Unveiling rainfall and erosivity dynamics in Odisha’s varied agro-climatic zones for sustainable soil and water conservation planning

• Published in: Theoretical and applied climatology 2024-08, Vol.155 (8), p.7557-7574
• Main Authors: Dash, Ch. Jyotiprava, Shrimali, S. S., Madhu, M., Kumar, Randhir, Adhikary, Partha Pratim
• Format: Article
• Language: English
• Subjects: Agricultural land; Agricultural practices; Agricultural production; Annual; Annual rainfall; Annual rainfall data; Aquatic Pollution; Arable land; Aromatic compounds; Atmospheric Protection/Air Quality Control/Air Pollution; Atmospheric Sciences; Bioengineering; Climate change; Climatic zones; Climatology; Coastal plains; Crop production; Earth and Environmental Science; Earth Sciences; Eleusine coracana; Erosion rates; Fingers; Grasses; Highlands; Hydrologic data; Intercropping; Land conservation; Land use; Millet; Moisture content; Plateaus; Precipitation; Rainfall; Rainfall distribution; Rainfall patterns; Rainfall-climatic change relationships; Soil conservation; Soil erosion; Soil fertility; Soil loss; Soil water; Spatial variability; Spatial variations; Strip cropping; Waste Water Technology; Water availability; Water conservation; Water Management; Water Pollution Control
• ISSN: 0177-798X; 1434-4483
• DOI: 10.1007/s00704-024-05089-0

Climate change leads to changes in climatic variables, with rainfall being one of them. Changes in rainfall influence rainfall erosivity and subsequently erosion rates. This study analysed rainfall data from 1901 to 2017 in Odisha, focusing on different agro-climatic zones to discern annual rainfall pattern, its spatial variation, and trend, particularly concerning the rainfall erosivity factor and its impact on soil erosion and agricultural productivity. Notably, the Eastern Ghats Highland region received the highest average annual rainfall of 1578.5 mm, while the Western Undulating Zone received the lowest (1308.4 mm). The rainfall distribution showed spatial variability largely influenced by topography, with areas experiencing orographic lifting receiving higher rainfall. The study observed significant trend in annual rainfall, noting a maximum decline of 1.2 mm yr −1 in the North Western Plateau, Western Central Table Land, and Western Undulating Zone, whereas the East and South Eastern Plain, Mid Central Table Land, North Eastern Coastal Plain, North Eastern Ghats, and South Eastern Ghats exhibited a noteworthy increase in annual rainfall (0 to 3.9 mm yr −1 ). The decline in rainfall can result in the drying up of water bodies and reduced soil water availability to crop, thereby influencing agricultural production. On the other hand, areas with increased rainfall, may face extreme events which can aggravate soil erosion and thereby loss of soil fertility. Considering the scarcity of pluviographic data in countries like India, Modified Fournier Index (MFI) may be considered as one of the useful methods to capture rainfall’s aggressiveness towards soil erosion through rainfall erosivity (R-factor). Therefore, to evaluate potential soil erosion levels, the Modified Fournier Index method was employed, revealing varying degrees of soil erosiveness across different regions. The Eastern Ghats Highlands exhibited the highest erosion potential. The R-factor, aligned with these spatial patterns, with the Eastern Ghats Highland (12,965.4 MJ mm ha −1  h −1  yr −1 ) and South Eastern Ghats (12,242.3 MJ mm ha −1  h −1  yr −1 ) regions displaying the highest R-factor values. Furthermore, the research identified areas prone to soil erosion by overlaying R-factor, slope, and land use maps, highlighting vulnerable regions such as Eastern Ghats Highlands, North Eastern Ghats, South Eastern Ghats, and Western Undulating Zone. This comprehensive analysis allows for inform