GRACE and GRACE-FO Related Publications (no abstracts)

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Would the 2021 Western Europe Flood Event Be Visible in Satellite Gravimetry?

Kracheletz, Magdalena, Liu, Ziyu, Springer, Anne, Kusche, Jürgen, and Friederichs, Petra, 2025. Would the 2021 Western Europe Flood Event Be Visible in Satellite Gravimetry?. Journal of Geophysical Research (Atmospheres), 130(3):2024JD042190, doi:10.1029/2024JD042190.

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BibTeX

@ARTICLE{2025JGRD..13042190K,
       author = {{Kracheletz}, Magdalena and {Liu}, Ziyu and {Springer}, Anne and {Kusche}, J{\"u}rgen and {Friederichs}, Petra},
        title = "{Would the 2021 Western Europe Flood Event Be Visible in Satellite Gravimetry?}",
      journal = {Journal of Geophysical Research (Atmospheres)},
         year = 2025,
        month = feb,
       volume = {130},
       number = {3},
        pages = {2024JD042190},
     abstract = "{The primary objective of the GRACE Follow-On satellite mission is to
        measure temporal changes in the Earth's gravitational field.
        Distance variations between the two GRACE-FO satellites,
        recorded by a K-Band Ranging system and a new Laser Ranging
        Interferometer (LRI), are significantly influenced by
        atmospheric mass redistribution. We investigate whether the sub-
        monthly variations in atmospheric water mass, precipitation, and
        changes in total water storage during the extreme flood event in
        western Europe in 2021 were sufficiently large to influence the
        satellite gravity field measurements, if the GRACE-FO satellites
        would have passed directly over the region. We use several data
        sets such as weather forecasts (ICON-D2 model), hydrological
        simulations (ParFlow/CLM), observations as well as reanalyses,
        showing the high uncertainty between different estimations of
        the considered variables: total precipitable water, total
        precipitation, and total water storage. Our estimates suggest a
        potentially noticeable impact of the 2021 flood event on the
        GRACE-FO satellites. Although it was globally seen a rather
        small event, even the atmospheric water mass beyond water vapor,
        which is not considered within the de-aliasing process, is close
        to the LRI detection accuracy. This is particularly relevant for
        future gravity missions, which will use the LRI with potentially
        higher sensitivity as their main instrument. Sub-monthly
        variations in the total atmospheric water mass, that is, beyond
        water vapor of huge extreme precipitation events should be
        investigated further to reduce potential future aliasing errors.}",
          doi = {10.1029/2024JD042190},
       adsurl = {https://ui.adsabs.harvard.edu/abs/2025JGRD..13042190K},
      adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}

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