Shoreline Change Analysis along the Udupi-Dakshina Kannada Coastal Stretch in Karnataka, West Coast of India using DSAS

Author(s):  
N.A. Anjita ◽  
G.S. Dwarakish

Study of morphological variations and the effects of oceanographic processes such as erosion and accretion at different temporal scales are important to understand the nature of the coast and the cyclic changes occurring during different seasons. The Udupi-Dakshina Kannada coast along the west coast of India exhibits a wide range of changes depending on the interactions of tide and wave energy, sediment supply and more importantly human intervention. In view of this, the present work has been carried out to study the changes in shoreline changes along the Udupi-Dakshina Kannada coast over a period of 29 years from 1990 to 2019. Remote Sensing and GIS techniques have been used to demarcate shorelines and calculate the shoreline change rates. Overall accretion and erosion rates were found to be 1.28 m/year and 0.91 m/year respectively along the coast. Highest accretion and erosion rates of 12.57 m/year and 5.34 m/year was noticed along the Dakshina Kannada coast. The study also suggests that multi-dated satellite data along with statistical techniques can be effectively used for prediction of shoreline changes. Keywords: remote sensing, GIS, Dakshina Kannada coast, oceanography, shoreline.

Author(s):  
Vu Cong Huu ◽  
Dinh Van Uu

The central beach in west coast of Nha Trang bay has experienced erosion in recent years. The determination of hydrodynamic regime and causes of this beach fluctuation is still an open problem and is concerned by scientists and managers. This study shows the causes and scales of the shoreline change processes based on the results of shoreline change model and the analysis of remote sensing images of shoreline location.


2020 ◽  
Vol 36 (6) ◽  
Author(s):  
Sagar M. Waghmare ◽  
Pramod T. Hanamgond ◽  
Debashish Mitra ◽  
Basavraj K. Koti ◽  
Priyanka S. Shinde

2018 ◽  
Vol 77 (5) ◽  
Author(s):  
S. Sathish ◽  
R. S. Kankara ◽  
S. Chenthamil Selvan ◽  
M. Umamaheswari ◽  
K. Rasheed

2019 ◽  
Vol 100 (1) ◽  
pp. 17-38 ◽  
Author(s):  
S. Chenthamil Selvan ◽  
R. S. Kankara ◽  
K. Prabhu ◽  
B. Rajan

1976 ◽  
Vol 20 (04) ◽  
pp. 235-238
Author(s):  
J. Dattatri ◽  
N. Jothi Shankar ◽  
H. Raman

Hoffman and Karst have recently reported, in the title paper, an excellent review of the Rayleigh distribution and some of its applications. They mention that for many ocean zones there is a lack of measured wave data. The primary purpose of this note is to supplement their conclusions with some additional measured ocean wave data. These data, from the west coast of India near Mangalore, where a new major port has recently been commissioned, were obtained over a period of 18 months during 1968–1969, using a frequency-modulated subsurface pressure-type recorder. The analysis of this data has been reported in an earlier paper [1]. 3 More recently, during 1974, some additional data were obtained using an accelerometer-type Wave Rider buoy. The data obtained from the subsurface recorder need to be modified to account for the pressure response and instrument factors, and considerable uncertainties are involved in this computation. On the other hand, the Wave Rider data need no such modifications and can be considered to be more representative of the sea state at the locality. As such, the surface recorder data (Wave Rider data) have been utilized mainly in the preparation of this note, and the subsurface recorder data are furnished for the purpose of comparison. The west coast of India is under the influence of the southwest monsoon during the months of June to September, when the prevailing strong winds cause heavy seas. During the nonmonsoon period, the Arabian Sea is practically calm, with long low swells. Hence the data used herein cover a wide range of conditions from the 'sea' to the 'swell.'


2014 ◽  
Vol 51 (6) ◽  
pp. 644-661 ◽  
Author(s):  
Victor Joseph Loveson ◽  
Khare Richa ◽  
Mayappan Sundararajan ◽  
Anup Ramchandra Gujar

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