Publications related to the GRACE Missions (no abstracts)

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Quantification of Glacier Depletion in the Central Tibetan Plateau by Using Integrated Satellite Remote Sensing and Gravimetry

Tseng, K. -H., Liu, K. T., Shum, C. K., Jia, Y., Shang, K., and Dai, C., 2016. Quantification of Glacier Depletion in the Central Tibetan Plateau by Using Integrated Satellite Remote Sensing and Gravimetry. ISPRS - International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, 41B8:399–402, doi:10.5194/isprs-archives-XLI-B8-399-2016.

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@ARTICLE{2016ISPAr41B8..399T,
       author = {{Tseng}, K. -H. and {Liu}, K.~T. and {Shum}, C.~K. and {Jia}, Y. and {Shang}, K. and {Dai}, C.},
        title = "{Quantification of Glacier Depletion in the Central Tibetan Plateau by Using Integrated Satellite Remote Sensing and Gravimetry}",
      journal = {ISPRS - International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences},
         year = 2016,
        month = jun,
       volume = {41B8},
        pages = {399-402},
     abstract = "{Glaciers over the Tibetan Plateau have experienced accelerated depletion
        in the last few decades due primarily to the global warming. The
        freshwater drained into brackish lakes is also observed by
        optical remote sensing and altimetry satellites. However, the
        actual water storage change is difficult to be quantified since
        the altimetry or remote sensing only provide data in limited
        dimensions. The altimetry data give an elevation change of
        surface while the remote sensing images provide an extent
        variation in horizontal plane. Hence a data set used to describe
        the volume change is needed to measure the exact mass transition
        in a time span. In this study, we utilize GRACE gravimetry
        mission to quantify the total column mass change in the central
        Tibetan Plateau, especially focused on the lakes near Tanggula
        Mountains. By removing these factors, the freshwater storage
        change of glacier system at study area can be potentially
        isolated.}",
          doi = {10.5194/isprs-archives-XLI-B8-399-2016},
       adsurl = {https://ui.adsabs.harvard.edu/abs/2016ISPAr41B8..399T},
      adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}

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