Glitson Pereira

Mr. Glitson Pereira


Research Focus & Metrics

Academic Career Length

8Years (2019-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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1 May 2019 in Geodesy and Geodynamics
Verified
Journal Article
Open access
NRNithu Raj
Nithu Raj
BGB. Gurugnanam
B. Gurugnanam
VSV. Sudhakar
V. Sudhakar
GPGlitson Pereira
Glitson Pereira

1 September 2022 in Journal of the Geological Society of India
Verified
Journal Article
Closed access
PDF file
GPGlitson Pereira
Glitson Pereira
GGGurugnanam Gurugnanam
Gurugnanam Gurugnanam
Santonu GoswamiSantonu Goswami
Santonu Goswami
SCSaroj Choudhury
Saroj Choudhury
The coastal region is one of the most sensitive areas on earth. This region has a diversified ecosystem. Erosion and accretion are common natural phenomena that can be seen in this region. In some circumstances, these changes become hazardous to the coastal ecosystem. Natural processes such as rainfall, flood, cyclone, longshore drift, and tectonic shifts can trigger irregular coastal changes. Similarly, anthropogenic factors such as urbanization, unscientific land usage, mining, etc., enhance coastal dynamics and make larger changes. Hence identification of such region has great importance. Geospatial technology has brought various advanced methods for shoreline change studies. It has decreased the huge effort for getting an accurate result for a larger area. Landsat satellite imageries with 30 m spatial resolution have been used for studying the changes in the shoreline of Ramanathapuram for the years 2000, 2005, 2010, 2015 and 2020. In Geographic Information System (GIS) software, the Digital Shoreline Analysis System (DSAS) tool is added for shoreline change analysis. DSAS will build the baseline transects. The rate of shoreline change was calculated using the MATLAB feature runtime function for ArcGIS. Based on the DSAS output, the region of high erosion, low erosion, stable, and low accretion, high accretion zones have been identified on the shore. The results reveal that 5.1% of the shoreline, around 9.3 km is under high erosion, 11.5% of the shoreline, which is around 20.8 km, is under low erosion, 71% of the shoreline, around 128 km, is a stable region, 6.7% of shorelines, around 12 km, have low accretion, and 5.6% of shorelines, around 10.1 km, have high accretion. The coastal villages, namely, Mayakulam, Keelakakrai, Periapattinam, Mandapam, West-Pamban, and East-Rameswaram, have a high erosion with a maximum rate of change between 2.29 to 5.11 m/y. The coastal villages Ervadi, Kalimankund, Sattankonvalsai, South-Pamban and South-Rameswaram have high accretion with a maximum rate of change between 2.34 to 5.24 m/y.

1 September 2022 in Geodesy and Geodynamics
Verified
Journal Article
Open access
GGGurugnanam Gurugnanam
Gurugnanam Gurugnanam
SSSreechitra Suresh
Sreechitra Suresh
SGSantonu Goswami
Santonu Goswami
BSBairavi Swaminathan
Bairavi Swaminathan
GPGlitson Pereira
Glitson Pereira