Your search found 5 records
1 Singh, K.; Sandhu, H. S.; Singh, N.; Kumar, B.. 1991. Kandi watershed and area development project: Cost benefit analysis of investments in two watersheds. Indian Journal of Agricultural Economics, 46(2):132-141.
Watershed management ; Cost benefit analysis ; Investment ; Agricultural production / India / Punjab
(Location: IWMI-HQ Call no: PER Record No: H04363)
2 Nachiappan, R. P.; Kumar, B.. 1999. Study of the interconnection between a lake and surrounding springs using environmental tracers in the Kumaun Lesser Himalayas. In Leibundgut, C.; McDonnell, J.; Schultz, G. (Eds.), Integrated methods in catchment hydrology: Tracer, remote sensing and new hydrometric techniques. Wallingford, UK: IAHS. pp.215-219.
Water resources ; Hydrology ; Water quality ; Water springs ; Lakes ; Monitoring / India / Kumaun Lesser Himalayas / Nainital Lake / Balia Ravine
(Location: IWMI-HQ Call no: 551.48 G000 LEI Record No: H027505)
3 Nachiappan, R. P.; Kumar, B.; Saravanakumar, U.; Jacob, N.; Sharma, S.; Joseph, T. B.; Navada, S. V.; Manickavasagam, R. 2000. Estimation of sub-surface components in the water balance of lake Nainital (Kuamun Himalaya, India) using environmental isotopes. In Mehrotra, R.; Soni, B.; Bhatia, K. K. S. (Eds.), Integrated water resources management for sustainable development - Volume 1. Roorkee, India: National Institute of Hydrology. pp.239-254.
Water balance ; Pumping ; Precipitation ; Drains ; Groundwater ; Seepage ; Recharge / India / Uttar Pradesh / Lake Nainital
(Location: IWMI-HQ Call no: 333.91 G000 MEH Record No: H028052)
4 Rao, M. S.; Kumar, B.; Nachiappan, R. P.; Jagmohan. 2000. Identification of aquifer recharge sources and zones in parts of Ganga-Yamuna Doab using environmental isotopes. In Mehrotra, R.; Soni, B.; Bhatia, K. K. S. (Eds.), Integrated water resources management for sustainable development - Volume 1. Roorkee, India: National Institute of Hydrology. pp.271-281.
River basins ; Groundwater ; Aquifers ; Recharge / India / Uttar Pradesh / Ganga River / Yamuna River
(Location: IWMI-HQ Call no: 333.91 G000 MEH Record No: H028053)
5 Pranjal, P.; Chatterjee, R. S.; Kumar, D.; Dwivedi, S.; Jally, S. K.; Kumar, B.. 2023. Satellite gravity observation and hydrological modelling-based integrated groundwater storage change in northwestern India. Journal of Hydroinformatics, 25(2):226-242. [doi: https://doi.org/10.2166/hydro.2023.072]
Groundwater recharge ; Hydrological modelling ; Satellite observation ; Hydrometeorology ; Water storage ; Soil moisture ; Groundwater table ; Water balance ; Groundwater depletion ; Infiltration ; Aquifers ; River basins ; Land use ; Land cover ; Infiltration water ; Remote sensing ; Rainfall ; Runoff ; Evapotranspiration ; Soil moisture / India / Delhi / Haryana / Punjab / Rajasthan / Gujarat / Uttar Pradesh / Uttarakhand / Himachal Pradesh / Madhya Pradesh / Maharashtra / Upper Ganga Basin / Yamuna Basin / Chambal Basin / Luni-Ghaggar Basin / Narmada Basin
(Location: IWMI HQ Call no: e-copy only Record No: H051924)
https://iwaponline.com/jh/article-pdf/25/2/226/1201970/jh0250226.pdf
https://vlibrary.iwmi.org/pdf/H051924.pdf
https://vlibrary.iwmi.org/pdf/H051924.pdf
(1.46 MB) (1.46 MB)
This paper presents a novel approach for an improved estimate of regional groundwater storage (GWS) change in Northwestern India by integrating satellite-based Gravity Recovery and Climate Exchange (GRACE) gravity observation and hydrological modelling of satellite/in situ hydrometeorological data. Initially, GRACE observation-based terrestrial water storage (TWS) change and hydrological model-based TWS change products were integrated using weight coefficients derived from multi-linear regression analysis of TWS change vs governing hydrological components. Later, the monthly average soil moisture change was subtracted from the monthly average individual and integrated TWS change products to obtain GWS change products. By spatial correlation analysis, three GWS change products were then compared with groundwater level (GWL) fluctuation-based in situ GWS change. Hydrological model, spaceborne GRACE observation, and integrated GWS change products show a positive correlation in ~59, ~69, and ~73% of the area with in situ GWS change. While a hydrological model-based estimate considers geology, terrain, and hydrometeorological conditions, GRACE gravity observation includes groundwater withdrawal from aquifers. All the factors are included in the integrated product. The approach overcomes the limitations of GRACE observation (spatial resolution, geology, terrain, and hydrometeorological factors), hydrological modelling (groundwater withdrawal conditions), and conventional GWL fluctuation-based method (inadequate spatial continuity and cumbersome, labour-intensive exercise).
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