Subodh Chandra Pal

Dr. Subodh Chandra Pal

Department of Geography, The University of Burdwan, West Bengal, India

Research Focus & Metrics

Academic Career Length

19Years (2008-Present)

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

Representative Publications

View All Publications
31 October 2020 in Remote Sensing
Verified
Journal Article
Open access
PDF file
SBShahab S. Band
Shahab S. Band
SJSaeid Janizadeh
Saeid Janizadeh
SPSubodh Chandra Pal
Subodh Chandra Pal
ASAsish Saha
Asish Saha
Rabin ChakraborttyRabin Chakrabortty
Rabin Chakrabortty
Amir MosaviAmir Mosavi
Amir Mosavi
Flash flooding is considered one of the most dynamic natural disasters for which measures need to be taken to minimize economic damages, adverse effects, and consequences by mapping flood susceptibility. Identifying areas prone to flash flooding is a crucial step in flash flood hazard management. In the present study, the Kalvan watershed in Markazi Province, Iran, was chosen to evaluate the flash flood susceptibility modeling. Thus, to detect flash flood-prone zones in this study area, five machine learning (ML) algorithms were tested. These included boosted regression tree (BRT), random forest (RF), parallel random forest (PRF), regularized random forest (RRF), and extremely randomized trees (ERT). Fifteen climatic and geo-environmental variables were used as inputs of the flash flood susceptibility models. The results showed that ERT was the most optimal model with an area under curve (AUC) value of 0.82. The rest of the models’ AUC values, i.e., RRF, PRF, RF, and BRT, were 0.80, 0.79, 0.78, and 0.75, respectively. In the ERT model, the areal coverage for very high to moderate flash flood susceptible area was 582.56 km2 (28.33%), and the rest of the portion was associated with very low to low susceptibility zones. It is concluded that topographical and hydrological parameters, e.g., altitude, slope, rainfall, and the river’s distance, were the most effective parameters. The results of this study will play a vital role in the planning and implementation of flood mitigation strategies in the region.

1 March 2020 in Advances In Space Research
Verified
Journal Article
Closed access
ICIndrajit Chowdhuri
Indrajit Chowdhuri
SPSubodh Chandra Pal
Subodh Chandra Pal
RCRabin Chakrabortty
Rabin Chakrabortty

6 January 2023 in Journal of Environmental Management
Verified
Journal Article
Closed access
PRParamita Roy
Paramita Roy
SPSubodh Chandra Pal
Subodh Chandra Pal
RCRabin Chakrabortty
Rabin Chakrabortty
ICIndrajit Chowdhuri
Indrajit Chowdhuri
ASAsish Saha
Asish Saha
MSManisa Shit
Manisa Shit

1 November 2020 in Journal of Cleaner Production
Verified
Journal Article
Closed access
PRParamita Roy
Paramita Roy
SPSubodh Chandra Pal
Subodh Chandra Pal
RCRabin Chakrabortty
Rabin Chakrabortty
ICIndrajit Chowdhuri
Indrajit Chowdhuri
SMSadhan Malik
Sadhan Malik
BDBiswajit Das
Biswajit Das

9 December 2018 in Geology, Ecology, and Landscapes
Verified
Journal Article
Open access
BDBiswajit Das
Biswajit Das
SPSubodh Chandra Pal
Subodh Chandra Pal
SMSadhan Malik
Sadhan Malik
Rabin ChakraborttyRabin Chakrabortty
Rabin Chakrabortty
Remote sensing and geographical information system (RS-GIS) have become a leading tool for modeling and mapping of groundwater resources. An attempt has been made to delineate the groundwater potential zones of Puruliya district using the integrated RS-GIS and AHP techniques. All the themes and their features have been assigned weights according to their relative importance and their normalized weights were calculated after the hierarchical ranking by pair-wise comparison matrix of analytical hierarchy process (AHP). Groundwater potential map has been prepared through weighted overlay model in GIS environment after integrating all the thematic layers. The entire district has been classified into three different groundwater potential zones—high, moderate, and low. Greater portion of the study area (60.92%) fall within the moderate potentiality zone, about 22.55% and 16.53% of the total area fall under the high and low potential zone, respectively. Potential zones have been validated with the groundwater yield data, 10 out of 14 validation points (71.43%), matches with the expected yield classes. It shows that the applied method produces significantly reliable results for the present study which can help the decision makers to formulate an effective plan for the study area.

19 January 2021 in Water
Verified
Journal Article
Open access
PDF file
ASAsish Saha
Asish Saha
SPSubodh Chandra Pal
Subodh Chandra Pal
AAAlireza Arabameri
Alireza Arabameri
Thomas BlaschkeThomas Blaschke
Thomas Blaschke
SPSomayeh Panahi
Somayeh Panahi
AAAman Arora
Aman Arora
Recurrent floods are one of the major global threats among people, particularly in developing countries like India, as this nation has a tropical monsoon type of climate. Therefore, flood susceptibility (FS) mapping is indeed necessary to overcome this type of natural hazard phenomena. With this in mind, we evaluated the prediction performance of FS mapping in the Koiya River basin, Eastern India. The present research work was done through preparation of a sophisticated flood inventory map; eight flood conditioning variables were selected based on the topography and hydro-climatological condition, and by applying the novel ensemble approach of hyperpipes (HP) and support vector regression (SVR) machine learning (ML) algorithms. The ensemble approach of HP-SVR was also compared with the stand-alone ML algorithms of HP and SVR. In relative importance of variables, distance to river was the most dominant factor for flood occurrences followed by rainfall, land use land cover (LULC), and normalized difference vegetation index (NDVI). The validation and accuracy assessment of FS maps was done through five popular statistical methods. The result of accuracy evaluation showed that the ensemble approach is the most optimal model (AUC = 0.915, sensitivity = 0.932, specificity = 0.902, accuracy = 0.928 and Kappa = 0.835) in FS assessment, followed by HP (AUC = 0.885) and SVR (AUC = 0.871).