Impact of Hydro-meteorological parameters on Ground water resource and potential source identification at Port Blair city, Andaman and Nicobar

Abstract Understanding hydro-meteorological drivers and spatial flow dynamics is critical for sustainable urban groundwater management in fragile island ecosystems. This study presents a comprehensive assessment of climate variability, groundwater recharge dynamics, and potential source distribution across Port Blair City, Andaman and Nicobar Islands, spanning 2000 to 2023. Long-term meteorological analysis reveals that warm ENSO (El Niño) events significantly suppress rainfall frequency and volume across the region. Although the annual wet days remain steady at 135 ± 11 days, pre-monsoon precipitation exhibits a declining trend (-17mm/year), coupled with increasing pre-monsoon evapotranspiration (+ 6.13 mm/year). Primary groundwater recharge occurs between April and December, where total precipitation (~ 2627mm) exceeds evapotranspiration losses (~ 363 mm). Shallow unconfined aquifers display rapid seasonal response, peaking at depths of ~ 0.4m below ground level (BGL) following the September rainfall peak. However, long-term trends show a post-monsoon water level decline of 0.038m/year, driven by urban expansion, abstraction, and rapid marine discharge. Time-series forecasting using an Exponential Triple Smoothing (ETS AAA) model projects this downward trajectory to continue through 2030 without intervention. Hydrogeological mapping indicates that shallow groundwater (0–2\(\:\text{m}\) BGL) dominates the urban landscape. Formations within the Mithakhari Melange yield the highest groundwater potential (> 1-3L/s to >3L/s). Water table contours reveal prominent radial flow divergence and key recharge/discharge zones in the southeastern, northwestern, northeastern, north-central, and southern sectors. To mitigate localized depletion and capture excessive monsoonal runoff, targeted artificial recharge structures and large-diameter dug wells are recommended within these identified high-potential discharge zones.

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Publication Details

Journal
Research Square
Published
2026-11-09
DOI
https://doi.org/10.21203/rs.3.rs-10685264/v1
Primary Topic
Groundwater and Isotope Geochemistry
Type
preprint
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preprint

Impact of Hydro-meteorological parameters on Ground water resource and potential source identification at Port Blair city, Andaman and Nicobar

Kunal Gaurav Sandip Bhowal, Anadi Gayen, Debasish Bagchi, Nilamoni Barman et al.
Research Square
Groundwater and Isotope Geochemistry
preprint

Impact of Hydro-meteorological parameters on Ground water resource and potential source identification at Port Blair city, Andaman and Nicobar

Kunal Gaurav Sandip Bhowal, Anadi Gayen, Debasish Bagchi, Nilamoni Barman, Prasant Yentapalli, Awadesh Kumar
preprint en

Abstract

Abstract Understanding hydro-meteorological drivers and spatial flow dynamics is critical for sustainable urban groundwater management in fragile island ecosystems. This study presents a comprehensive assessment of climate variability, groundwater recharge dynamics, and potential source distribution across Port Blair City, Andaman and Nicobar Islands, spanning 2000 to 2023. Long-term meteorological analysis reveals that warm ENSO (El Niño) events significantly suppress rainfall frequency and volume across the region. Although the annual wet days remain steady at 135 ± 11 days, pre-monsoon precipitation exhibits a declining trend (-17mm/year), coupled with increasing pre-monsoon evapotranspiration (+ 6.13 mm/year). Primary groundwater recharge occurs between April and December, where total precipitation (~ 2627mm) exceeds evapotranspiration losses (~ 363 mm). Shallow unconfined aquifers display rapid seasonal response, peaking at depths of ~ 0.4m below ground level (BGL) following the September rainfall peak. However, long-term trends show a post-monsoon water level decline of 0.038m/year, driven by urban expansion, abstraction, and rapid marine discharge. Time-series forecasting using an Exponential Triple Smoothing (ETS AAA) model projects this downward trajectory to continue through 2030 without intervention. Hydrogeological mapping indicates that shallow groundwater (0–2\(\:\text{m}\) BGL) dominates the urban landscape. Formations within the Mithakhari Melange yield the highest groundwater potential (> 1-3L/s to >3L/s). Water table contours reveal prominent radial flow divergence and key recharge/discharge zones in the southeastern, northwestern, northeastern, north-central, and southern sectors. To mitigate localized depletion and capture excessive monsoonal runoff, targeted artificial recharge structures and large-diameter dug wells are recommended within these identified high-potential discharge zones.

Research Square
Central Ground Water Board (IN)
Groundwater and Isotope Geochemistry
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