• CH SAMUREMBI CHANU

      Articles written in Journal of Earth System Science

    • Use of GRACE time-series data for estimating groundwater storage at small scale

      CH SAMUREMBI CHANU HARIKA MUNAGAPATI VM TIWARI ARVIND KUMAR L ELANGO

      More Details Abstract Fulltext PDF

      This study integrates the time series of satellite data, i.e. (terrestrial water storage (TWS) extracted from Gravity Recovery and Climate Experiment (GRACE), soil moisture (SM) from Global Land Data Assimilation System (GLDAS), rainfall from Tropical Rainfall Measuring Mission (TRMM)) with in-situ data, i.e. (groundwater (GW) observatory well data and surface water (SW) as reservoir level from Tamil Nadu Public Work Department (TN PWD)) to estimate the water storage of the study area for the period from 2002 March to 2016 December. The study area encompasses three districts of Tamil Nadu State – Chennai, Kancheepuram and Tiruvallur. It was previously observed that the groundwater level in this study area is decreasing at an alarming rate. Trends and residuals of the times series of all the previously stated components were analyzed. Negative trends were observed in the case of $\Delta$SW, $\Delta$SM, $\Delta$GW, $\Delta$TWS-GRACE, but rainfall shows a slight positive trend. Rainfall, being the input for water storage, a marginal increase in rainfall cannot affect the variability of $\Delta$SM, $\Delta$SW, $\Delta$GW and $\Delta$TWS-GRACE. $\Delta$TWS decreases approximately 0.12 cm yr$^{-1}$ averaged water level equal to a total volume −7.5 km$^{3}$. The result of this study shows a decrease in the total storage of groundwater in the study area during the study period from 2002 March to 2016 December. Seawater intrusion due to an increase in sea surface height also shows an impact on $\Delta$TWS derived from grace, in the form of anomalously elevated $\Delta$TWS. A good agreement between $\Delta$TWS-GRACE and $\Delta$TWS- in-situ is found except where sea-water intrusion occurs.

      $\bf{Highlights}$

      $\bullet$ Areal extent of the study area is less than the optimum suggested for GRACE related investigation. The amplitude of the GRACE signal is 300 km and it is recommended that the study area to be larger than that. Our study is perhaps the first such attempt where the study area is much less than recommended.

      $\bullet$ We were able to get a good correlation between $\Delta$GWGRACE and $\Delta$GWINSITU despite the challenge of spatial resolution.

      $\bullet$ A significant finding of the investigation is that distinction in estimates of groundwater changes between GRACE estimates and in-situ perception happens in grids which mostly have sea-area or are intensely impact by urbanization related LULC changes.

      $\bullet$ The impact of various precipitation mechanisms in the examination area was contemplated.

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