EGU24-19178, updated on 11 Mar 2024
https://doi.org/10.5194/egusphere-egu24-19178
EGU General Assembly 2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.

Assessment of total water storage and other variables over the Indus, Ganga, and Brahmaputra River basins

Mohit Yadav1, Ashok Priyadarshan Dimri2, Suraj Mal3, and Pyarimohan Maharana4
Mohit Yadav et al.
  • 1Jawaharlal Nehru University, School of Environmental Sciences, New Delhi, India (yadav.mohit343@gmail.com)
  • 2Jawaharlal Nehru University, School of Environmental Sciences, School of Environmental Sciences, New Delhi, India (apdimri@hotmail.com)
  • 3Jawaharlal Nehru University, Center for the Study of Regional Development, New Delhi, India (suraj.mal@sbs.du.ac.in)
  • 4Dept. of Environmental Studies, Delhi College of Arts and Commerce, University of Delhi, India (maharanapyarimohan@gmail.com)

In the present study, assessment of the abating total water storage (TWS) in the three river basins viz Indus (IRB), Ganga (GRB), and Brahmaputra (BRB) and its associated changes in precipitation across the Indian Himalayan Region (IHR) are examined. Time lead and lag relationship among TWS and other contributory factors viz., precipitation, evaporation, runoff, snow water equivalent (SWE), soil moisture, groundwater, etc., are assessed. In the present study precipitation dataset and TWS available from Global Precipitation Measurement Mission (GPM) and Gravity Recovery and Climate Experiment (GRACE) is used respectively while other variables were extracted from ERA5. Mann-Kendall and Theil Sen estimator test is used for calculating trend of precipitation and TWS during different seasons (winter, pre-monsoon, monsoon, post-monsoon). Our study supports, there is a decreasing trend of TWS over the Indus Ganga Brahmaputra (IGB) basin, though all the basins are drying but slower during monsoon. IRB shows maximum decrease in TWS in postmonsoon whereas over GRB and BRB it is observed in premonsoon. In all seasons, heat flux distributions suggested drying, especially over the higher reaches of the IHR and certain areas of the IRB. The changes in temporal and spatial distribution of TWS over IRB indicate a rapid drop in monsoonal moisture flux. More evaporation and runoff during the monsoon season reduce the TWS process. Present work will be of utmost importance for the policy or planning for state-level governance for societal benefit.

How to cite: Yadav, M., Dimri, A. P., Mal, S., and Maharana, P.: Assessment of total water storage and other variables over the Indus, Ganga, and Brahmaputra River basins, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-19178, https://doi.org/10.5194/egusphere-egu24-19178, 2024.