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Sediment Characteristics, Processes and Stability of the Beaches in the Northern Kerala Coast, India


Affiliations
1 Marine Science Division, Centre for Earth Science Studies, P. O. Box No. 7250, Akkulam, Trivandrum, 695 031, India
     

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The cyclicity in the erosional and accretional pattern is monsoon controlled. The erosion during monsoon (May-August) and accretion during pre-monsoon (January-April) and post-monsoon (September-December) are well defined. The transport trends derived from the progressive changes in the grain-size characteristics show relatively better correlation with the measured trends where they are not influenced by the input of sediments from multiple sources. The obliquely approaching swell waves which generate intense northerly longshore currents during non-monsoon season favour accretion of the beaches. The foreshore in the accreted zones are gentler and are characterized by finer and negatively skewed sediments. This zone exhibits a higher period for the breaking waves. The converse is true in the beaches where erosion is prevalent during the monsoon season.

Keywords

Sedimentology, Grain-Size, Sediment Transport, Beach Stability, Kerala Coast.
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  • Sediment Characteristics, Processes and Stability of the Beaches in the Northern Kerala Coast, India

Abstract Views: 199  |  PDF Views: 1

Authors

M. Samsuddin
Marine Science Division, Centre for Earth Science Studies, P. O. Box No. 7250, Akkulam, Trivandrum, 695 031, India
K. K. Ramachandran
Marine Science Division, Centre for Earth Science Studies, P. O. Box No. 7250, Akkulam, Trivandrum, 695 031, India
G. K. Suchindan
Marine Science Division, Centre for Earth Science Studies, P. O. Box No. 7250, Akkulam, Trivandrum, 695 031, India

Abstract


The cyclicity in the erosional and accretional pattern is monsoon controlled. The erosion during monsoon (May-August) and accretion during pre-monsoon (January-April) and post-monsoon (September-December) are well defined. The transport trends derived from the progressive changes in the grain-size characteristics show relatively better correlation with the measured trends where they are not influenced by the input of sediments from multiple sources. The obliquely approaching swell waves which generate intense northerly longshore currents during non-monsoon season favour accretion of the beaches. The foreshore in the accreted zones are gentler and are characterized by finer and negatively skewed sediments. This zone exhibits a higher period for the breaking waves. The converse is true in the beaches where erosion is prevalent during the monsoon season.

Keywords


Sedimentology, Grain-Size, Sediment Transport, Beach Stability, Kerala Coast.