B. Kennedy, et al. "Hurricane Gustav (2008) Waves and Storm Surge: Hindcast, Synoptic Analysis, and Validation in Southern Louisiana." Monthly Weather Review 139, no. 8 (2011): 2488–522. http://dx.doi.org/10.1175/2011mwr3611.1.

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AbstractHurricane Gustav (2008) made landfall in southern Louisiana on 1 September 2008 with its eye never closer than 75 km to New Orleans, but its waves and storm surge threatened to flood the city. Easterly tropical-storm-strength winds impacted the region east of the Mississippi River for 12–15 h, allowing for early surge to develop up to 3.5 m there and enter the river and the city’s navigation canals. During landfall, winds shifted from easterly to southerly, resulting in late surge development and propagation over more than 70 km of marshes on the river’s west bank, over more than 40 km

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Samiksha, Volvaiker, Ponnumony Vethamony, Charls Antony, Prasad Bhaskaran, and Balakrishnan Nair. "Wave–current interaction during Hudhud cyclone in the Bay of Bengal." Natural Hazards and Earth System Sciences 17, no. 12 (2017): 2059–74. http://dx.doi.org/10.5194/nhess-17-2059-2017.

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Abstract. The present work describes the interaction between waves and currents utilizing a coupled ADCIRC+SWAN model for the very severe cyclonic storm Hudhud, which made landfall at Visakhapatnam on the east coast of India in October 2014. Model-computed wave and surge heights were validated with measurements near the landfall point. The Holland model reproduced the maximum wind speed of ≈ 54 m s−1 with the minimum pressure of 950 hPa. The modelled maximum surge of 1.2 m matches with the maximum surge of 1.4 m measured off Visakhapatnam. The two-way coupling with SWAN showed that waves contr

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Vizy, Edward K., and Kerry H. Cook. "Tropical Storm Development from African Easterly Waves in the Eastern Atlantic: A Comparison of Two Successive Waves Using a Regional Model as Part of NASA AMMA 2006." Journal of the Atmospheric Sciences 66, no. 11 (2009): 3313–34. http://dx.doi.org/10.1175/2009jas3064.1.

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Abstract Two successive African easterly waves (AEWs) from August 2006 are analyzed utilizing observational data, the European Centre for Medium-Range Weather Forecasts reanalysis, and output from the National Center for Atmospheric Research–National Oceanic and Atmospheric Administration Weather Research and Forecasting model (WRF) to understand why the first wave does not develop over the eastern Atlantic while the second wave does. The first AEW eventually forms Hurricane Ernesto over the Caribbean Sea, but genesis does not occur over the eastern Atlantic. The second wave, although weaker t

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Vinayachandran, Puthenveettil Narayana Menon, Yukio Masumoto, Michael J. Roberts, et al. "Reviews and syntheses: Physical and biogeochemical processes associated with upwelling in the Indian Ocean." Biogeosciences 18, no. 22 (2021): 5967–6029. http://dx.doi.org/10.5194/bg-18-5967-2021.

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Abstract. The Indian Ocean presents two distinct climate regimes. The north Indian Ocean is dominated by the monsoons, whereas the seasonal reversal is less pronounced in the south. The prevailing wind pattern produces upwelling along different parts of the coast in both hemispheres during different times of the year. Additionally, dynamical processes and eddies either cause or enhance upwelling. This paper reviews the phenomena of upwelling along the coast of the Indian Ocean extending from the tip of South Africa to the southern tip of the west coast of Australia. Observed features, underlyi

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Amrutha, M. M., V. Sanil Kumar, and J. Singh. "Changes in nearshore waves during the active sea/land breeze period off Vengurla, central west coast of India." Annales Geophysicae 34, no. 2 (2016): 215–26. http://dx.doi.org/10.5194/angeo-34-215-2016.

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Abstract. A unique feature observed in the tropical and subtropical coastal area is the diurnal sea-breeze/land-breeze cycle. We examined the nearshore waves at 5 and 15 m water depth during the active sea/land breeze period (January–April) in the year 2015 based on the data measured using the waverider buoys moored in the eastern Arabian sea off Vengurla, central west coast of India. Temporal variability of diurnal wave response is examined. Numerical model Delft3D is used to study the nearshore wave transformation. The wave height increased due to the sea breeze and reached its peak at ∼ 13:

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Vallivattathillam, Parvathi, Suresh Iyyappan, Matthieu Lengaigne, et al. "Positive Indian Ocean Dipole events prevent anoxia off the west coast of India." Biogeosciences 14, no. 6 (2017): 1541–59. http://dx.doi.org/10.5194/bg-14-1541-2017.

