Beach-Face Morphodynamics of Different Morphological Setting Along Teluk Chempedak to Kuala Pahang, Malaysia

Mustapa, Mohd Zaini; Saad, Shahbudin; Hadi, Muhammad Salihi Abdul; Yunus, Kamaruzzaman; Sapon, Noraisyah

doi:10.11113/jt.v77.6739

Cited by 7 publications

(5 citation statements)

References 17 publications

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“…Previous studies was conducted by [21] revealed that the shoreline of the Cherating have rocky shores and sandy beaches except at the mouth of the river where the sand spit are formed. According to recent studies by [17] also proved the study's findings that Pahang's beaches have rocky shores located in Teluk Cempedak and Tanjung Tembeling, the muddy coastline of Tanjung Lumpur and the sandy shores are located in Kuala Pahang. These findings are supported by the findings of [22,18] which showed that coastal of Sungai Ular, Balok and Tanjung Agas are consists fine sand and medium sand respectively.…”

Section: Geomorphology Of Coastalmentioning

confidence: 72%

“…The study area comprises of seven distinguish beach profile in Pahang, from Pantai Cherating (4° 7'29.83"N, 103°23'47.59"E) located at the north eastern of the state to Tanjung Agas (3°30'32.02"N, 103°28'34.57"E) where it is located at the southern east of the state as shown Figure 1. Located in the eastern region, the coastline of study area is facing the South China Sea where the coastline consists of sandy and muddy beaches with a total length of 209 km [17]. Based on the NCES 1985, these area were classified as a high erosion of coastal among of East Coast of Peninsular Malaysia with known as K1 and K2 category.…”

Section: Study Areamentioning

confidence: 99%

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Variation of Beach Profile Along Pahang Coast in Malaysia

Mohd¹,

Maulud²,

Begum³

et al. 2018

IJET

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Pahang is placed at the east coast of Peninsular Malaysia and has a lot of attractive coasts with interesting scenery, which can capture the attention of people to the coasts. The seven (7) of significant coasts namely Pantai Cherating, Holiday Villa beach, Pantai Balok, Sungai Ular, Pantai Sepat, Pantai Cheruk Palok and Pantai Tanjung Agas are classified has experienced about erosion coastal problem especially having significantly for social, environment and economic value recreational activities along of this shoreline. Coastal erosion is recognized as the permanent loss of land and habitats along of the coast. The variation of beach profile characteristics along the shoreline of Pahang will be identified and described using the beach profile survey and interpolation technique. From that, the information of erosion and accretion for topography surface of coastal was generated by calculating distance and elevation of coasts. Most of these study are consist the sandy coastal. Hence the ranges value of coastal width for Tanjung Agas is shows high value of erosion and accretion with -7.74 and 3.93 m/year. To sum up, the findings of study might be useful in significant decision making for protecting and mitigation measures towards sustainable coastal management along the Pahang coastal.

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Section: Geomorphology Of Coastalmentioning

confidence: 72%

Section: Study Areamentioning

confidence: 99%

Variation of Beach Profile Along Pahang Coast in Malaysia

Mohd¹,

Maulud²,

Begum³

et al. 2018

IJET

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“…rocky shore (Teluk Cempedak [TC] and Batu Hitam [BH]) and sandy shore (BA, Kempadang [KEM] and SEP). According to Mustapa et al (2015), the geomorphology characteristics along the coastal area consist of sandy and muddy beaches with total length of 209 km of Pahang coastline. This study identified five recreational beaches along the South China Sea, namely, BA, BH, TC, KEM and SEP. Coordinates (latitude and longitude) for each station were recorded using Garmin 62S Global Positioning System (GPS).…”

Section: Description Of Study Areamentioning

confidence: 99%

Rip current occurrence probability at selected recreational beaches along Pahang coastline

