Hydro-meteorological and biophysical characterization of semi-arid eastern India using geospatial approach

Semi-arid regions are ecologically fragile systems where vegetation dynamics are strongly governed by hydro-meteorological variability. Western Odisha, typifies this climatic sensitivity, with recurrent droughts, erratic rainfall, and high evapotranspiration challenging sustainable land use and agriculture. This study assessed long-term (2001 to 2024) trends of hydro-meteorological and biophysical parameters including precipitation, maximum and minimum air temperature, land surface temperature (LST), actual evapotranspiration (AET), and Normalized Difference Vegetation Index (NDVI) across eight districts of semi-arid Western Odisha using remote sensing datasets and non-parametric trend analysis. Results revealed significant seasonal and spatial heterogeneity. AET exhibited statistically significant declined across most districts during winter and pre-monsoon months, with maximum reductions occurring in April. LST demonstrated widespread cooling during February- May, with rates between − 0.15 and − 0.27 °C year⁻¹ in several districts, while monsoon months showed near-neutral or weakly positive changes. Maximum air temperature displayed strong pre-monsoon warming (0.15–0.22 °C year⁻¹), whereas minimum temperature increased primarily during winter nights (0.05–0.10 °C year⁻¹), indicating intensifying nocturnal warming. NDVI displayed a general greening tendency in pre-monsoon, linked to agricultural intensification, despite declining monsoon precipitation across all districts. LST was highly correlated with maximum air temperature (0.91) and negatively with NDVI (− 0.63). Rainfall exhibited a moderate positive relationship with AET (0.69). The findings highlight a complex climatic transition wherein surface cooling coexists with atmospheric warming, night-time warming, and rainfall reduction. These shifts have direct implications for agricultural water demand, vegetation resilience, and regional climate adaptation planning.

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Journal
Discover Geoscience
Published
2026-01-13
DOI
https://doi.org/10.1007/s44288-026-00397-6
Primary Topic
Plant Water Relations and Carbon Dynamics
Type
article
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article

Hydro-meteorological and biophysical characterization of semi-arid eastern India using geospatial approach

Bishakha Priyadarshini, Argha Ghosh, Arnab Mandal, Dibyalochan Das
Discover Geoscience
Plant Water Relations and Carbon Dynamics
article

Hydro-meteorological and biophysical characterization of semi-arid eastern India using geospatial approach

Bishakha Priyadarshini, Argha Ghosh, Arnab Mandal, Dibyalochan Das
article en

Abstract

Semi-arid regions are ecologically fragile systems where vegetation dynamics are strongly governed by hydro-meteorological variability. Western Odisha, typifies this climatic sensitivity, with recurrent droughts, erratic rainfall, and high evapotranspiration challenging sustainable land use and agriculture. This study assessed long-term (2001 to 2024) trends of hydro-meteorological and biophysical parameters including precipitation, maximum and minimum air temperature, land surface temperature (LST), actual evapotranspiration (AET), and Normalized Difference Vegetation Index (NDVI) across eight districts of semi-arid Western Odisha using remote sensing datasets and non-parametric trend analysis. Results revealed significant seasonal and spatial heterogeneity. AET exhibited statistically significant declined across most districts during winter and pre-monsoon months, with maximum reductions occurring in April. LST demonstrated widespread cooling during February- May, with rates between − 0.15 and − 0.27 °C year⁻¹ in several districts, while monsoon months showed near-neutral or weakly positive changes. Maximum air temperature displayed strong pre-monsoon warming (0.15–0.22 °C year⁻¹), whereas minimum temperature increased primarily during winter nights (0.05–0.10 °C year⁻¹), indicating intensifying nocturnal warming. NDVI displayed a general greening tendency in pre-monsoon, linked to agricultural intensification, despite declining monsoon precipitation across all districts. LST was highly correlated with maximum air temperature (0.91) and negatively with NDVI (− 0.63). Rainfall exhibited a moderate positive relationship with AET (0.69). The findings highlight a complex climatic transition wherein surface cooling coexists with atmospheric warming, night-time warming, and rainfall reduction. These shifts have direct implications for agricultural water demand, vegetation resilience, and regional climate adaptation planning.

Discover GeoscienceVol. 4(1)
Odisha University of Agriculture and Technology (IN)
Zero hunger
Openalex Percentile: Top 93%
Plant Water Relations and Carbon Dynamics
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