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Abstract. The seasonal upwelling along the west coast of India (WCI) brings nutrient-rich, oxygen-poor subsurface waters to the continental shelf, favoring very low oxygen concentrations in the surface waters during late boreal summer and fall. This yearly-recurring coastal hypoxia is more severe during some years, leading to coastal anoxia that has strong impacts on the living resources. In the present study, we analyze a 1/4° resolution coupled physical–biogeochemical regional oceanic simulation over the 1960–2012 period to investigate the physical processes influencing the oxycline interann

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Verhagen, Henk Jan. "Financial Benefits of Mangroves for Surge Prone High-Value Areas." Water 11, no. 11 (2019): 2374. http://dx.doi.org/10.3390/w11112374.

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In this paper, protection options for a high-value, industrial area along the coast of West Bengal (India) are investigated. The options are designed to protect against cyclone surges with a probability of 1/100 per year. Two alternatives are compared, a classical solution of a dike with a revetment and a solution with a mangrove belt in front of the dike. The results reveal that from a pure infrastructural cash-flow point-of-view, the mangrove solution is at least 25% cheaper than the classical solution with a rock revetment. An important finding is that this conclusion does not need the fina

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Lai, R. J., and S. L. Bales. "EFFECTS OF THE GULF STREAM ON NEARSHORE WAVE CLIMATE." Coastal Engineering Proceedings 1, no. 20 (1986): 35. http://dx.doi.org/10.9753/icce.v20.35.

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Large scale ocean currents, such as the Gulf Stream, Kuroshlo, Peru Current, Agulhaus Current, etc., strongly modify the surrounding wave characteristics. As the Gulf Stream moves along the Continental Shelf of the southeast coast of the United States, the local ocean environment is divided into three wave climatic regimes. They are the offshore, the Gulf Stream, and the nearshore regimes. The nearshore zone is bounded by the land to the west and the Gulf Stream to the east. The distance between land and the Gulf Stream varies from 10 to 60 miles. Most of the waves in this regime are generated

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Li, Xiuzhen, Zhiping Wen, and Wan-Ru Huang. "Modulation of South Asian Jet Wave Train on the Extreme Winter Precipitation over Southeast China: Comparison between 2015/16 and 2018/19." Journal of Climate 33, no. 10 (2020): 4065–81. http://dx.doi.org/10.1175/jcli-d-19-0678.1.

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AbstractTwo extremely wet winters in 2015/16 and 2018/19 over Southeast China are compared in this study. South-to-north discrepancies appear in the spatial distribution of precipitation, with anomalous precipitation centered over the southeast coast in 2015/16 and the lower reaches of Yangtze River valley in 2018/19, respectively. Both instances of enhanced precipitation are ascribed mainly to warm and moist advection from the south, with transport in 2015/16 partly by a deepened India–Burma trough to the west, whereas with transport in 2018/19 mainly by a subtropical western North Pacific an

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Mehra, P., R. G. Prabhudesai, A. Joseph, et al. "A study of meteorologically and seismically induced water level and water temperature oscillations in an estuary located on the west coast of India (Arabian Sea)." Natural Hazards and Earth System Sciences 12, no. 5 (2012): 1607–20. http://dx.doi.org/10.5194/nhess-12-1607-2012.

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Abstract. The study examines the observed storm-generated sea-level oscillations (June 2007 and November 2009) along with the Sumatra geophysical tsunami (September 2007), indicating similarities in the sea-level response in the Mandovi estuary of Goa in the eastern Arabian Sea. Sea-level and surface meteorological measurements collected during storms exhibit strong synoptic disturbances leading to the coherent oscillations in the estuary with significant energy bands centred at periods of 24, 45, and 80 min. In particular, during the sporadic atmospheric event of June 2007, the atmospheric pr

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Li, Yanping, and R. E. Carbone. "Offshore Propagation of Coastal Precipitation." Journal of the Atmospheric Sciences 72, no. 12 (2015): 4553–68. http://dx.doi.org/10.1175/jas-d-15-0104.1.