Hamsan

Ramli

2020

EFCC

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Purpose Pahang beaches draw more than thousand visitors throughout the year. From the year 2006 to 2018, more than 30 drowning and near-drowning cases were recorded mainly from rip currents. Rip currents are defined as unexpected currents that carried beachgoers away to seaward direction more than approximately 50 m from shore. The prediction of rip current development is very important for the protection of human life. This study aims to conduct preliminary survey and field works to identify rip current hazards. Design/methodology/approach The output would be an early warning preventative mitigation to public in Pahang. Beach state model, dimensionless fall velocity, littoral environment observation and relative tidal range were recorded for five recreational beaches during two different months (March and April 2018). The morphodynamic parameters such sediment fall velocity, sediment grain size and beach slope are then analysed using software PROFILER. Classification of risks was done based on beach morphodynamic model. The morphodynamics are classified as low tide bar rip, barred and low tide terrace associated with rip current, bar dissipative, reflective, non-bar dissipative, low tide terrace and ultra-dissipative. Findings Result shows three out of five recreational beaches may develop high-risk rip currents. During the first month of the survey, Batu Hitam (BH) was recorded the only one recreational beach that may develop high-risk rip current followed by Teluk Cempedak (TC) and Kempadang (KEM) as middle-risk rip current beaches, while Balok (BA) and Sepat (SEP) as low-risk rip current beaches. Different during second month of the survey, BA, BH and SEP were recorded as high-risk rip current beaches while TC and KEM as low-risk rip current beaches. Originality/value The results are consistent with beach incidents (drowning and near-drowning) reported.

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“…The most important beach classifications around the world have been carried out in Australia (Wright et al, 1979;Wright and Short, 1984;Masselink and Short, 1993;Masselink and Pattiaratchi, 2001;Masselink et al, 2006;Sénéchal et al, 2009;Valiente et al, 2019), and the United Kingdom (Scott et al, 2011;Valiente et al, 2019). Classifications have also been carried out in Brazil (Pereira et al, 2010;Andreoli et al, 2019;Holanda et al, 2020), Malaysia (Mustapa et al, 2015), Mexico (where 2015), México (donde se realizaron análisis comparativos entre secciones subaéreas y submareales) (Ruiz de Alegría-Arzaburu et al, 2013, 2016Torres-Freyermuth et al, 2017; Ruiz de Alegría-Arzaburu y Vidal-Ruiz, 2018) y Francia (Sénéchal et al, 2009;Castelle et al, 2014;Sénéchal y Ruiz de Alegría-Arzaburu, 2020).…”

Section: Introductionmentioning

confidence: 99%

Morfodinámica de una playa tropical macromareal: La Bocana, Costa Pacífica de Colombia

Ricaurte-Villota,

Coca Domínguez

2023

Bol. Investig. Mar. Costeras

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Este estudio analiza la morfodinámica de la playa La Bocana en el Pacífico tropical colombiano, en un régimen macromareal. Los datos se tomaron con un sistema de posicionamiento global diferencial para generar modelos digitales de elevación y perfiles de playa entre 2014 y 2019. Posteriormente, se realizó una clasificación morfodinámica utilizando los parámetros de velocidad de caída adimensional y amplitud relativa de las mareas. Los resultados indican que los tipos de playa predominantes fueron dominados y modificados por la marea: tipo disipativas (modificadas por mareas, dominadas por mareas y erosivas) e intermedias (modificadas por mareas y no erosivas). Se observaron perfiles reflectantes frente a la playa (época erosiva) en 2014 y 2015. A pesar de que la playa estudiada se localiza en el trópico, los resultados no difieren con los propuestos para playas de latitudes medias. Los resultados sugieren el dominio del rango mareal en la determinación de los estados morfodinámicos de la playa. Este estudio muestra que la playa La Bocana tiene diferentes estados morfodinámicos espacio-temporales, es decir que no existe un único estado de playa representativo. 6 años de datos muestran variaciones intranuales (estacionales) o bajo ciertas condiciones ambientales (relacionadas con El Niño), las cuales cambian significativamente las playas.

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Beach-Face Morphodynamics of Different Morphological Setting Along Teluk Chempedak to Kuala Pahang, Malaysia

Cited by 7 publications

References 17 publications

Variation of Beach Profile Along Pahang Coast in Malaysia

Variation of Beach Profile Along Pahang Coast in Malaysia

Rip current occurrence probability at selected recreational beaches along Pahang coastline

Morfodinámica de una playa tropical macromareal: La Bocana, Costa Pacífica de Colombia

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