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    A study of Bangladesh's sub-surface water storages using satellite products and data assimilation scheme

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    Fulltext not available
    Authors
    Khaki, M.
    Forootan, E.
    Kuhn, Michael
    Awange, Joseph
    Papa, F.
    Shum, C.
    Date
    2018
    Type
    Journal Article
    
    Metadata
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    Citation
    Khaki, M. and Forootan, E. and Kuhn, M. and Awange, J. and Papa, F. and Shum, C. 2018. A study of Bangladesh's sub-surface water storages using satellite products and data assimilation scheme. Science of the Total Environment. 625: pp. 963-977.
    Source Title
    Science of the Total Environment
    DOI
    10.1016/j.scitotenv.2017.12.289
    ISSN
    0048-9697
    School
    School of Earth and Planetary Sciences (EPS)
    URI
    http://hdl.handle.net/20.500.11937/65487
    Collection
    • Curtin Research Publications
    Abstract

    © 2018 Elsevier B.V. Climate change can significantly influence terrestrial water changes around the world particularly in places that have been proven to be more vulnerable such as Bangladesh. In the past few decades, climate impacts, together with those of excessive human water use have changed the country's water availability structure. In this study, we use multi-mission remotely sensed measurements along with a hydrological model to separately analyze groundwater and soil moisture variations for the period 2003–2013, and their interactions with rainfall in Bangladesh. To improve the model's estimates of water storages, terrestrial water storage (TWS) data obtained from the Gravity Recovery And Climate Experiment (GRACE) satellite mission are assimilated into the World-Wide Water Resources Assessment (W3RA) model using the ensemble-based sequential technique of the Square Root Analysis (SQRA) filter. We investigate the capability of the data assimilation approach to use a non-regional hydrological model for a regional case study. Based on these estimates, we investigate relationships between the model derived sub-surface water storage changes and remotely sensed precipitations, as well as altimetry-derived river level variations in Bangladesh by applying the empirical mode decomposition (EMD) method. A larger correlation is found between river level heights and rainfalls (78% on average) in comparison to groundwater storage variations and rainfalls (57% on average). The results indicate a significant decline in groundwater storage (~32% reduction) for Bangladesh between 2003 and 2013, which is equivalent to an average rate of 8.73 ± 2.45 mm/year.

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