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Abstract This work focuses on the seaward propagation of coastal precipitation with and without mountainous terrain nearby. Offshore of India, diurnal propagation of precipitation is observed over the Bay of Bengal. On the eastern side of the bay, a diurnal but nonpropagating signal is observed near the west coast of Burma. This asymmetry is consistent with the inertio-gravity wave mechanism. Perturbations generated by diurnal heating over the coastal mountains of India propagate offshore, amplify in the upwind direction, and dissipate in the downwind direction relative to the steering wind, o

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PRADHAN, D., and U. K. DE. "Doppler Weather Radar analysis of short term cyclonic storm." MAUSAM 63, no. 3 (2022): 459–68. http://dx.doi.org/10.54302/mausam.v63i3.1242.

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On the east coast of India, during South-West monsoon period severe cyclonic storms are very rare and if they are short term cyclones then their prediction becomes very difficult due to rapid change in the intensity of the system. Though synoptic observations failed and satellite observations also cannot give decisive picture about such systems, in that case timely warning can not be issued by the weather agencies. Such a system was formed on 19 September, 2006 at about 250 km South-East of Kolkata (India). Very heavy rainfall associated with the system caused several human casualties and exte

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Han, Weiqing, Julian P. McCreary, Yukio Masumoto, Jérôme Vialard, and Benét Duncan. "Basin Resonances in the Equatorial Indian Ocean." Journal of Physical Oceanography 41, no. 6 (2011): 1252–70. http://dx.doi.org/10.1175/2011jpo4591.1.

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Abstract Previous studies have investigated how second-baroclinic-mode (n = 2) Kelvin and Rossby waves in the equatorial Indian Ocean (IO) interact to form basin resonances at the semiannual (180 day) and 90-day periods. This paper examines unresolved issues about these resonances, including the reason the 90-day resonance is concentrated in the eastern ocean, the time scale for their establishment, and the impact of complex basin geometry. A hierarchy of ocean models is used: an idealized one-dimensional (1D) model, a linear continuously stratified ocean model (LCSM), and an ocean general cir

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Mohanty, Shravani, and Rajendra Kumar. "Review Paper on Beach Evolution of the Indian Coasts." International Journal of Ocean and Coastal Engineering 04, no. 03n04 (2022). http://dx.doi.org/10.1142/s2529807022300010.

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Beaches provide protection to residents living near the ocean by acting as a buffer against the high winds and waves of powerful storms or rough seas. It also helps the government to increase revenue and the development of infrastructure. Because beaches are very accessible to humans, it is very important to go through the demerits that are causing changes in the beaches and what steps can be taken to prevent the beaches from evolving. There are several studies indicating that there is an increase in the wave heights and wave periods along the Indian coasts, with maximum wave heights increasin

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Rabinovich, Alexander B., Jadranka Šepić, and Richard E. Thomson. "Strength in numbers: The tail-end of Typhoon Songda combines with local cyclones to generate extreme sea level oscillations on the British Columbia and Washington coasts during mid-October 2016." Journal of Physical Oceanography, October 5, 2022. http://dx.doi.org/10.1175/jpo-d-22-0096.1.

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Abstract From 12 to 16 October 2016, a series of three major low-pressure systems, including the tail-end of Typhoon Songda, crossed the coasts of British Columbia (BC) and Washington State (WA). Songda was generated on 2 October and, after travelling northward along the coast of Japan, turned eastward toward North America. Once there, it merged with two extratropical cyclones moving along the coast of Vancouver Island. The combined lows generated pronounced storm surges, seiches and infragravity waves off southern BC and northern WA. Here, we examine the event in terms of sea levels measured

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Koiting, Russel Felix, Ejria Saleh, and Md Nizam Ismail. "Beach Morphology Changes during the Northeast and Southwest Monsoons at Mantanani Besar Island, Sabah (Malaysia)." Journal of Tropical Biology & Conservation (JTBC) 14 (October 15, 2017). http://dx.doi.org/10.51200/jtbc.v14i0.890.

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Mantanani Besar Island is a tourism and island that also has communities and is located in the west coast of Sabah. The island coastline is dominated by sandy beaches that tend to change due to direct exposure from natural phenomenon (waves, wind, current and periodic storm) and anthropogenic activities. The seasonal monsoon (NEM and SWM) is an important factor that intensifies the natural phenomenon leading to major beach changes in a short period of time. Therefore, this study aims to determine the beach morphology changes (profile, width, angle and volume) and to identify short-term beach c

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