MODERN BENTHIC FORAMINIFERA IN SUBTIDAL WATERS OF JOHOR: IMPLICATIONS FOR HOLOCENE SEA-LEVEL CHANGE ON THE EAST COAST OF PENINSULAR MALAYSIA

2016 ◽  
Vol 46 (4) ◽  
pp. 347-357 ◽  
Author(s):  
Fatin Izzati Minhat ◽  
Behara Satyanarayana ◽  
Mohd-Lokman Husain ◽  
Vijayan V.V. Rajan
Keyword(s):  
Sea Level ◽  
Benthic Foraminifera ◽  
East Coast ◽  
Sea Level Change ◽  
Peninsular Malaysia ◽  
Level Change ◽  
Holocene Sea Level

scholarly journals Impacts of Future Sea-Level Rise under Global Warming Assessed from Tide Gauge Records: A Case Study of the East Coast Economic Region of Peninsular Malaysia

Land ◽  
2021 ◽  
Vol 10 (12) ◽  
pp. 1382
Author(s):  
Milad Bagheri ◽  
Zelina Z. Ibrahim ◽  
Mohd Fadzil Akhir ◽  
Bahareh Oryani ◽  
Shahabaldin Rezania ◽  
...  
Keyword(s):  
Neural Network ◽  
Global Warming ◽  
Sea Level Rise ◽  
Sea Level ◽  
East Coast ◽  
Tide Gauge ◽  
Sea Level Change ◽  
Peninsular Malaysia ◽  
Tide Gauge Records ◽  
Level Change

The effects of global warming are putting the world’s coasts at risk. Coastal planners need relatively accurate projections of the rate of sea-level rise and its possible consequences, such as extreme sea-level changes, flooding, and coastal erosion. The east coast of Peninsular Malaysia is vulnerable to sea-level change. The purpose of this study is to present an Artificial Neural Network (ANN) model to analyse sea-level change based on observed data of tide gauge, rainfall, sea level pressure, sea surface temperature, and wind. A Feed-forward Neural Network (FNN) approach was used on observed data from 1991 to 2012 to simulate and predict the sea level change until 2020 from five tide gauge stations in Kuala Terengganu along the East Coast of Malaysia. From 1991 to 2020, predictions estimate that sea level would increase at a pace of roughly 4.60 mm/year on average, with a rate of 2.05 ± 7.16 mm on the East Coast of Peninsular Malaysia. This study shows that Peninsular Malaysia’s East Coast is vulnerable to sea-level rise, particularly at Kula Terengganu, Terengganu state, with a rate of 1.38 ± 7.59 mm/year, and Tanjung Gelang, Pahang state, with a rate of 1.87 ± 7.33 mm/year. As a result, strategies and planning for long-term adaptation are needed to control potential consequences. Our research provides crucial information for decision-makers seeking to protect coastal cities from the risks of rising sea levels.

Delta initiation and Holocene sea-level change: example from the Song Hong (Red River) delta, Vietnam

2004 ◽  
Vol 164 (3-4) ◽  
pp. 237-249 ◽  
Author(s):  
Kazuaki Hori ◽  
Susumu Tanabe ◽  
Yoshiki Saito ◽  
Shigeko Haruyama ◽  
Viet Nguyen ◽  
...  
Keyword(s):  
Sea Level ◽  
Sea Level Change ◽  
River Delta ◽  
Red River ◽  
Red River Delta ◽  
Level Change ◽  
Holocene Sea Level

scholarly journals Late Holocene sea-level change around Newfoundland

2007 ◽  
Vol 44 (10) ◽  
pp. 1453-1465 ◽  
Author(s):  
Julia F Daly ◽  
Daniel F Belknap ◽  
Joseph T Kelley ◽  
Trevor Bell
Keyword(s):  
Salt Marsh ◽  
Sea Level Rise ◽  
Sea Level ◽  
Late Holocene ◽  
Sea Level Change ◽  
Laurentide Ice Sheet ◽  
Change Analysis ◽  
Level Change ◽  
Rising Sea Level ◽  
Holocene Sea Level

Differential sea-level change in formerly glaciated areas is predicted owing to variability in extent and timing of glacial coverage. Newfoundland is situated close to the margin of the former Laurentide ice sheet, and the orientation of the shoreline affords the opportunity to investigate variable rates and magnitudes of sea-level change. Analysis of salt-marsh records at four sites around the island yields late Holocene sea-level trends. These trends indicate differential sea-level change in recent millennia. A north–south geographic trend reflects submergence in the south, very slow sea-level rise in the northeast, and a recent transition from falling to rising sea-level at the base of the Northern Peninsula. This variability is best explained as a continued isostatic response to deglaciation.

Rauk - A Forgotten Witness of Holocene Sea-level Change and Development of Baltic Rocky Coasts: A Pilot Geomorphological Study in Lergrav Raukar Field

2020 ◽  
Vol 95 (sp1) ◽  
pp. 659
Author(s):  
Mateusz C. Strzelecki ◽  
Filip Duszyński ◽  
Sebastian Tyszkowski ◽  
Łukasz Zbucki ◽  
Marek Kasprzak
Keyword(s):  
Sea Level ◽  
Sea Level Change ◽  
Level Change ◽  
Rocky Coasts ◽  
Holocene Sea Level
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