About Me |
---|
Dr. Kamal Kumar Barik is working an Associate Professor in the Dept. of Civil Engineering, School of Engineering and Technology, CUTM, Bhubaneswar Campus. He did his Ph.D. at SRM University, Chennai in the field of Remote Sensing and GIS. He has been more than 8 years of teaching experience at the Post Graduate level (M.Sc. and M.Tech.). Previously he was served as a Lecturer / Assistant Professor at the Dept. of Earth Sciences, Sambalpur University. |
He has more than 30 National and International peer-review journals and 4 book chapters. He has attended more than 15 numbers of National and International Conferences. He has supervised 8 numbers of M.Tech students.
Sl. No. | Title | Issuer |
---|
Abstract: Odisha, a coastal state on eastern seaboard of India possesses a ~450 km long coastline vulnerable to a multitude of natural and anthropogenic threats. The present study reports a systematic assessment of rates of shoreline change over a period of 25 years from 1990- 2015, using Landsat 5 and 8 series of (Thematic Mapper and Operational Land Imager) satellite images. An analysis of rate of shoreline change was carried out along select regions of Odisha coast using Digital Shoreline Analysis System (DSAS). Linear Regression Method (LRR) was used to estimate net shoreline change at sub decade time scale and End Point Rate (EPR) to estimate net shoreline change rate in between two consecutive years. The highest erosion with a coastline length of 63 km was observed between Rajnagar (around Satabhaya beach) and Mahakalapara (near to Hukitola beach) block of Kendrapara district and between Ersama (around Paradeep port) and Balikuda blocks (northern parts of Devi River mouth) of Jagatsinghpur coastal district. The result suggest that both EPR and LRR techniques were used to estimate shoreline change rate and the similar result of erosion by both EPR and LRR technique indicated weaker cyclic trend in erosion.
K K Barik, R. Annaduari, P C Mohanty, R S Mahendra, J K Tripathy and D Mitra (2019) Statistical Assessment of Long-term Shoreline Changes along the Odisha Coast
PRAKASH CHANDRA DALEI, J.K. TRIPATHY, K.K. BARIK AND SMRUTI R. PANDA (2019) GROUNDWATER HYDROCHEMISTRY AROUND THE SHRIMP PONDS OF ERSAMA AND BALIKUDA BLOCKS OF JAGATSINGHPUR DISTRICT, ODISHA
Kamal Kumar Barik, Sanjiba Kumar Baliarsingh, Amit Kumar Jena, Suchismita Srichandan (2020) Satellite Retrieved Spatio-temporal Variability of Phytoplankton Size
Classes in the Arabian Sea
•
Alakes Samanta2
• Aneesh Anandrao Lotliker2
Sridhara Setti, Rathinasamy Maheswaran, Venkataramana Sridhar ,
Kamal Kumar Barik, Bruno Merz and Ankit Agarwal
Binod Kumar Sethi, Siba Prasad Mishra, Kabir Sethi and Kamal Barik
https://doi.org/10.1061/(ASCE)HE.1943-5584.0001937
S. Setti, R. Maheswaran, D. Radha, V. Sridhar,
K. K. Barik, and M. L. Narasimham
Prithviraj N, Tripathy J K, Panda S R and Barik K K
The coastal zones of northern Odisha coast, western Bay of Bengal, are highly exposed to natural forcing. These regions
are vulnerable due to natural hazards such as cyclones, tsunamis, floods, shoreline/beach erosion and sea-level rise. Further,
the increased intensity and density of the extreme events in the recent decades have contributed more to the coastal
vulnerability, thereby causing floods and inundation. Therefore, there is a need of sustainable use of the coastal zone with
proper management practices. In this context, coastal vulnerability index (CVI) has been proved as an effective method for
assigning the vulnerability status to any coastal zone. The present research work aims to develop a CVI by integrating risk
values of nine input variables and to segment them into low, moderate, high and very high vulnerability categories as per
their degree of vulnerability. The study area exhibits a long 273.8 km coastal tract, and about 9.6% of the coastal tract is
under very high vulnerability category, followed by 29.7% under high vulnerability, 46.3% under medium vulnerability
and rest 14.3% under low vulnerability.
Phytoplankton pigment composition was evaluated during the pre-cyclone phase (PRCP) and post-cyclone phase
(POCP) of tropical cyclone Fani in the coastal waters of the northwestern Bay of Bengal. The chromatographic
analysis revealed higher pigment diversity and an increase in individual pigment concentration during POCP.
Chlorophyll–a (chl–a) was the dominant pigment during PRCP and POCP, followed by fucoxanthin. However,
chl–a and fucoxanthin concentrations increased 18- and 14-folds, respectively, during the POCP, signifying
Bacillariophyta bloom. Complementing microscopy confirmed the dominance of the toxic Bacillariophyta species
Pseudo-nitzschia pungens (reaching 5.47 × 104 cells l
? 1
) during the POCP. The cyclone-induced nutrient recharge
of the ambient medium could have promoted phytoplankton growth, causing the reappearance of diatom bloom
during the later phase of the pre-southwest monsoon. Small-sized Prymnesiophyta and Cryptophyta were not
detected microscopically; however, they were identified by chromatographic analysis through pigment markers
during POCP.
Hydrological model calibration is a quintessential step in model development, and the time scale of calibration depends on the application. However, the implications of choice of time scale of calibration have not been explored extensively. Here, we evaluate the effect of the time scale of calibration on model sensitivity, best parameter ranges, and predictive uncertainty for three river basins using the Soil and Water Assessment Tool (SWAT) model. Multiple models were set up for three different catchments from southern India. Our results showed that the sensitivity of the parameters, best parameter ranges, and model performance are conditioned on the time scale of calibration. The models calibrated at coarser time scales marginally outperformed the models calibrated at fine time scale in terms of Nash-Sutcliffe efficiency and percentage bias. Transfer of parameters across scales (both from coarse to fine and from fine to coarse) have a general tendency to worsen the model performance in all three catchments, with few exceptions.