Mathematical Modelling of Rainfall and Water Security in Ranchi Using Prophet under Climate Change

Climate change significantly affects water availability in monsoon-dependent Ranchi, India. This study analyzes historical weather data (1979–2024) and uses the Prophet forecasting model to project monthly rainfall (PRCP) and average temperature (TAVG) through 2045. Based on regional trends, a 7% increase in monsoon rainfall and a 0.2°C/decade temperature rise is integrated. Rainfall deficits are calculated against a 100 mm/month baseline, adjusted for evaporation losses. Results show persistent non-monsoon deficits (e.g., 100 mm in December–February), with monsoon peaks rising to 268 mm by 2045. Temperature increases (0.4–0.6°C by 2045) exacerbate deficits, especially in May (31.2°C). These findings underscore the need for adaptive water management, such as enhanced storage and irrigation, to ensure water security in a warming climate.

Publication Details

Journal
International Journal of Mathematics Trends and Technology
Published
2025-08-30
DOI
https://doi.org/10.14445/22315373/ijmtt-v71i8p107
Primary Topic
Hydrology and Drought Analysis
Type
article
Field-Weighted Citation Impact
0.00

Funders

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article

Mathematical Modelling of Rainfall and Water Security in Ranchi Using Prophet under Climate Change

International Journal of Mathematics Trends and Technology
Hydrology and Drought Analysis
article

Mathematical Modelling of Rainfall and Water Security in Ranchi Using Prophet under Climate Change

article en

Abstract

Climate change significantly affects water availability in monsoon-dependent Ranchi, India. This study analyzes historical weather data (1979–2024) and uses the Prophet forecasting model to project monthly rainfall (PRCP) and average temperature (TAVG) through 2045. Based on regional trends, a 7% increase in monsoon rainfall and a 0.2°C/decade temperature rise is integrated. Rainfall deficits are calculated against a 100 mm/month baseline, adjusted for evaporation losses. Results show persistent non-monsoon deficits (e.g., 100 mm in December–February), with monsoon peaks rising to 268 mm by 2045. Temperature increases (0.4–0.6°C by 2045) exacerbate deficits, especially in May (31.2°C). These findings underscore the need for adaptive water management, such as enhanced storage and irrigation, to ensure water security in a warming climate.

International Journal of Mathematics Trends and TechnologyVol. 71(8)
National Oceanic and Atmospheric Administration
Openalex Percentile: Top 76%
Hydrology and Drought Analysis
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