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dc.contributor.authorManiMurali, R.
dc.contributor.authorReshma, K.N.
dc.contributor.authorSanthoshKumar, S.
dc.contributor.authorAgrawal, Ritesh
dc.contributor.authorRatheesh, Ramakrishnan
dc.contributor.authorSreejith, K.M.
dc.contributor.authorRajawat, A.S.
dc.date.accessioned2023-12-20
dc.date.accessioned2023-12-11T04:44:37Z
dc.date.available2023-11-20
dc.date.available2023-12-11T04:44:37Z
dc.date.issued2023
dc.identifier.citationEcological Informatics, vol.78; 2023; Article no: 102373
dc.identifier.issn1574-9541
dc.identifier.otherhttps://www.sciencedirect.com/science/article/abs/pii/S1574954123004028
dc.identifier.urihttps://doi.org/10.1016/J.ECOINF.2023.102373
dc.identifier.urihttp://drs.nio.res.in/drs/handle/2264/9155
dc.descriptionIF(JCR2023) = 5.1
dc.description.abstractSubsidence in coastal deltas is a challenging issue globally, influenced by both climate and anthropogenic pressures. Owing to its rich economic value, the Godavari Delta on the east coast of India attracts the human population and is therefore a hub of developmental activities. We quantified the line of sight (LOS) rate of land deformation in the Godavari Delta, India, for two different periods using the time series interferometric analysis of Advanced Land Observing Satellite Phase Arrayed L-band Synthetic Aperture Radar (ALOS PALSAR) (2007–2011) and C-band Sentinel-1A (2017–2020) datasets. This approach was based on the Small Baseline Subset (SBAS) algorithm, which constructed 76 (ALOS) and 333 (Sentinel-1A) pairs of interferograms. The results indicated that the majority of deltas had varying LOS deformation rates in both periods. The southern and northern coastline of the deltas showed subsidence (-10 to -20 mm/yr) and uplift (5 mm to 7 mm/yr), respectively, from 2007 to 2011. The uplift (11 mm/yr) during 2017–2020 was attributed to coastal erosion and accretion during the study period. Statistical analyses showed that the majority of the coastline experienced erosion from 2006 to 2011, ranging from 0 ‐30 m/yr. Conversely, during 2017–2019, accretion ranging from 0-30 m/yr was dominant. The Kakinada spit has recently experienced an uplift of 8 mm/yr. Many factors contributing to deformation, such as groundwater fluctuations, rainfall, land use and land cover (LULC) changes, and water quality, were explored. Groundwater level variations were strongly correlated with the rate of deformation. A direct relationship was also observed between water recharge through rainfall and the ground deformation rate. The subsidence rate was estimated as 0 to ‐8 mm/yr from 2007-2011 and -10 to -20 mm/yr for 2017–2020 in the Godavari Delta. Increased urban areas and land conversion from the LULC analysis were the causative factors of subsidence in this region. Thus, the Godavari Delta will become highly vulnerable, as the region has shown various LOS deformation rates. Studies on land subsidence are highly relevant for effective coastal management planning and management
dc.languageen
dc.publisherElsevier
dc.relation.isreferencedbySCI
dc.rightsOnly the author version of the copright reserved papers uploaded. Contact drs@nio.org for any complaints regarding copyright violations
dc.titleLand subsidence studies in the Godavari Delta regions of the East coast of India using ALOS and Sentinel 1 data
dc.typeJournal Article
dc.affiliation.authorCSIR-National Institute of Oceanography, Dona Paula, Goa, India


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